{"pageNumber":"492","pageRowStart":"12275","pageSize":"25","recordCount":184582,"records":[{"id":70220871,"text":"sir20205057 - 2021 - Flood-inundation maps for the Blue River near Red Bridge Road, Kansas City, Missouri, 2019","interactions":[],"lastModifiedDate":"2021-05-28T19:21:03.271116","indexId":"sir20205057","displayToPublicDate":"2021-05-28T11:11:37","publicationYear":"2021","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2020-5057","displayTitle":"Flood-Inundation Maps for the Blue River near Red Bridge Road, Kansas City, Missouri, 2019","title":"Flood-inundation maps for the Blue River near Red Bridge Road, Kansas City, Missouri, 2019","docAbstract":"<p>Digital flood-inundation maps for a 4.6-mile reach of the Blue River near Red Bridge Road in Kansas City, Missouri, were created by the U.S. Geological Survey (USGS), in cooperation with the City of Kansas City, Missouri. The flood-inundation maps, which can be accessed through the USGS Flood Inundation Mapping Program website at <a data-mce-href=\"https://www.usgs.gov/mission-areas/water-resources/science/flood-inundation-mapping-fim-program\" href=\"https://www.usgs.gov/mission-areas/water-resources/science/flood-inundation-mapping-fim-program\">https://www.usgs.gov/mission-areas/water-resources/science/flood-inundation-mapping-fim-program</a>, depict estimates of the areal extent and depth of flooding corresponding to selected water levels (stages) at the USGS streamgage 06893195, Blue River at Red Bridge Road, Kansas City, Mo. Near-real-time stages at this streamgage may be obtained from the USGS National Water Information System at <a data-mce-href=\"https://doi.org/10.5066/F7P55KJN\" href=\"https://doi.org/10.5066/F7P55KJN\">https://doi.org/10.5066/F7P55KJN</a> or the Johnson County, Kansas, StormWatch Automated Local Elevation in Real Time Flood Warning System at <a data-mce-href=\"https://www.stormwatch.com\" href=\"https://www.stormwatch.com\">https://www.stormwatch.com</a>.</p><p>Flood profiles were computed for the Blue River reach by means of a one-dimensional model for simulating water-surface profiles with steady-state flow computations. The model was calibrated by using the current stage-streamflow relations at the upstream USGS streamgage 06893150, Blue River at Blue Ridge Boulevard Extension, Kansas City, Mo., and the downstream streamgage 06893500, Blue River at Kansas City, Mo.</p><p>The hydraulic model was then used to compute 37 water-surface profiles for flood stages at 1-foot (ft) intervals referenced to the streamgage datum and ranging from 11 ft, or near bankfull, to 47 ft at the reference streamgage 06893195. The upper stage for the map library exceeds the stage corresponding to the estimated 0.2-percent annual exceedance probability flood (500-year recurrence interval flood) in the model reach. The simulated water-surface profiles were then combined with a geographic information system digital elevation model with a maximum 10-centimeter vertical root mean square error and 4.0-ft horizontal resolution to delineate the area flooded at each water level.</p><p>The availability of these maps, along with real-time internet information regarding current stage from the USGS streamgage, will help guide emergency management personnel and residents in flood mitigation, preparedness and planning, flood-response activities such as evacuations and road closures, and any postflood recovery efforts.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20205057","collaboration":"Prepared in cooperation with the City of Kansas City, Missouri","usgsCitation":"Heimann, D.C., Voss, J.D., and Rydlund, P.H., Jr., 2021, Flood-inundation maps for the Blue River near Red Bridge Road, Kansas City, Missouri, 2019: U.S. Geological Survey Scientific Investigations Report 2020–5057, 14 p., https://doi.org/10.3133/sir20205057.","productDescription":"Report: vi, 14 p.; Data Release; Dataset","numberOfPages":"24","onlineOnly":"Y","ipdsId":"IP-117597","costCenters":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":385983,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P90MH291","text":"USGS data release","description":"USGS Data Release","linkHelpText":"Geospatial datasets for the flood-inundation study of the Blue River near Red Bridge Road, Kansas City, Missouri, 2019"},{"id":385984,"rank":4,"type":{"id":28,"text":"Dataset"},"url":"https://doi.org/10.5066/F7P55KJN","text":"U.S. Geological Survey National Water Information System","description":"USGS Dataset","linkHelpText":"— USGS water data for the Nation"},{"id":385981,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2020/5057/coverthb.jpg"},{"id":385982,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2020/5057/sir20205057.pdf","text":"Report","size":"1.51 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2020–5057"}],"country":"United States","state":"Kansas, Missouri","otherGeospatial":"Blue River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.83333,\n              38.8333\n            ],\n            [\n              -94.45,\n              38.8333\n            ],\n            [\n              -94.45,\n              39.1666\n            ],\n            [\n              -94.833333,\n              39.1666\n            ],\n            [\n              -94.833333,\n              38.8333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a data-mce-href=\"mailto:%20dc_mo@usgs.gov\" href=\"mailto:%20dc_mo@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/cm-water\" href=\"https://www.usgs.gov/centers/cm-water\">Central Midwest Water Science Center</a> <br><a data-mce-href=\"https://www.usgs.gov/\" href=\"https://www.usgs.gov/\">U.S. Geological Survey</a><br>1400 Independence Road <br>Rolla, MO 65401</p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Creation of Flood-Inundation-Map Library</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2021-05-28","noUsgsAuthors":false,"publicationDate":"2021-05-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Heimann, David C. 0000-0003-0450-2545 dheimann@usgs.gov","orcid":"https://orcid.org/0000-0003-0450-2545","contributorId":3822,"corporation":false,"usgs":true,"family":"Heimann","given":"David","email":"dheimann@usgs.gov","middleInitial":"C.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voss, Jonathon D. 0000-0001-8219-7887","orcid":"https://orcid.org/0000-0001-8219-7887","contributorId":224636,"corporation":false,"usgs":true,"family":"Voss","given":"Jonathon","email":"","middleInitial":"D.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rydlund, Paul H. Jr. 0000-0001-9461-9944 prydlund@usgs.gov","orcid":"https://orcid.org/0000-0001-9461-9944","contributorId":3840,"corporation":false,"usgs":true,"family":"Rydlund","given":"Paul","suffix":"Jr.","email":"prydlund@usgs.gov","middleInitial":"H.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70220894,"text":"sir20215044 - 2021 - Characterization of historical and stochastically generated climate and streamflow conditions in the Souris River Basin, United States and Canada","interactions":[],"lastModifiedDate":"2021-05-28T19:05:24.819834","indexId":"sir20215044","displayToPublicDate":"2021-05-28T10:53:21","publicationYear":"2021","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2021-5044","displayTitle":"Characterization of Historical and Stochastically Generated Climate and Streamflow Conditions in the Souris River Basin, United States and Canada","title":"Characterization of historical and stochastically generated climate and streamflow conditions in the Souris River Basin, United States and Canada","docAbstract":"<p>The Souris River Basin is a 61,000-square-kilometer basin in the Provinces of Saskatchewan and Manitoba in Canada and the State of North Dakota in the United States. Greater than average snowpack during the winter of 2010–11, along with record-setting rains in May and June 2011, resulted in historically unprecedented flooding in the Souris River Basin. The severity of the 2011 flood led the United States and Canada to request a review of the operating plan for any improvements of reservoir operations and flood control measures in the basin, and the Souris River Basin Task Force was formed. The International Souris River Study Board was then formed in 2017 to carry out the recommendations of the Souris River Basin Task Force laid out in a plan of study. To support the International Souris River Study Board, the U.S. Geological Survey (USGS), in cooperation with the North Dakota State Water Commission and the International Joint Commission, used the previously developed unregulated and regulated streamflow models and data for stochastic streamflow in the Souris River Basin to characterize climate and streamflow and support selection of streamflow traces based on their characterization. Components of the original stochastic hydrology models and their outputs were used in this phase of the study to (1) characterize historical and stochastic climate and streamflow for the Souris River Basin, (2) disaggregate monthly stochastic streamflow spatially and temporally to meet the needs of the U.S. Army Corps of Engineers, Hydrologic Engineering Center, Reservoir System Simulation model for the Souris River Basin, and (3) discuss selection of disaggregated streamflow traces (simulations) using the characteristics of climate and streamflow. A trace is a time series of a stochastic variable such as streamflow, potential evapotranspiration, or precipitation.</p><p>To characterize climate conditions, precipitation, potential evapotranspiration (PET), and moisture deficit for the Souris River Basin and individual points at Rafferty, Grant Devine, and Lake Darling Reservoirs were determined annually and seasonally. The annual basin (November 1–October 31) precipitation for the 50-percent nonexceedance probability is 452 millimeters (mm). Spring (March–May) is the wettest season, followed by summer (June–August), fall (September–November), and winter (December–February). Annual moisture deficit was largest at Lake Darling Reservoir, followed by Rafferty Reservoir, and then Grant Devine Reservoir.</p><p>Annual maximum monthly mean streamflow was determined for the Souris River below Rafferty Reservoir, Saskatchewan (Canadian streamgage 05NB036); Long Creek near Noonan (above Boundary Reservoir), North Dakota (USGS streamgage 05113600); Moose Mountain Creek near Oxbow, Saskatchewan (Canadian streamgage 05ND004); the Souris River near Sherwood, N. Dak. (USGS streamgage 05114000); the Des Lacs River at Foxholm, N. Dak. (USGS streamgage 05116500); and the Souris River above Minot, N. Dak. (USGS streamgage 05117500). When the seasonal maximum monthly mean streamflows are evaluated in contrast to annual maximum monthly mean streamflows separated by their seasonal occurrence, summer months of annual maximum monthly mean streamflows have a higher 50-percent exceedance probability of streamflow compared to annual maximum monthly mean streamflows that occur in spring, seasonal maximum monthly mean streamflows that occur in spring, and seasonal maximum monthly mean streamflows that occur in summer. When annual maximum monthly mean streamflows in summer are compared to annual maximum monthly mean streamflows in spring, they are consistently higher in streamflow but occur in less than 4.2 percent of years. Evaluation of whether the annual maximum monthly mean streamflows that occur in summer can be described as a separate population from annual maximum monthly mean streamflows that occur in spring was outside the scope of this study, and the summer and spring annual maximum monthly mean streamflows were not tested for statistical differences in mean or variance. Further investigation of seasonal weather patterns that induce flooding could lead to a better understanding of the seasonal differences in flooding.</p><p>Long-term hydrologic drought was characterized by evaluating multiyear mean streamflow. Shorter averaging periods have greater streamflow variability than longer periods and hence have a wider range of values. As the averaging period is extended to a longer period, the variability of mean streamflow decreases, and the more extreme streamflow volumes seen in shorter averaging periods cannot be sustained. Stochastic streamflow time series were disaggregated spatially and temporally for use in a HEC–ResSim model. The combination of monthly and daily stochastic streamflow data was used to select traces with qualities that could be used to test alternatives focused on water supply, summer flooding, and apportionment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20215044","collaboration":"Prepared in cooperation with the North Dakota State Water Commission and the International Joint Commission","usgsCitation":"Gregory, A., and Galloway, J.M., 2021, Characterization of historical and stochastically generated climate and streamflow conditions in the Souris River Basin, United States and Canada: U.S. Geological Survey Scientific Investigations Report 2021–5044, 36 p., https://doi.org/10.3133/sir20215044.","productDescription":"Report: viii, 36 p.; Data Release; Dataset","numberOfPages":"48","onlineOnly":"Y","ipdsId":"IP-120682","costCenters":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":386014,"rank":4,"type":{"id":28,"text":"Dataset"},"url":"https://doi.org/10.5066/F7P55KJN","text":"U.S. Geological Survey National Water Information System database","linkHelpText":"— USGS water data for the Nation"},{"id":386011,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2021/5044/coverthb.jpg"},{"id":386012,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2021/5044/sir20215044.pdf","text":"Report","size":"5.03 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2021—5044"},{"id":386013,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P93AOWFL","text":"USGS data release","linkHelpText":"Historical and stochastically generated climate and streamflow data for the Souris River Basin, United States and Canada"}],"country":"Canada, United States","state":"Manitoba, North Dakota, Saskatchewan","otherGeospatial":"Souris River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.55859375,\n              46.6795944656402\n            ],\n            [\n              -98.0859375,\n              50.12057809796008\n            ],\n            [\n              -101.25,\n              51.67255514839674\n            ],\n            [\n              -107.138671875,\n              53.48804553605622\n            ],\n            [\n              -108.6328125,\n              50.958426723359935\n            ],\n            [\n              -102.568359375,\n              48.22467264956519\n            ],\n            [\n              -99.66796875,\n              46.98025235521883\n            ],\n            [\n              -97.55859375,\n              46.6795944656402\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a data-mce-href=\"mailto:%20dc_nd@usgs.gov\" href=\"mailto:%20dc_nd@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/dakota-water\" href=\"https://www.usgs.gov/centers/dakota-water\">Dakota Water Science Center</a> <br>U.S. Geological Survey<br>821 East Interstate Avenue<br>Bismarck, ND 58503 <br>1608 Mountain View Road<br>Rapid City, SD 57702</p><p><a data-mce-href=\"../contact\" href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Methods of Analysis</li><li>Historical and Stochastic Climate Characteristics</li><li>Stochastically Generated Natural (Unregulated) Streamflow Characteristics</li><li>Disaggregated Daily Stochastic Streamflow</li><li>Stochastically Generated Regulated Streamflow and Reservoir Volume Characteristics</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2021-05-28","noUsgsAuthors":false,"publicationDate":"2021-05-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Gregory, Angela 0000-0002-9905-1240","orcid":"https://orcid.org/0000-0002-9905-1240","contributorId":45018,"corporation":false,"usgs":true,"family":"Gregory","given":"Angela","email":"","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galloway, Joel M. 0000-0002-9836-9724 jgallowa@usgs.gov","orcid":"https://orcid.org/0000-0002-9836-9724","contributorId":1562,"corporation":false,"usgs":true,"family":"Galloway","given":"Joel","email":"jgallowa@usgs.gov","middleInitial":"M.","affiliations":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70226770,"text":"70226770 - 2021 - Introduction: Does water flow on Martian slopes?","interactions":[],"lastModifiedDate":"2021-12-13T13:30:41.0207","indexId":"70226770","displayToPublicDate":"2021-05-28T07:29:38","publicationYear":"2021","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Introduction: Does water flow on Martian slopes?","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mars Geological Enigmas From the Late Noachian Epoch to the Present Day","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Elsevier","doi":"10.1016/B978-0-12-820245-6.00021-5","usgsCitation":"Dundas, C., Conway, S.J., and Stillman, D.E., 2021, Introduction: Does water flow on Martian slopes?, chap. <i>of</i> Mars Geological Enigmas From the Late Noachian Epoch to the Present Day, p. 205-206, https://doi.org/10.1016/B978-0-12-820245-6.00021-5.","productDescription":"2 p.","startPage":"205","endPage":"206","ipdsId":"IP-123147","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":392787,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dundas, Colin M. 0000-0003-2343-7224","orcid":"https://orcid.org/0000-0003-2343-7224","contributorId":237028,"corporation":false,"usgs":true,"family":"Dundas","given":"Colin M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":828201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conway, Susan J.","contributorId":203697,"corporation":false,"usgs":false,"family":"Conway","given":"Susan","email":"","middleInitial":"J.","affiliations":[{"id":36693,"text":"University of Nantes","active":true,"usgs":false}],"preferred":false,"id":828202,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stillman, David E","contributorId":141053,"corporation":false,"usgs":false,"family":"Stillman","given":"David","email":"","middleInitial":"E","affiliations":[{"id":13664,"text":"Southwest Research Institute, Boulder CO","active":true,"usgs":false}],"preferred":false,"id":828203,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70226787,"text":"70226787 - 2021 - Dry formation of recent Martian slope features","interactions":[],"lastModifiedDate":"2021-12-13T13:27:42.656542","indexId":"70226787","displayToPublicDate":"2021-05-28T07:26:38","publicationYear":"2021","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"10","title":"Dry formation of recent Martian slope features","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab0010\" class=\"abstract author\"><div id=\"abs0010\"><p id=\"sp0045\">Martian surface conditions are cold and dry, unfavorable for liquid water, yet steep slopes display young and currently active features suggestive of wet processes. These include recurring slope lineae and slope streaks, gully landforms, and small lobate features. Wet origins for these features would imply surprising amounts of liquid water at the surface. However, detailed observations of the morphology and activity of these features have demonstrated that dry processes, some of them unique to the Martian environment, can account for all of them. This reconciles the contradiction between physics and geomorphology and provides a self-consistent model of a Martian surface that is very active today despite having negligible volumes of liquid water.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mars Geological Enigmas From the Late Noachian Epoch to the Present Day","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Elsevier","doi":"10.1016/B978-0-12-820245-6.00010-0","usgsCitation":"Dundas, C., 2021, Dry formation of recent Martian slope features, chap. 10 <i>of</i> Mars Geological Enigmas From the Late Noachian Epoch to the Present Day, p. 263-288, https://doi.org/10.1016/B978-0-12-820245-6.00010-0.","productDescription":"26 p.","startPage":"263","endPage":"288","ipdsId":"IP-117640","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":392786,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dundas, Colin M. 0000-0003-2343-7224","orcid":"https://orcid.org/0000-0003-2343-7224","contributorId":237028,"corporation":false,"usgs":true,"family":"Dundas","given":"Colin M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":828257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70226594,"text":"70226594 - 2021 - Floral resource selection by wild bees and honey bees in the Midwest United States: Implications for designing pollinator habitat","interactions":[],"lastModifiedDate":"2021-12-01T13:21:30.054747","indexId":"70226594","displayToPublicDate":"2021-05-28T07:19:46","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3271,"text":"Restoration Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Floral resource selection by wild bees and honey bees in the Midwest United States: Implications for designing pollinator habitat","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Many seed mix recommendations for creating pollinator habitat are in part based on anecdotal evidence or field observations of bees visiting forbs (i.e. use). However, there is limited information on what forbs are preferred by bees, particularly in working landscapes where bee forage may be limited. We examined floral resource selection by wild bees and honey bees on grasslands in the Midwest using a 5-year dataset containing over 8,000 plant-bee interactions. We observed wild bees visiting 83 forb species, but only 14 species were significantly selected (i.e. bees visited a plant more than expected based on availability). Approximately 70% of all wild bee visitations were on native flowers, whereas only 20% of all honey bee visitations were on natives. Honey bees visited 70 forb species, but only four forbs were significantly selected. The selection ratio for each forb species was not correlated with proportion of use by wild bees or honey bees, suggesting that bee visitation data alone do not elucidate patterns of forb selection or avoidance. We then compared our resource selection results to forbs recommended by U.S. Department of Agriculture (USDA) for regional pollinator habitat plantings. Many forbs that were selected by bees in our study were also recommended by USDA; however, some USDA-recommended forbs were selected against by bees. A greater understanding of which floral resources are selected by bees can assist land managers in assessing conservation seed mixes and ultimately provide diverse, season-long pollinator forage in working landscapes.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/rec.13456","usgsCitation":"Simanonok, S.C., Otto, C., and Buhl, D.A., 2021, Floral resource selection by wild bees and honey bees in the Midwest United States: Implications for designing pollinator habitat: Restoration Ecology, v. 29, no. 8, e13456, 11 p., https://doi.org/10.1111/rec.13456.","productDescription":"e13456, 11 p.","ipdsId":"IP-121320","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":392299,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota, North Dakota, South 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,{"id":70221162,"text":"70221162 - 2021 - Amplified impact of climate change on fine-sediment delivery to a subsiding coast, Humboldt Bay, California","interactions":[],"lastModifiedDate":"2021-11-01T15:19:55.310982","indexId":"70221162","displayToPublicDate":"2021-05-28T07:19:44","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1584,"text":"Estuaries and Coasts","active":true,"publicationSubtype":{"id":10}},"title":"Amplified impact of climate change on fine-sediment delivery to a subsiding coast, Humboldt Bay, California","docAbstract":"<p><span>In Humboldt Bay, tectonic subsidence exacerbates sea-level rise (SLR). To build surface elevations and to keep pace with SLR, the sediment demand created by subsidence and SLR must be balanced by an adequate sediment supply. This study used an ensemble of plausible future scenarios to predict potential climate change impacts on suspended-sediment discharge (Q</span><sub>ss</sub><span>) from fluvial sources. Streamflow was simulated using a deterministic water-balance model, and Q</span><sub>ss</sub><span>&nbsp;was computed using statistical sediment-transport models. Changes relative to a baseline period (1981–2010) were used to assess climate&nbsp;impacts. For local basins that discharge directly to the bay, the ensemble means projected increases in Q</span><sub>ss</sub><span>&nbsp;of 27% for the mid-century (2040–2069) and 58% for the end-of-century (2070–2099). For the Eel River, a regional sediment source that discharges sediment-laden plumes to the coastal margin, the ensemble means projected increases in Q</span><sub>ss</sub><span>&nbsp;of 53% for the mid-century and 99% for the end-of-century. Climate projections of increased precipitation and streamflow produced amplified increases in the regional sediment supply that may partially or wholly mitigate sediment demand caused by the combined effects of subsidence and SLR. This finding has important implications for coastal resiliency. Coastal regions with an increasing sediment supply may be more resilient to SLR. In a broader context, an increasing sediment supply from fluvial sources has global relevance for communities threatened by SLR that are increasingly building resiliency to SLR using sediment-based solutions that include regional sediment management, beneficial reuse strategies, and marsh restoration.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s12237-021-00938-x","usgsCitation":"Curtis, J., Flint, L.E., Stern, M.A., Lewis, J., and Klein, R.D., 2021, Amplified impact of climate change on fine-sediment delivery to a subsiding coast, Humboldt Bay, California: Estuaries and Coasts, v. 44, p. 2173-2193, https://doi.org/10.1007/s12237-021-00938-x.","productDescription":"21 p.","startPage":"2173","endPage":"2193","ipdsId":"IP-102755","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":452090,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s12237-021-00938-x","text":"Publisher Index Page"},{"id":436333,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P97UBENK","text":"USGS data release","linkHelpText":"Daily Basin Characterization Model (BCM) archive for Humboldt Bay/Eel River"},{"id":386195,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"California","county":"Humboldt County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.49707031249999,\n              39.53793974517623\n            ],\n            [\n              -123.96972656249999,\n              39.53793974517623\n            ],\n            [\n              -123.96972656249999,\n              41.41801503608022\n            ],\n            [\n              -124.49707031249999,\n              41.41801503608022\n            ],\n            [\n              -124.49707031249999,\n              39.53793974517623\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"44","noUsgsAuthors":false,"publicationDate":"2021-05-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Curtis, Jennifer 0000-0001-7766-994X","orcid":"https://orcid.org/0000-0001-7766-994X","contributorId":212727,"corporation":false,"usgs":true,"family":"Curtis","given":"Jennifer","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Lorraine E. 0000-0002-7868-441X lflint@usgs.gov","orcid":"https://orcid.org/0000-0002-7868-441X","contributorId":1184,"corporation":false,"usgs":true,"family":"Flint","given":"Lorraine","email":"lflint@usgs.gov","middleInitial":"E.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816913,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stern, Michelle A. 0000-0003-3030-7065 mstern@usgs.gov","orcid":"https://orcid.org/0000-0003-3030-7065","contributorId":4244,"corporation":false,"usgs":true,"family":"Stern","given":"Michelle","email":"mstern@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816914,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lewis, Jack","contributorId":189105,"corporation":false,"usgs":false,"family":"Lewis","given":"Jack","email":"","affiliations":[],"preferred":false,"id":816915,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klein, Randy D.","contributorId":259269,"corporation":false,"usgs":false,"family":"Klein","given":"Randy","email":"","middleInitial":"D.","affiliations":[{"id":36189,"text":"National Park Service","active":true,"usgs":false}],"preferred":false,"id":816916,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70229016,"text":"70229016 - 2021 - Declining diversity of wild-caught species puts dietary nutrient supplies at risk","interactions":[],"lastModifiedDate":"2022-02-25T13:11:00.258941","indexId":"70229016","displayToPublicDate":"2021-05-28T07:06:40","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5010,"text":"Science Advances","active":true,"publicationSubtype":{"id":10}},"title":"Declining diversity of wild-caught species puts dietary nutrient supplies at risk","docAbstract":"<div id=\"abstracts\"><div class=\"core-container\"><div>Although biodiversity loss adversely influences a variety of ecosystem functions, how declining wild food diversity affects nutrient supplies for people is poorly understood. Here, we analyze the impact of declining biodiversity on nutrients supplied by fish using detailed information from the Peruvian Amazon, where inland fisheries provide a critical source of nutrition for many of the region’s 800,000 people. We found that the impacts of biodiversity loss on nutrient supplies depended on compensation, trophic dynamics, and functional diversity. When small sedentary species compensated for declines in large migratory species, fatty acid supplies increased, while zinc and iron supplies decreased. In contrast, the probability of failing to maintain supplies or nutrient supply risk increased when species were nutritionally unique. Our results show that trait-based regulations and public health polices need to consider biodiversity’s vital role in sustaining nutritional benefits for over 2 billion people dependent on wild foods across the globe.</div></div></div>","language":"English","publisher":"Science","doi":"10.1126/sciadv.abf9967","usgsCitation":"Heilpern, S.A., DeFries, R., Fiorella, K.J., Flecker, A., Sethi, S., Uriarte, M., and Naeem, S., 2021, Declining diversity of wild-caught species puts dietary nutrient supplies at risk: Science Advances, v. 7, no. 22, eabf9967, 8 p., https://doi.org/10.1126/sciadv.abf9967.","productDescription":"eabf9967, 8 p.","ipdsId":"IP-120442","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":452094,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1126/sciadv.abf9967","text":"External Repository"},{"id":396474,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"22","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Heilpern, Sebastian A.","contributorId":280260,"corporation":false,"usgs":false,"family":"Heilpern","given":"Sebastian","email":"","middleInitial":"A.","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":836131,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeFries, Ruth","contributorId":280261,"corporation":false,"usgs":false,"family":"DeFries","given":"Ruth","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":836132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fiorella, Kathryn J.","contributorId":268093,"corporation":false,"usgs":false,"family":"Fiorella","given":"Kathryn","email":"","middleInitial":"J.","affiliations":[{"id":12722,"text":"Cornell University","active":true,"usgs":false}],"preferred":false,"id":836158,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flecker, Alexander","contributorId":280262,"corporation":false,"usgs":false,"family":"Flecker","given":"Alexander","affiliations":[{"id":12722,"text":"Cornell University","active":true,"usgs":false}],"preferred":false,"id":836133,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sethi, Suresh 0000-0002-0053-1827 ssethi@usgs.gov","orcid":"https://orcid.org/0000-0002-0053-1827","contributorId":191424,"corporation":false,"usgs":true,"family":"Sethi","given":"Suresh","email":"ssethi@usgs.gov","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":836159,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Uriarte, María","contributorId":280263,"corporation":false,"usgs":false,"family":"Uriarte","given":"María","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":836134,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Naeem, Shahid","contributorId":280264,"corporation":false,"usgs":false,"family":"Naeem","given":"Shahid","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":836135,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70221343,"text":"70221343 - 2021 - Use of the smeltCam as an efficient fish sampling alternative within the San Francisco Estuary","interactions":[],"lastModifiedDate":"2021-06-11T12:05:22.631939","indexId":"70221343","displayToPublicDate":"2021-05-28T07:04:41","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3331,"text":"San Francisco Estuary and Watershed Science","active":true,"publicationSubtype":{"id":10}},"title":"Use of the smeltCam as an efficient fish sampling alternative within the San Francisco Estuary","docAbstract":"<p><span>Resource managers often rely on long-term monitoring surveys to detect trends in biological data. However, no survey gear is 100% efficient, and many sources of bias can be responsible for detecting or not detecting biological trends. The SmeltCam is an imaging apparatus developed as a potential sampling alternative to long-term trawling gear surveys within the San Francisco Estuary, California, to reduce handling stress on sensitive species like the Delta Smelt (</span><i>Hypomesus transpacificus</i><span>). Although believed to be a reliable alternative to closed cod-end trawling surveys, no formal test of sampling efficiency has been implemented using the SmeltCam. We used a paired deployment of the SmeltCam and a conventional closed cod-end trawl within the Napa River and San Pablo Bay, a Bayesian binomial&nbsp;</span><i>N</i><span>-mixture model, and data simulations to determine the sampling efficiency of both deployed gear types to capture a Delta Smelt surrogate (Northern Anchovy,&nbsp;</span><i>Engraulis mordax</i><span>) and to test potential bias in our modeling framework. We found that retention efficiency—a component of detection efficiency that estimates the probability a fish is retained by the gear, conditional on gear contact—was slightly higher using the SmeltCam (mean = 0.58) than the conventional trawl (mean = 0.47, Probability SmeltCam retention efficiency &gt; trawl retention efficiency = 94%). We also found turbidity did not affect the SmeltCam’s retention efficiency, although total fish density during an individual tow improved the trawl’s retention efficiency. Simulations also showed the binomial model was accurate when model assumptions were met. Collectively, our results suggest the SmeltCam to be a reliable alternative to sampling with conventional trawling gear, but future tests are needed to confirm whether the SmeltCam is as reliable when applied to taxa other than Northern Anchovy over a greater range of conditions.</span></p>","language":"English","publisher":"University of California","doi":"10.15447/sfews.2021v19iss2art6","usgsCitation":"Huntsman, B., Feyrer, F.V., and Young, M.J., 2021, Use of the smeltCam as an efficient fish sampling alternative within the San Francisco Estuary: San Francisco Estuary and Watershed Science, v. 19, no. 2, 16 p., https://doi.org/10.15447/sfews.2021v19iss2art6.","productDescription":"16 p.","ipdsId":"IP-123894","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":452096,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.15447/sfews.2021v19iss2art6","text":"Publisher Index Page"},{"id":386410,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"San Francisco","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.57421875,\n              36.84446074079564\n            ],\n            [\n              -121.86035156249999,\n              36.84446074079564\n            ],\n            [\n              -121.86035156249999,\n              39.40224434029275\n            ],\n            [\n              -123.57421875,\n              39.40224434029275\n            ],\n            [\n              -123.57421875,\n              36.84446074079564\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2020-06-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Huntsman, Brock 0000-0003-4090-1949","orcid":"https://orcid.org/0000-0003-4090-1949","contributorId":223101,"corporation":false,"usgs":true,"family":"Huntsman","given":"Brock","email":"","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":817384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feyrer, Frederick V. 0000-0003-1253-2349 ffeyrer@usgs.gov","orcid":"https://orcid.org/0000-0003-1253-2349","contributorId":178379,"corporation":false,"usgs":true,"family":"Feyrer","given":"Frederick","email":"ffeyrer@usgs.gov","middleInitial":"V.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":817385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, Matthew J. 0000-0001-9306-6866 mjyoung@usgs.gov","orcid":"https://orcid.org/0000-0001-9306-6866","contributorId":206255,"corporation":false,"usgs":true,"family":"Young","given":"Matthew","email":"mjyoung@usgs.gov","middleInitial":"J.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":817386,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70239051,"text":"70239051 - 2021 - Predicting light regime controls on primary productivity across CONUS river networks","interactions":[],"lastModifiedDate":"2022-12-22T13:03:46.202793","indexId":"70239051","displayToPublicDate":"2021-05-28T06:54:43","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Predicting light regime controls on primary productivity across CONUS river networks","docAbstract":"<div class=\"article-section__content en main\"><p>Solar radiation is a fundamental driver of ecosystem productivity, but widespread estimates of light available for primary producers in rivers are lacking. We developed a model to predict light available for river primary producers and used it to estimate river primary production across the contiguous United States (CONUS). Successively accounting for riparian and water column processes improved predictions of primary production as a function of light. We calculated the ratio of river width to riparian tree height and used this metric to predict whether riparian zones or water column processes most limit productivity for over 2 million reaches. Water column processes limited productivity for 50% of the nation's river length and 80% of its surface area, with variations across ecoregions related to riparian forest cover. Our findings facilitate large-scale predictions of stream and river ecosystem productivity, as well as understanding the processes controlling productivity across networks.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2020GL092149","usgsCitation":"Savoy, P., and Harvey, J., 2021, Predicting light regime controls on primary productivity across CONUS river networks: Geophysical Research Letters, v. 48, no. 10, e2020GL092149, 10 p., https://doi.org/10.1029/2020GL092149.","productDescription":"e2020GL092149, 10 p.","ipdsId":"IP-123965","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":452099,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2020gl092149","text":"Publisher Index Page"},{"id":436334,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9LREC3P","text":"USGS data release","linkHelpText":"Light model and GPP estimates for 173 U.S. rivers"},{"id":410924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n          [\n            [\n              [\n                -94.81758,\n                49.38905\n              ],\n              [\n                -94.64,\n                48.84\n              ],\n              [\n                -94.32914,\n                48.67074\n              ],\n              [\n                -93.63087,\n                48.60926\n              ],\n              [\n                -92.61,\n                48.45\n              ],\n              [\n                -91.64,\n                48.14\n              ],\n              [\n                -90.83,\n                48.27\n      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              -89.41373,\n                29.89419\n              ],\n              [\n                -89.43,\n                29.48864\n              ],\n              [\n                -89.21767,\n                29.29108\n              ],\n              [\n                -89.40823,\n                29.15961\n              ],\n              [\n                -89.77928,\n                29.30714\n              ],\n              [\n                -90.15463,\n                29.11743\n              ],\n              [\n                -90.88022,\n                29.14854\n              ],\n              [\n                -91.62678,\n                29.677\n              ],\n              [\n                -92.49906,\n                29.5523\n              ],\n              [\n                -93.22637,\n                29.78375\n              ],\n              [\n                -93.84842,\n                29.71363\n              ],\n              [\n                -94.69,\n                29.48\n              ],\n              [\n                -95.60026,\n                28.73863\n              ],\n              [\n                -96.59404,\n                28.30748\n              ],\n              [\n                -97.14,\n                27.83\n              ],\n              [\n                -97.37,\n                27.38\n              ],\n              [\n                -97.38,\n                26.69\n              ],\n              [\n                -97.33,\n                26.21\n              ],\n              [\n                -97.14,\n                25.87\n              ],\n              [\n                -97.53,\n                25.84\n              ],\n              [\n                -98.24,\n                26.06\n              ],\n              [\n                -99.02,\n                26.37\n              ],\n              [\n                -99.3,\n                26.84\n              ],\n              [\n                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       [\n                -117.29594,\n                33.04622\n              ],\n              [\n                -117.944,\n                33.62124\n              ],\n              [\n                -118.4106,\n                33.74091\n              ],\n              [\n                -118.51989,\n                34.02778\n              ],\n              [\n                -119.081,\n                34.078\n              ],\n              [\n                -119.43884,\n                34.34848\n              ],\n              [\n                -120.36778,\n                34.44711\n              ],\n              [\n                -120.62286,\n                34.60855\n              ],\n              [\n                -120.74433,\n                35.15686\n              ],\n              [\n                -121.71457,\n                36.16153\n              ],\n              [\n                -122.54747,\n                37.55176\n              ],\n              [\n                -122.51201,\n                37.78339\n              ],\n              [\n                -122.95319,\n                38.11371\n              ],\n              [\n                -123.7272,\n                38.95166\n              ],\n              [\n                -123.86517,\n                39.76699\n              ],\n              [\n                -124.39807,\n                40.3132\n              ],\n              [\n                -124.17886,\n                41.14202\n              ],\n              [\n                -124.2137,\n                41.99964\n              ],\n              [\n                -124.53284,\n                42.76599\n              ],\n              [\n                -124.14214,\n                43.70838\n              ],\n              [\n                -124.02053,\n                44.6159\n              ],\n              [\n                -123.89893,\n                45.52341\n              ],\n              [\n                -124.07963,\n                46.86475\n              ],\n              [\n                -124.39567,\n                47.72017\n              ],\n              [\n                -124.68721,\n                48.18443\n              ],\n              [\n                -124.5661,\n                48.37971\n              ],\n              [\n                -123.12,\n                48.04\n              ],\n              [\n                -122.58736,\n                47.096\n              ],\n              [\n                -122.34,\n                47.36\n              ],\n              [\n                -122.5,\n                48.18\n              ],\n              [\n                -122.84,\n                49\n              ],\n              [\n                -120,\n                49\n              ],\n              [\n                -117.03121,\n                49\n              ],\n              [\n                -116.04818,\n                49\n              ],\n              [\n                -113,\n                49\n              ],\n              [\n                -110.05,\n                49\n              ],\n              [\n                -107.05,\n                49\n              ],\n              [\n                -104.04826,\n                48.99986\n              ],\n              [\n                -100.65,\n                49\n              ],\n              [\n                -97.22872,\n                49.0007\n              ],\n              [\n                -95.15907,\n                49\n              ],\n              [\n                -95.15609,\n                49.38425\n              ],\n              [\n                -94.81758,\n                49.38905\n              ]\n            ]\n          ]\n        ]\n      },\n      \"properties\": {\n        \"name\": \"United States\"\n      }\n    }\n  ]\n}","volume":"48","issue":"10","noUsgsAuthors":false,"publicationDate":"2021-05-24","publicationStatus":"PW","contributors":{"authors":[{"text":"Savoy, Philip 0000-0002-6075-837X","orcid":"https://orcid.org/0000-0002-6075-837X","contributorId":300288,"corporation":false,"usgs":true,"family":"Savoy","given":"Philip","email":"","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":859854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harvey, Judson 0000-0002-2654-9873","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":219104,"corporation":false,"usgs":true,"family":"Harvey","given":"Judson","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":859855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221054,"text":"70221054 - 2021 - Ten years of volcanic activity at Mt Etna: High-resolution mapping and accurate quantification of the morphological changes by Pleiades and Lidar data","interactions":[],"lastModifiedDate":"2021-06-01T14:22:02.175408","indexId":"70221054","displayToPublicDate":"2021-05-28T06:52:40","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":8912,"text":"International Journal of Applied Earth Observations and Geoinformation","active":true,"publicationSubtype":{"id":10}},"title":"Ten years of volcanic activity at Mt Etna: High-resolution mapping and accurate quantification of the morphological changes by Pleiades and Lidar data","docAbstract":"<p><span>The topography of Mt. Etna, Italy, is subjected to continuous modifications depending on intensity and magnitude of eruptions that frequently occur at the volcano summit and flanks. In order to make high-resolution maps of morphological changes and accurately calculate the overall volume of the erupted products (e.g., lava flows, tephra fall out, scoriae cones) in ten years, we have compared the altimetry models of Mt. Etna derived from 2005 Airborne Laser Scanning data and 2015 Pleiades stereo satellite imagery. Both models cover a common area of 400&nbsp;km</span><sup>2</sup><span>&nbsp;with spatial resolution of 2&nbsp;m and comparable vertical accuracy (RMSE&nbsp;&lt;&nbsp;0.8&nbsp;m). The results show that the area most affected by the erupted products is the mid-upper portion of the volcano with an altitude ranging from 1300&nbsp;m to more than 3300&nbsp;m a.s.l., value reached at the summit of the North East crater. In particular, this portion changes dramatically in the eastern sector due to the birth and growth of the New South-East Crater, the invasion of dozens of lava flows in the Valle del Bove, and the formation of the 2014 scoriae cones and lava field at the base of the North-East Crater. The total volume of products erupted in the investigated period results in 284.3±15.8 x 10</span><sup>6</sup><span>&nbsp;m</span><sup>3</sup><span>&nbsp;with a yearly average volume of 28.4 x 10</span><sup>6</sup><span>&nbsp;m</span><sup>3</sup><span>/y comparable with the previous decades. In addition, the products emitted by the 2014 sub-terminal eruption are mapped and quantified including, for the first time, the volume of the 2014 scoriae cones generated on the eastern flank of North-East Crater This study demonstrates how a rigorous comparison between digital elevation models derived from different remote sensing techniques produce high accurate mapping and quantifications of morphological changes applicable for worldwide active volcanoes. This allows to quantify volumes and areas of erupted products reducing the error estimations, a crucial point to provide precise data often used as key parameters for many volcanic hazard studies.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jag.2021.102369","usgsCitation":"Bisson, M., Spinetti, C., Andronico, D., Palaseanu-Lovejoy, M., Buongiorno, M.F., Alexandrov, O., and Cecere, T., 2021, Ten years of volcanic activity at Mt Etna: High-resolution mapping and accurate quantification of the morphological changes by Pleiades and Lidar data: International Journal of Applied Earth Observations and Geoinformation, v. 102, 102369, 11 p., https://doi.org/10.1016/j.jag.2021.102369.","productDescription":"102369, 11 p.","ipdsId":"IP-121404","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":452102,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.jag.2021.102369","text":"Publisher Index Page"},{"id":386026,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Italy","otherGeospatial":"Mt. Etna, Sicily","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              14.849395751953125,\n              37.62402129571883\n            ],\n            [\n              15.137786865234377,\n              37.62402129571883\n            ],\n            [\n              15.137786865234377,\n              37.85859141570558\n            ],\n            [\n              14.849395751953125,\n              37.85859141570558\n            ],\n            [\n              14.849395751953125,\n              37.62402129571883\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"102","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bisson, Marina 0000-0002-7104-9210","orcid":"https://orcid.org/0000-0002-7104-9210","contributorId":221724,"corporation":false,"usgs":false,"family":"Bisson","given":"Marina","email":"","affiliations":[{"id":40408,"text":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, via Della Faggiola, Pisa, 56126, Italy","active":true,"usgs":false}],"preferred":false,"id":816657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinetti, Claudia 0000-0002-1861-5666","orcid":"https://orcid.org/0000-0002-1861-5666","contributorId":221725,"corporation":false,"usgs":false,"family":"Spinetti","given":"Claudia","email":"","affiliations":[{"id":40409,"text":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione ONT, via di Vigna Murata, Roma, 00143, Italy","active":true,"usgs":false}],"preferred":false,"id":816658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andronico, Daniele 0000-0002-8333-1547","orcid":"https://orcid.org/0000-0002-8333-1547","contributorId":259163,"corporation":false,"usgs":false,"family":"Andronico","given":"Daniele","email":"","affiliations":[{"id":52323,"text":"Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo","active":true,"usgs":false}],"preferred":false,"id":816659,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Palaseanu-Lovejoy, Monica 0000-0002-3786-5118 mpal@usgs.gov","orcid":"https://orcid.org/0000-0002-3786-5118","contributorId":3639,"corporation":false,"usgs":true,"family":"Palaseanu-Lovejoy","given":"Monica","email":"mpal@usgs.gov","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true},{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":816660,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Buongiorno, Maria Fabrizia 0000-0002-6095-6974","orcid":"https://orcid.org/0000-0002-6095-6974","contributorId":221726,"corporation":false,"usgs":false,"family":"Buongiorno","given":"Maria","email":"","middleInitial":"Fabrizia","affiliations":[{"id":40409,"text":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione ONT, via di Vigna Murata, Roma, 00143, Italy","active":true,"usgs":false}],"preferred":false,"id":816661,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Alexandrov, Oleg","contributorId":167662,"corporation":false,"usgs":false,"family":"Alexandrov","given":"Oleg","email":"","affiliations":[{"id":24796,"text":"NASA Ames Research Center","active":true,"usgs":false}],"preferred":false,"id":816662,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cecere, Thomas 0000-0001-5254-8404 tcecere@usgs.gov","orcid":"https://orcid.org/0000-0001-5254-8404","contributorId":221727,"corporation":false,"usgs":true,"family":"Cecere","given":"Thomas","email":"tcecere@usgs.gov","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":816663,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70222118,"text":"70222118 - 2021 - The contribution of land cover change to the decline of honey yields in the Northern Great Plains","interactions":[],"lastModifiedDate":"2021-07-21T11:49:16.089532","indexId":"70222118","displayToPublicDate":"2021-05-28T06:51:43","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1562,"text":"Environmental Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"The contribution of land cover change to the decline of honey yields in the Northern Great Plains","docAbstract":"<p><span>Decreased availability of forage, as well as increased pesticide exposure, are important factors in the decline of honey bee health. Here, we isolate land cover transitions and their effect on honey production at 160 commercial apiaries in the Northern Great Plains. We found that land cover changes from 2008 to 2012 caused an annual decline in honey yields of 0.9% in the study area. Transitions from grassland to soybean (but not corn) were particularly detrimental to honey yields, potentially due to bee contact with pesticides within and around agricultural fields. When our results are applied to known apiary locations across all of North Dakota (U.S.A.), we estimate a 2.5% (1.6 million USD) decline in 2012 honey yields due to land cover changes occurring between 2008 and 2012. Even when controlling for changes in land cover, we found that on average colonies in the study area experienced a 14% annual decline in honey yields. We discuss possible explanations for these non-land-cover-related honey yield declines, including changing economic conditions (e.g. pollination services), changes in land management (e.g. pesticides), and increases in pests or diseases.</span></p>","language":"English","publisher":"IOP Publishing","doi":"10.1088/1748-9326/abfde8","usgsCitation":"Smith, D., Davis, A.Y., Hitaj, C., Hellerstein, D., Preslicka, A., Kirkpatrick, E., Mushet, D., and Lonsdorf, E., 2021, The contribution of land cover change to the decline of honey yields in the Northern Great Plains: Environmental Research Letters, v. 16, 064050, 12 p., https://doi.org/10.1088/1748-9326/abfde8.","productDescription":"064050, 12 p.","ipdsId":"IP-105742","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":452104,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1088/1748-9326/abfde8","text":"Publisher Index Page"},{"id":387285,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.755859375,\n              43.004647127794435\n            ],\n            [\n              -96.50390625,\n              43.004647127794435\n            ],\n            [\n              -96.50390625,\n              44.465151013519616\n            ],\n            [\n              -99.755859375,\n              44.465151013519616\n            ],\n            [\n              -99.755859375,\n              43.004647127794435\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","noUsgsAuthors":false,"publicationDate":"2021-05-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, David","contributorId":261251,"corporation":false,"usgs":false,"family":"Smith","given":"David","affiliations":[{"id":52784,"text":"U.S. Department of Agriculture, Economic Research Service","active":true,"usgs":false}],"preferred":false,"id":819594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Amelie Y. 0000-0001-7373-7618","orcid":"https://orcid.org/0000-0001-7373-7618","contributorId":261252,"corporation":false,"usgs":false,"family":"Davis","given":"Amelie","email":"","middleInitial":"Y.","affiliations":[{"id":17754,"text":"Miami University, Department of Geography & Institute for the Environment and Sustainability","active":true,"usgs":false}],"preferred":false,"id":819595,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hitaj, Claudia 0000-0002-6408-9265","orcid":"https://orcid.org/0000-0002-6408-9265","contributorId":261253,"corporation":false,"usgs":false,"family":"Hitaj","given":"Claudia","email":"","affiliations":[{"id":52784,"text":"U.S. Department of Agriculture, Economic Research Service","active":true,"usgs":false}],"preferred":false,"id":819596,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hellerstein, Dan","contributorId":261254,"corporation":false,"usgs":false,"family":"Hellerstein","given":"Dan","affiliations":[{"id":52784,"text":"U.S. Department of Agriculture, Economic Research Service","active":true,"usgs":false}],"preferred":false,"id":819597,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Preslicka, Amanda","contributorId":261255,"corporation":false,"usgs":false,"family":"Preslicka","given":"Amanda","email":"","affiliations":[{"id":17754,"text":"Miami University, Department of Geography & Institute for the Environment and Sustainability","active":true,"usgs":false}],"preferred":false,"id":819598,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kirkpatrick, Emma","contributorId":261256,"corporation":false,"usgs":false,"family":"Kirkpatrick","given":"Emma","email":"","affiliations":[{"id":17754,"text":"Miami University, Department of Geography & Institute for the Environment and Sustainability","active":true,"usgs":false}],"preferred":false,"id":819599,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mushet, David M. 0000-0002-5910-2744","orcid":"https://orcid.org/0000-0002-5910-2744","contributorId":248468,"corporation":false,"usgs":true,"family":"Mushet","given":"David M.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":819600,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lonsdorf, Eric","contributorId":261257,"corporation":false,"usgs":false,"family":"Lonsdorf","given":"Eric","email":"","affiliations":[{"id":52785,"text":"University of Minnesota, Institute on the Environment","active":true,"usgs":false}],"preferred":false,"id":819601,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70220717,"text":"sir20215033 - 2021 - Overview and methodology for a study to identify fecal contamination sources using microbial source tracking in seven embayments on Long Island, New York","interactions":[],"lastModifiedDate":"2022-09-01T10:06:27.850627","indexId":"sir20215033","displayToPublicDate":"2021-05-27T18:19:54","publicationYear":"2021","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2021-5033","displayTitle":"Overview and Methodology for a Study To Identify Fecal Contamination Sources Using Microbial Source Tracking in Seven Embayments on Long Island, New York","title":"Overview and methodology for a study to identify fecal contamination sources using microbial source tracking in seven embayments on Long Island, New York","docAbstract":"<p>Between June 2018 and July 2019, the U.S. Geological Survey collaborated with the New York State Department of Environmental Conservation to analyze water quality in seven embayments on Long Island, New York, for a study to examine fecal contamination using microbial source tracking. This report documents the approach, methodology, and quality-assurance data used in the study. All samples and field data were collected in accordance with U.S. Geological Survey National Field Manual procedures. Samples were analyzed for host-specific deoxyribonucleic acid (DNA) markers, fecal coliform bacteria, inorganic and total organic nitrogen, and stable isotopes of nitrate and ammonium.</p><p>Samples for quality control were collected for microbiological analyses at a rate of 1 per 20 environmental samples. A total of 14 blank and 15 replicate samples were collected for DNA markers, 52 sequential field replicates were analyzed by the Public Environmental Health Laboratory of the Suffolk County Department of Health Services and the New York State Department of Conservation Marine Laboratory for fecal coliform, and 7 blank and 7 replicate samples were collected to be analyzed for nutrients. Results from quality-control samples collected throughout the course of the study confirmed that sampling procedures were adequate and did not disqualify any data from analysis.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20215033","collaboration":"Prepared in cooperation with the New York State Department of Environmental Conservation","usgsCitation":"Tagliaferri, T.N., Fisher, S.C., Kephart, C.M., Cheung, N., Reed, A.P., and Welk, R.J., 2021, Overview and methodology for a study to identify fecal contamination sources using microbial source tracking in seven embayments on Long Island, New York: U.S. Geological Survey Scientific Investigations Report 2021–5033, 8 p., https://doi.org/10.3133/sir20215033.","productDescription":"iv, 8 p.","numberOfPages":"8","onlineOnly":"Y","ipdsId":"IP-128174","costCenters":[{"id":474,"text":"New York Water Science 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Source Tracking To Identify Fecal Contamination Sources in Patchogue and Bellport Bays on Long Island, New York"},{"id":406047,"rank":6,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20225028","text":"Scientific Investigations Report 2022–5028","linkHelpText":"- Using Microbial Source Tracking To Identify Fecal Contamination Sources in Sag Harbor on Long Island, New York"},{"id":406046,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20225038","text":"Scientific Investigations Report 2022–5038","linkHelpText":"- Using Microbial Source Tracking To Identify Fecal Contamination Sources in Lake Montauk on Long Island, New York"},{"id":406045,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20225057","text":"Scientific Investigations Report 2022–5057","linkHelpText":"- Using Microbial Source Tracking To Identify Fecal Contamination Sources in Great South Bay on Long 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,{"id":70221055,"text":"70221055 - 2021 - Spring 2021 edition","interactions":[],"lastModifiedDate":"2024-02-16T17:32:14.648614","indexId":"70221055","displayToPublicDate":"2021-05-27T11:31:35","publicationYear":"2021","noYear":false,"publicationType":{"id":25,"text":"Newsletter"},"publicationSubtype":{"id":30,"text":"Newsletter"},"seriesTitle":{"id":10521,"text":"RAMPS Newsletter","active":true,"publicationSubtype":{"id":30}},"title":"Spring 2021 edition","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"McCormick, M.L., and Munson, S.M., 2021, Spring 2021 edition: RAMPS Newsletter, HTML Document.","productDescription":"HTML Document","ipdsId":"IP-129916","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":425737,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":386025,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.usgs.gov/center-news/ramps-newsletter-spring-2021-edition"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McCormick, Molly L. 0000-0002-4361-7567 mmccormick@usgs.gov","orcid":"https://orcid.org/0000-0002-4361-7567","contributorId":196257,"corporation":false,"usgs":true,"family":"McCormick","given":"Molly","email":"mmccormick@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":816664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Munson, Seth M. 0000-0002-2736-6374 smunson@usgs.gov","orcid":"https://orcid.org/0000-0002-2736-6374","contributorId":1334,"corporation":false,"usgs":true,"family":"Munson","given":"Seth","email":"smunson@usgs.gov","middleInitial":"M.","affiliations":[{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":816665,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70229737,"text":"70229737 - 2021 - Improving short-term recruitment forecasts for coho salmon using a spatiotemporal integrated population model","interactions":[],"lastModifiedDate":"2022-03-16T16:11:47.02032","indexId":"70229737","displayToPublicDate":"2021-05-27T11:06:46","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1661,"text":"Fisheries Research","active":true,"publicationSubtype":{"id":10}},"title":"Improving short-term recruitment forecasts for coho salmon using a spatiotemporal integrated population model","docAbstract":"<p><span>Fishery managers often rely on forecasts of future population abundance to set allowable harvest quotas or exploitation rates. While there has been substantial research devoted to identifying environmental factors that can predict recruitment for individual populations, such correlations often degrade over time, thereby limiting their utility for management. Conversely, examining multiple populations at once to detect shared, spatially structured patterns can offer insights into their recruitment dynamics that are advantageous for forecasting. Here, we develop a population dynamics model for natural origin coho salmon (</span><span><i>Oncorhynchus kisutch</i></span><span>) stocks in Washington State that leverages spatial and temporal&nbsp;autocorrelation&nbsp;in marine survival to improve one-year-ahead forecasts of adult returns. Executed in a Bayesian hierarchical integrated modelling framework, our spatiotemporal approach incorporates multiple data types and shares information among stocks to estimate key biological parameters that are informative for forecasting. Retrospective evaluation of one-year-ahead forecast skill indicated that the spatiotemporal integrated population model (ST-IPM) outperformed existing forecasts of Washington State coho salmon returns by 25–38 % on average. Moreover, the ST-IPM estimates parameters that were previously non-identifiable for many stocks, and propagates uncertainty from multiple contributing data sources into model forecasts. Our results add to a growing body of work demonstrating the utility of spatiotemporal and integrated approaches for modelling population dynamics, and the framework developed here has broad applications to the assessment and management of coho salmon in Washington State and elsewhere throughout their range.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.fishres.2021.106014","usgsCitation":"DeFilippo, L.B., Buehrens, T., Scheuerell, M.D., Kendall, N.W., and Schindler, D.E., 2021, Improving short-term recruitment forecasts for coho salmon using a spatiotemporal integrated population model: Fisheries Research, v. 242, 106014, 12 p., https://doi.org/10.1016/j.fishres.2021.106014.","productDescription":"106014, 12 p.","ipdsId":"IP-129173","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":452108,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index 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,{"id":70228726,"text":"70228726 - 2021 - Large-scale variation in wave attenuation of oyster reef living shorelines and the influence of inundation duration","interactions":[],"lastModifiedDate":"2022-02-17T15:27:17.969322","indexId":"70228726","displayToPublicDate":"2021-05-27T09:18:07","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Large-scale variation in wave attenuation of oyster reef living shorelines and the influence of inundation duration","docAbstract":"<p><span>One of the paramount goals of oyster reef living shorelines is to achieve sustained and adaptive coastal protection, which requires meeting ecological (i.e., develop a self-sustaining oyster population) and engineering (i.e., provide coastal defense) targets. In a large-scale comparison along the Atlantic and Gulf coasts of the United States, the efficacy of various designs of oyster reef living shorelines at providing wave attenuation was evaluated accounting for the ecological limitations of oysters with regard to inundation duration. A critical threshold for intertidal oyster reef establishment is 50% inundation duration. Living shorelines that spent less than one-half of the time (&lt;50%) inundated were not considered suitable habitat for oysters, however, were effective at wave attenuation (68% reduction in wave height). Reefs that experienced &gt;50% inundation were considered suitable habitat for oysters, but wave attenuation was similar to controls (no reef; ~5% reduction in wave height). Many of the oyster reef living shoreline approaches therefore failed to optimize the ecological and engineering goals. In both inundation regimes, wave transmission decreased with an increasing freeboard (difference between reef crest elevation and water level), supporting its importance in the wave attenuation capacity of oyster reef living shorelines. However, given that the reef crest elevation (and thus freeboard) should be determined by the inundation duration requirements of oysters, research needs to be refocused on understanding the implications of other reef parameters (e.g., width) for optimizing wave attenuation. A broader understanding of the reef characteristics and seascape contexts that result in effective coastal defense by oyster reefs is needed to inform appropriate design and implementation of oyster-based living shorelines globally.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1002/eap.2382","usgsCitation":"Morris, R.L., La Peyre, M., Webb, B.M., Marshall, D.A., Bilkovic, D., Cebrian, J., McClenachan, G., Kibler, K.M., Walters, L.J., Bushek, D., Sparks, E.L., Temple, N.A., Moody, J., Angstadt, K., Goff, J., Boswell, M.K., Sacks, P.E., and Swearer, S.E., 2021, Large-scale variation in wave attenuation of oyster reef living shorelines and the influence of inundation duration: Ecological Applications, v. 31, no. 6, e02382, 15 p., https://doi.org/10.1002/eap.2382.","productDescription":"e02382, 15 p.","ipdsId":"IP-113781","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":481103,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://scholarworks.wm.edu/vimsarticles/2082","text":"External Repository"},{"id":396101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Louisiana, New Jersey, Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.35205078124999,\n              30.278044377800153\n            ],\n            [\n              -88.0224609375,\n              30.278044377800153\n            ],\n            [\n              -88.0224609375,\n              30.751277776257812\n            ],\n            [\n              -88.35205078124999,\n              30.751277776257812\n            ],\n            [\n              -88.35205078124999,\n              30.278044377800153\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.736328125,\n              29.707139348134145\n            ],\n            [\n              -89.31884765624999,\n              29.707139348134145\n            ],\n            [\n              -89.31884765624999,\n              30.20211367909724\n            ],\n            [\n              -89.736328125,\n              30.20211367909724\n            ],\n            [\n              -89.736328125,\n              29.707139348134145\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.14501953125,\n              28.671310915880834\n            ],\n            [\n              -80.5078125,\n              28.671310915880834\n            ],\n            [\n              -80.5078125,\n              29.209713225868185\n            ],\n            [\n              -81.14501953125,\n              29.209713225868185\n            ],\n            [\n              -81.14501953125,\n              28.671310915880834\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.43212890625,\n              39.07890809706475\n            ],\n            [\n              -74.970703125,\n              39.07890809706475\n            ],\n            [\n              -74.970703125,\n              39.50404070558415\n            ],\n            [\n              -75.43212890625,\n              39.50404070558415\n            ],\n            [\n              -75.43212890625,\n              39.07890809706475\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.61865234374999,\n              37.09023980307208\n            ],\n            [\n              -76.0693359375,\n              37.09023980307208\n            ],\n            [\n              -76.0693359375,\n              37.77071473849609\n            ],\n            [\n              -76.61865234374999,\n              37.77071473849609\n            ],\n            [\n              -76.61865234374999,\n              37.09023980307208\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"6","noUsgsAuthors":false,"publicationDate":"2021-06-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Morris, R. L. 0000-0003-0455-0811","orcid":"https://orcid.org/0000-0003-0455-0811","contributorId":243390,"corporation":false,"usgs":false,"family":"Morris","given":"R.","email":"","middleInitial":"L.","affiliations":[{"id":13336,"text":"University of Melbourne","active":true,"usgs":false}],"preferred":false,"id":835203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"La Peyre, Megan K. 0000-0001-9936-2252","orcid":"https://orcid.org/0000-0001-9936-2252","contributorId":264343,"corporation":false,"usgs":true,"family":"La Peyre","given":"Megan K.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":835204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webb, B. M.","contributorId":243400,"corporation":false,"usgs":false,"family":"Webb","given":"B.","email":"","middleInitial":"M.","affiliations":[{"id":48710,"text":"University of South Alabama","active":true,"usgs":false}],"preferred":false,"id":835205,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marshall, D. A.","contributorId":276081,"corporation":false,"usgs":false,"family":"Marshall","given":"D.","email":"","middleInitial":"A.","affiliations":[{"id":5115,"text":"Louisiana State University","active":true,"usgs":false}],"preferred":false,"id":835206,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bilkovic, D. M.","contributorId":243391,"corporation":false,"usgs":false,"family":"Bilkovic","given":"D. M.","affiliations":[{"id":37406,"text":"College of William & Mary","active":true,"usgs":false}],"preferred":false,"id":835207,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cebrian, J.","contributorId":243394,"corporation":false,"usgs":false,"family":"Cebrian","given":"J.","affiliations":[{"id":48710,"text":"University of South Alabama","active":true,"usgs":false}],"preferred":false,"id":835208,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McClenachan, G.","contributorId":243397,"corporation":false,"usgs":false,"family":"McClenachan","given":"G.","email":"","affiliations":[{"id":18879,"text":"University of Central Florida","active":true,"usgs":false}],"preferred":false,"id":835209,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kibler, K. M.","contributorId":243396,"corporation":false,"usgs":false,"family":"Kibler","given":"K.","email":"","middleInitial":"M.","affiliations":[{"id":18879,"text":"University of Central Florida","active":true,"usgs":false}],"preferred":false,"id":835210,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Walters, L. J.","contributorId":243403,"corporation":false,"usgs":false,"family":"Walters","given":"L.","email":"","middleInitial":"J.","affiliations":[{"id":12727,"text":"Rutgers University","active":true,"usgs":false}],"preferred":false,"id":835211,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bushek, D.","contributorId":243393,"corporation":false,"usgs":false,"family":"Bushek","given":"D.","affiliations":[{"id":12727,"text":"Rutgers University","active":true,"usgs":false}],"preferred":false,"id":835212,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Sparks, E. L.","contributorId":243402,"corporation":false,"usgs":false,"family":"Sparks","given":"E.","email":"","middleInitial":"L.","affiliations":[{"id":17848,"text":"Mississippi State University","active":true,"usgs":false}],"preferred":false,"id":835213,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Temple, N. A.","contributorId":243399,"corporation":false,"usgs":false,"family":"Temple","given":"N.","email":"","middleInitial":"A.","affiliations":[{"id":17848,"text":"Mississippi State University","active":true,"usgs":false}],"preferred":false,"id":835214,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Moody, J. A.","contributorId":187515,"corporation":false,"usgs":false,"family":"Moody","given":"J. A.","affiliations":[],"preferred":false,"id":835215,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Angstadt, K.","contributorId":279613,"corporation":false,"usgs":false,"family":"Angstadt","given":"K.","email":"","affiliations":[{"id":57314,"text":"William & Mary","active":true,"usgs":false}],"preferred":false,"id":835216,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Goff, J.","contributorId":279614,"corporation":false,"usgs":false,"family":"Goff","given":"J.","affiliations":[{"id":48711,"text":"Dauphin Island Sea Lab","active":true,"usgs":false}],"preferred":false,"id":835217,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Boswell, M. K.","contributorId":243392,"corporation":false,"usgs":false,"family":"Boswell","given":"M.","email":"","middleInitial":"K.","affiliations":[{"id":36518,"text":"Old Dominion University","active":true,"usgs":false}],"preferred":false,"id":835218,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Sacks, P. E.","contributorId":190958,"corporation":false,"usgs":false,"family":"Sacks","given":"P.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":835219,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Swearer, S. E.","contributorId":243401,"corporation":false,"usgs":false,"family":"Swearer","given":"S.","email":"","middleInitial":"E.","affiliations":[{"id":13336,"text":"University of Melbourne","active":true,"usgs":false}],"preferred":false,"id":835220,"contributorType":{"id":1,"text":"Authors"},"rank":18}]}}
,{"id":70220879,"text":"70220879 - 2021 - Appendix C: Central sands lakes study technical report: Modeling documentation","interactions":[],"lastModifiedDate":"2021-05-27T14:04:05.646141","indexId":"70220879","displayToPublicDate":"2021-05-27T08:51:14","publicationYear":"2021","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":8761,"text":"Wisconsin DNR Technical Report","active":true,"publicationSubtype":{"id":2}},"title":"Appendix C: Central sands lakes study technical report: Modeling documentation","docAbstract":"<p>This report provides the necessary documentation of the numerical models developed for the Central Sands Lake study in central Wisconsin and will be included as a technical appendix in the report to the Wisconsin State Legislature by the Wisconsin Department of Natural Resources (WDNR) in response to 2017 Wisconsin Act 10. This legislation directed WDNR to determine whether existing and potential groundwater withdrawals are causing or are likely to cause significant reduction of mean seasonal water levels at Pleasant Lake, Long Lake, and Plainfield Lake (s. 281.34(7m)(2)(b), Wis. Stats.) in Waushara County, Wisconsin. To evaluate the potential hydrologic connection between groundwater withdrawals and the nearby study lakes, hydrologic models were created that focused on the lakes of interest and yet were large enough to cover a broad enough region to extend to the major hydrologic boundaries of the natural flow system. The areas near the lakes require finer-scale grid discretization (or spacing) to better represent the lakes and streams in the model, but also need to cover a large enough area to include the groundwater withdrawal locations that have the potential to cause reduction in water levels in the lakes. To accomplish these goals, three groundwater models were created: a regional model extending to major hydrologic boundaries; and two inset models, inheriting boundaries from the regional model but focused near the lakes. Each of the inset models, in turn, included a detailed area close to the lakes surrounded by an area at the same spatial scale as the regional model (Figure 1). </p><p>To support WDNR in evaluating the connection between groundwater withdrawals and lake levels, a representative time period was required over which to compare land use with and without irrigated agriculture and for WDNR to evaluate potential lake stage and flux changes related to irrigated agriculture. WDNR chose the climate period of 1981-2018 to be representative of a typical period and provided two land use scenarios—one with no irrigated agriculture and one with assumed crop rotations similar to current conditions—to simulate with groundwater models to, then, compare lake responses with. As a result, simulations over this climate record are not intended to recreate the history of 1981-2018 because land use changed over that time. These runs are, instead, intended to provide a basis on which to compare land use with and without irrigation-related groundwater withdrawals based on the current arrangement of land use and a varied climatic record. Groundwater withdrawals focused on irrigated-agriculture-related water use because greater than 95% of groundwater withdrawal in the two inset models around the study lakes is for irrigated agriculture water use. </p><p>The period of 2012-2018 was used for parameter estimation (synonymously referred to as “history matching”) for the groundwater models. This time period was chosen because it includes the most complete water use records to simulate groundwater withdrawals. History matching was performed using groundwater elevations, lake stages, and streamflow observations over the 2012-2018 time period and processed observations derived from those raw data. </p><p>Climatic data were incorporated into the model using a soil-water balance approach. A soil water balance model was constructed at the scale of the regional groundwater model to both calculate recharge based on land use and climate, and in the long-term climate-period runs, to estimate water use required by irrigated agriculture to apply as well boundary conditions in the groundwater model in the absence of reported water use values over that period.</p>","language":"English","publisher":"Wisconsin Department of Natural Resources","usgsCitation":"Fienen, M., Haserodt, M.J., Leaf, A.T., and Westenbroek, S., 2021, Appendix C: Central sands lakes study technical report: Modeling documentation: Wisconsin DNR Technical Report, ix, 137 p.","productDescription":"ix, 137 p.","ipdsId":"IP-127829","costCenters":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":386002,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":385990,"type":{"id":15,"text":"Index Page"},"url":"https://dnr.wisconsin.gov/topic/Wells/HighCap/CSLStudy.html"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Central Sands region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.78851318359375,\n              43.58834891179792\n            ],\n            [\n              -89.29962158203125,\n              43.57641143300888\n            ],\n            [\n              -89.219970703125,\n              43.75919263886012\n            ],\n            [\n              -89.54132080078125,\n              44.471031231561845\n            ],\n            [\n              -89.7967529296875,\n              44.41808794374846\n            ],\n            [\n              -89.85443115234375,\n              44.33367180085156\n            ],\n            [\n              -89.98901367187499,\n              44.11125397357155\n            ],\n            [\n              -90.01373291015625,\n              44.03232064275081\n            ],\n            [\n              -89.96978759765625,\n              43.878097874251736\n            ],\n            [\n              -89.8187255859375,\n              43.71156424665851\n            ],\n            [\n              -89.78851318359375,\n              43.58834891179792\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fienen, Michael N. 0000-0002-7756-4651","orcid":"https://orcid.org/0000-0002-7756-4651","contributorId":245632,"corporation":false,"usgs":true,"family":"Fienen","given":"Michael N.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haserodt, Megan J. 0000-0002-8304-090X mhaserodt@usgs.gov","orcid":"https://orcid.org/0000-0002-8304-090X","contributorId":174791,"corporation":false,"usgs":true,"family":"Haserodt","given":"Megan","email":"mhaserodt@usgs.gov","middleInitial":"J.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leaf, Andrew T. 0000-0001-8784-4924 aleaf@usgs.gov","orcid":"https://orcid.org/0000-0001-8784-4924","contributorId":5156,"corporation":false,"usgs":true,"family":"Leaf","given":"Andrew","email":"aleaf@usgs.gov","middleInitial":"T.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816549,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Westenbroek, Stephen, M. 0000-0002-6284-8643","orcid":"https://orcid.org/0000-0002-6284-8643","contributorId":206429,"corporation":false,"usgs":true,"family":"Westenbroek","given":"Stephen, M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816550,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70230038,"text":"70230038 - 2021 - Assessing the uncertainties in climatic estimates based on vegetation assemblages: Examples from modern vegetation assemblages in the American Southwest","interactions":[],"lastModifiedDate":"2022-03-29T18:57:47.258287","indexId":"70230038","displayToPublicDate":"2021-05-27T08:35:57","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Assessing the uncertainties in climatic estimates based on vegetation assemblages: Examples from modern vegetation assemblages in the American Southwest","docAbstract":"<p id=\"abspara0010\"><span>Assemblages of fossil plant remains have been widely used to reconstruct past climatic conditions, usually through the application of methods that involve either finding vegetation analogues on the modern landscape (and using the modern associated climatic values as the basis for an estimate) or using the modern climatic ranges of individual taxa in an assemblage to determine the range of a given climate variable that would allow these plant taxa to live together. Although these approaches are relatively straightforward, it is difficult to assess the uncertainties associated with each approach, particularly in regard to their application to plant macrofossil assemblages. To explore the uncertainty that may arise from inaccuracy and imprecision in climate reconstructions and from ecological considerations we used variants of both approaches to estimate climate from two data sets of modern vegetation assemblages from the southwestern United States: (1) 1752 gridded “virtual plant assemblages” based on plant range maps that provide uniform spatial coverage of the presence or absence of major&nbsp;woody plant&nbsp;taxa across the study area; and (2) 43 modern packrat (</span><i>Neotoma</i><span>&nbsp;</span>spp.) midden presence-absence assemblages that are similar to fossil midden assemblages. By comparing observed and estimated climate values, we evaluated the quality of the climate estimates, identified sources of uncertainty, and characterized the nature and magnitude of the effects of these uncertainties on the climate estimates.</p><p id=\"abspara0015\">Uncertainties in estimating climate from vegetation assemblages arise because any given plant taxon (or assemblage) must have the resiliency to survive a range of climatic variability, and because of the strong intercorrelations among climatic variables in the modern climate data. Additional sources of uncertainty in climate estimates from plant assemblages include: (1) the modern climate and plant distribution data that are selected as the basis for estimation; (2) the particular quantitative approach that is used to estimate climate; (3) the sufficiency of the number of taxa in the analysis for providing an unbiased representation of the vegetation community as it existed for each time period in the analysis; and, (4) the location of the assemblage on the climatic and<span>&nbsp;</span>environmental gradients<span>&nbsp;</span>in the calibration data set for each climate variable under consideration.</p><p id=\"abspara0020\">We conclude that vegetation assemblages can provide valid and reproducible estimates of climatic variables and that the primary trends and mapped patterns in the observed climate data can be reconstructed from such estimates. However, many factors may affect the quality of an estimate from a given plant assemblage, including aspects of data selection, data adequacy, methodologies, and the location of the assemblage site relative to gradients in the base climate data. It is particularly difficult to accurately estimate extreme values in the observed climate data, because estimated values from either end of an observed climate gradient necessarily “move toward the middle” of the gradient. In addition, the interval chosen to represent modern climate (here we used 1961 to 1990) may have a large impact on the size of the estimated difference between modern and past climate at a given site.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.quascirev.2021.106880","usgsCitation":"Thompson, R.S., Anderson, K., Pelltier, R.T., Strickland, L.E., Shafer, S., and Bartlein, P.J., 2021, Assessing the uncertainties in climatic estimates based on vegetation assemblages: Examples from modern vegetation assemblages in the American Southwest: Quaternary Science Reviews, v. 262, 106880, 27 p., https://doi.org/10.1016/j.quascirev.2021.106880.","productDescription":"106880, 27 p.","ipdsId":"IP-100351","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":436335,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9CKCP22","text":"USGS data release","linkHelpText":"Data release for Assessing the Uncertainties in Climatic Estimates Based on Vegetation Assemblages: Examples from Modern Vegetation Assemblages in the American Southwest"},{"id":397596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Colorado, Nevada, New Mexico, Texas, Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.3046875,\n              29.84064389983441\n            ],\n            [\n              -104.765625,\n              32.32427558887655\n            ],\n            [\n              -106.435546875,\n              35.71083783530009\n            ],\n            [\n              -106.787109375,\n              37.75334401310656\n            ],\n           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rthompson@usgs.gov","orcid":"https://orcid.org/0000-0001-9287-2954","contributorId":891,"corporation":false,"usgs":true,"family":"Thompson","given":"Robert","email":"rthompson@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":838827,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Katherine H 0000-0003-2677-6109","orcid":"https://orcid.org/0000-0003-2677-6109","contributorId":289266,"corporation":false,"usgs":false,"family":"Anderson","given":"Katherine H","affiliations":[{"id":62090,"text":"Institute of Arctic and Alpine Research, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":838828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pelltier, Richard T. 0000-0001-8322-7961 rtpelltier@usgs.gov","orcid":"https://orcid.org/0000-0001-8322-7961","contributorId":4683,"corporation":false,"usgs":true,"family":"Pelltier","given":"Richard","email":"rtpelltier@usgs.gov","middleInitial":"T.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":838829,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Strickland, Laura E. 0000-0002-1958-7273 lstrickland@usgs.gov","orcid":"https://orcid.org/0000-0002-1958-7273","contributorId":4682,"corporation":false,"usgs":true,"family":"Strickland","given":"Laura","email":"lstrickland@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":838830,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shafer, Sarah 0000-0003-3739-2637 sshafer@usgs.gov","orcid":"https://orcid.org/0000-0003-3739-2637","contributorId":149866,"corporation":false,"usgs":true,"family":"Shafer","given":"Sarah","email":"sshafer@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":838831,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bartlein, Patrick J. 0000-0001-7657-5685","orcid":"https://orcid.org/0000-0001-7657-5685","contributorId":211587,"corporation":false,"usgs":false,"family":"Bartlein","given":"Patrick","email":"","middleInitial":"J.","affiliations":[{"id":33397,"text":"U of Oregon","active":true,"usgs":false}],"preferred":false,"id":838832,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70238937,"text":"70238937 - 2021 - Ten simple rules for productive lab meetings","interactions":[],"lastModifiedDate":"2022-12-19T14:19:07.541434","indexId":"70238937","displayToPublicDate":"2021-05-27T08:12:46","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5727,"text":"PLOS Computational Biology","active":true,"publicationSubtype":{"id":10}},"title":"Ten simple rules for productive lab meetings","docAbstract":"<p><span>The aim of this article is to delineate 10 simple rules on how to achieve productive lab meetings. We use the term “meeting” interchangeably to represent both the single meeting event and the overarching concept of the recurring meeting. In this article we speak from our experience, as a lab group at the University of Massachusetts that meets regularly (</span>Fig 1<span>). Although the rules are mostly tailored toward academic or research institution settings, insights can be gained for other contexts. We believe these rules are applicable across a diverse set of labs and lab structures. For example, while many members of our current lab have remained constant for many years, the lab composition has changed as various undergraduate students, graduate students, postdoctoral fellow, visiting professors, and other faculty have joined and/or moved on. Throughout these experiences, lab rules, presented in modified form here, proved flexible and adaptable enough to be useful in helping guide productive lab meetings. Note that this article is written for principal investigator/s (PI), students, postdocs, and other lab members; it takes the whole lab group to succeed. The key to planning productive lab meetings boils down to discussing and determining as a team the answers to why, who, what, where, when, and how: Why are lab meetings important for the functioning of the lab? Who will participate? What will be the focus of lab meetings? When and where should the lab meetings occur? How should each meeting be structured and carried out so that the goals and objectives of the lab and its participants are met?</span></p>","language":"English","publisher":"Public Library of Science","doi":"10.1371/journal.pcbi.1008953","usgsCitation":"Golden, N., Devarajan, K., Balantic, C., Drake, J., Hallworth, M.T., and Morelli, T.L., 2021, Ten simple rules for productive lab meetings: PLOS Computational Biology, v. 17, no. 5, e1008953, 13 p., https://doi.org/10.1371/journal.pcbi.1008953.","productDescription":"e1008953, 13 p.","ipdsId":"IP-125473","costCenters":[{"id":5080,"text":"Northeast Climate Adaptation Science Center","active":true,"usgs":true}],"links":[{"id":452113,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pcbi.1008953","text":"Publisher Index Page"},{"id":410702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"5","noUsgsAuthors":false,"publicationDate":"2021-05-27","publicationStatus":"PW","contributors":{"editors":[{"text":"Schwartz, Russell","contributorId":300129,"corporation":false,"usgs":false,"family":"Schwartz","given":"Russell","email":"","affiliations":[{"id":12943,"text":"Carnegie Mellon University","active":true,"usgs":false}],"preferred":false,"id":859459,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Golden, Nigel","contributorId":300012,"corporation":false,"usgs":false,"family":"Golden","given":"Nigel","email":"","affiliations":[{"id":65000,"text":"University of Massachusetts, Department of Environmental Conservation","active":true,"usgs":false}],"preferred":false,"id":859268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Devarajan, Kadambari","contributorId":236828,"corporation":false,"usgs":false,"family":"Devarajan","given":"Kadambari","email":"","affiliations":[],"preferred":false,"id":859269,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balantic, Cathleen","contributorId":275317,"corporation":false,"usgs":false,"family":"Balantic","given":"Cathleen","affiliations":[{"id":13253,"text":"University of Vermont","active":true,"usgs":false}],"preferred":false,"id":859270,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Drake, Joseph","contributorId":300015,"corporation":false,"usgs":false,"family":"Drake","given":"Joseph","email":"","affiliations":[{"id":36396,"text":"University of Massachusetts","active":true,"usgs":false}],"preferred":false,"id":859271,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hallworth, Michael T.","contributorId":213805,"corporation":false,"usgs":false,"family":"Hallworth","given":"Michael","email":"","middleInitial":"T.","affiliations":[{"id":38879,"text":"National Zoological Park, Migratory Bird Center","active":true,"usgs":false}],"preferred":false,"id":859272,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Morelli, Toni Lyn 0000-0001-5865-5294 tmorelli@usgs.gov","orcid":"https://orcid.org/0000-0001-5865-5294","contributorId":197458,"corporation":false,"usgs":true,"family":"Morelli","given":"Toni","email":"tmorelli@usgs.gov","middleInitial":"Lyn","affiliations":[{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":5080,"text":"Northeast Climate Adaptation Science Center","active":true,"usgs":true}],"preferred":true,"id":859273,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70221154,"text":"70221154 - 2021 - Transient disease dynamics across ecological scales","interactions":[],"lastModifiedDate":"2022-01-06T17:10:13.809411","indexId":"70221154","displayToPublicDate":"2021-05-27T08:12:42","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3592,"text":"Theoretical Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Transient disease dynamics across ecological scales","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Analyses of transient dynamics are critical to understanding infectious disease transmission and persistence. Identifying and predicting transients across scales, from within-host to community-level patterns, plays an important role in combating ongoing epidemics and mitigating the risk of future outbreaks. Moreover, greater emphases on non-asymptotic processes will enable timely evaluations of wildlife and human diseases and lead to improved surveillance efforts, preventive responses, and intervention strategies. Here, we explore the contributions of transient analyses in recent models spanning the fields of epidemiology, movement ecology, and parasitology. In addition to their roles in predicting epidemic patterns and endemic outbreaks, we explore transients in the contexts of pathogen transmission, resistance, and avoidance at various scales of the ecological hierarchy. Examples illustrate how (i) transient movement dynamics at the individual host level can modify opportunities for transmission events over time;&nbsp;(ii) within-host energetic processes often lead to transient dynamics in immunity, pathogen load, and transmission potential; (iii) transient connectivity between discrete populations in response to environmental factors and outbreak dynamics can affect disease spread across spatial networks; and (iv) increasing species richness in a community can provide transient protection to individuals against infection. Ultimately, we suggest that transient analyses offer deeper insights and raise new, interdisciplinary questions for disease research, consequently broadening the applications of dynamical models for outbreak preparedness and management.</p></div></div>","language":"English","publisher":"Springer","doi":"10.1007/s12080-021-00514-w","usgsCitation":"Tao, Y., Hite, J.L., Lafferty, K.D., Earn, D.J., and Bharti, N., 2021, Transient disease dynamics across ecological scales: Theoretical Ecology, v. 14, p. 625-640, https://doi.org/10.1007/s12080-021-00514-w.","productDescription":"16 p.","startPage":"625","endPage":"640","ipdsId":"IP-129495","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":452115,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s12080-021-00514-w","text":"Publisher Index Page"},{"id":386173,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","noUsgsAuthors":false,"publicationDate":"2021-05-27","publicationStatus":"PW","contributors":{"authors":[{"text":"Tao, Yun","contributorId":259235,"corporation":false,"usgs":false,"family":"Tao","given":"Yun","email":"","affiliations":[{"id":52331,"text":"Intelligence Community Postdoctoral Research Fellowship Program, Department of Ecology, Evolution and Marine Biology, University of California, Santa Barbara, CA, 93106, USA","active":true,"usgs":false}],"preferred":false,"id":816871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hite, Jessica L","contributorId":259236,"corporation":false,"usgs":false,"family":"Hite","given":"Jessica","email":"","middleInitial":"L","affiliations":[{"id":52333,"text":"School of Veterinary Medicine, Department of Pathobiological Sciences, University of Wisconsin, Madison, WI, 53706, USA","active":true,"usgs":false}],"preferred":false,"id":816872,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":816873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Earn, David J D","contributorId":259237,"corporation":false,"usgs":false,"family":"Earn","given":"David","email":"","middleInitial":"J D","affiliations":[{"id":52334,"text":"Department of Mathematics and Statistics, McMaster University, Hamilton, ON, L8S 4K1, Canada","active":true,"usgs":false}],"preferred":false,"id":816874,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bharti, Nita","contributorId":259238,"corporation":false,"usgs":false,"family":"Bharti","given":"Nita","email":"","affiliations":[{"id":52336,"text":"Department of Biology Center for Infectious Disease Dynamics, Penn State University, University Park, PA, 16802, USA","active":true,"usgs":false}],"preferred":false,"id":816875,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70223176,"text":"70223176 - 2021 - Enhancing Great Lakes coastal ecosystems research by initiating engagement between scientists and decision-makers","interactions":[],"lastModifiedDate":"2021-08-17T13:19:21.637383","indexId":"70223176","displayToPublicDate":"2021-05-27T08:11:26","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Enhancing Great Lakes coastal ecosystems research by initiating engagement between scientists and decision-makers","docAbstract":"<p><span>A disconnect between scientific research and environmental management communities can be a detriment to both. In the case of Great Lakes coastal ecosystems, which are inherently complex and subject to uncertain effects of future climatic, environmental, and anthropogenic drivers, greater collaboration could be beneficial to their sustainability. We capture the challenges and opportunities identified by a scientist/decision-maker co-production workshop focused on the future environmental quality of Great Lakes coastal wetlands. We explain our path through the stakeholder workshop process, our challenges in translating meeting outcomes into actionable items, and lessons learned to bridge gaps between scientists and decision-makers. Additionally, we determine topics and directions identified by decision-makers that can be modeled with existing technologies and others that require further research. These topics may be incorporated into future research efforts and could serve as a shortlist of research priorities that were identified by decision-makers working with coastal wetland issues. Based on lessons learned during and after the workshop, we provide suggestions for bridging the gap between researchers and decision-makers, including sustained engagement between these groups and improved interaction through the beginning, duration, and end of research and/or management efforts.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jglr.2021.04.018","usgsCitation":"Weinstein, C.B., Bourgeau-Chavez, L., Martin, S.L., Currie, W.S., Grantham, K., Hamlin, Q.F., Hyndman, D.W., Kowalski, K., Martina, J.P., and Pearsall, D., 2021, Enhancing Great Lakes coastal ecosystems research by initiating engagement between scientists and decision-makers: Journal of Great Lakes Research, v. 47, no. 4, p. 1235-1240, https://doi.org/10.1016/j.jglr.2021.04.018.","productDescription":"6 p.","startPage":"1235","endPage":"1240","ipdsId":"IP-125315","costCenters":[{"id":324,"text":"Great Lakes Science 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0000-0001-7127-279X","orcid":"https://orcid.org/0000-0001-7127-279X","contributorId":220963,"corporation":false,"usgs":false,"family":"Bourgeau-Chavez","given":"Laura","email":"","affiliations":[{"id":34530,"text":"Michigan Tech Research Institute","active":true,"usgs":false}],"preferred":false,"id":821247,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, S. L.","contributorId":264243,"corporation":false,"usgs":false,"family":"Martin","given":"S.","email":"","middleInitial":"L.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":821248,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Currie, W. S.","contributorId":264245,"corporation":false,"usgs":false,"family":"Currie","given":"W.","email":"","middleInitial":"S.","affiliations":[{"id":37387,"text":"University of Michigan","active":true,"usgs":false}],"preferred":false,"id":821249,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grantham, K.","contributorId":264247,"corporation":false,"usgs":false,"family":"Grantham","given":"K.","email":"","affiliations":[{"id":54411,"text":"Southeast Michigan Council of Governments","active":true,"usgs":false}],"preferred":false,"id":821250,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hamlin, Q. F.","contributorId":264248,"corporation":false,"usgs":false,"family":"Hamlin","given":"Q.","email":"","middleInitial":"F.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":821251,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hyndman, David W","contributorId":264249,"corporation":false,"usgs":false,"family":"Hyndman","given":"David","email":"","middleInitial":"W","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":821252,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kowalski, Kurt P. 0000-0002-8424-4701 kkowalski@usgs.gov","orcid":"https://orcid.org/0000-0002-8424-4701","contributorId":3768,"corporation":false,"usgs":true,"family":"Kowalski","given":"Kurt P.","email":"kkowalski@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":821253,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Martina, J. P.","contributorId":264250,"corporation":false,"usgs":false,"family":"Martina","given":"J.","email":"","middleInitial":"P.","affiliations":[{"id":6677,"text":"Texas State University","active":true,"usgs":false}],"preferred":false,"id":821254,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Pearsall, D.","contributorId":264252,"corporation":false,"usgs":false,"family":"Pearsall","given":"D.","email":"","affiliations":[{"id":7041,"text":"The Nature Conservancy","active":true,"usgs":false}],"preferred":false,"id":821255,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70223137,"text":"70223137 - 2021 - Impact of SST and surface waves on Hurricane Florence (2018): A coupled modeling investigation","interactions":[],"lastModifiedDate":"2021-09-21T13:11:40.385044","indexId":"70223137","displayToPublicDate":"2021-05-27T07:58:11","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3735,"text":"Weather and Forecasting","active":true,"publicationSubtype":{"id":10}},"title":"Impact of SST and surface waves on Hurricane Florence (2018): A coupled modeling investigation","docAbstract":"<div class=\"component component-content-item component-content-summary abstract_or_excerpt\"><div class=\"content-box box border-bottom border-bottom-inherit border-bottom-inherit no-padding no-header vertical-margin-bottom null\"><div class=\"content-box-body null\"><p>Hurricane Florence (2018) devastated the coastal communities of the Carolinas through heavy rainfall that resulted in massive flooding. Florence was characterized by an abrupt reduction in intensity (Saffir-Simpson Category 4 to Category 1) just prior to landfall and synoptic-scale interactions that stalled the storm over the Carolinas for several days. We conducted a series of numerical modeling experiments in coupled and uncoupled configurations to examine the impact of sea surface temperature (SST) and ocean waves on storm characteristics. In addition to experiments using a fully coupled atmosphere-ocean-wave model, we introduced the capability of the atmospheric model to modulate wind stress and surface fluxes by oceanwaves through data from an uncoupled wave model. We examined these experiments by comparing track, intensity, strength, SST, storm structure, wave height, surface roughness, heat fluxes, and precipitation in order to determine the impacts of resolving ocean conditions with varying degrees of coupling. We found differences in the storm’s intensity and strength, with the best correlation coefficient of intensity (r=0.89) and strength (r=0.95) coming from the fully-coupled simulations. Further analysis into surface roughness parameterizations added to the atmospheric model revealed differences in the spatial distribution and magnitude of the largest roughness lengths. Adding ocean andwave features to the model further modified the fluxes due to more realistic cooling beneath the stormwhich in turn modified the precipitation field. Our experiments highlight significant differences in how air-sea processes impact hurricane modeling. The storm characteristics of track, intensity, strength, and precipitation at landfall are crucial to predictability and forecasting of future landfalling hurricanes.</p></div></div></div>","language":"English","publisher":"American Meteorological Society","doi":"10.1175/WAF-D-20-0171.1","usgsCitation":"Zambon, J., He, R., Warner, J.C., and Hegermiller, C., 2021, Impact of SST and surface waves on Hurricane Florence (2018): A coupled modeling investigation: Weather and Forecasting, v. 36, no. 5, p. 1713-1734, https://doi.org/10.1175/WAF-D-20-0171.1.","productDescription":"22 p.","startPage":"1713","endPage":"1734","ipdsId":"IP-131401","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":452119,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/waf-d-20-0171.1","text":"Publisher Index Page"},{"id":387898,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zambon, Joseph","contributorId":264200,"corporation":false,"usgs":false,"family":"Zambon","given":"Joseph","affiliations":[{"id":54401,"text":"Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, North Carolina","active":true,"usgs":false}],"preferred":false,"id":821095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"He, Ruoying 0000-0001-6158-2292","orcid":"https://orcid.org/0000-0001-6158-2292","contributorId":202189,"corporation":false,"usgs":false,"family":"He","given":"Ruoying","email":"","affiliations":[],"preferred":false,"id":821096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":258015,"corporation":false,"usgs":true,"family":"Warner","given":"John","email":"jcwarner@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":821097,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hegermiller, Christie 0000-0002-6383-7508 chegermiller@usgs.gov","orcid":"https://orcid.org/0000-0002-6383-7508","contributorId":149010,"corporation":false,"usgs":true,"family":"Hegermiller","given":"Christie","email":"chegermiller@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":821098,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70221099,"text":"70221099 - 2021 - Long-term shedding from fully convalesced individuals indicates that Pacific herring are a reservoir for viral hemorrhagic septicemia virus","interactions":[],"lastModifiedDate":"2021-06-02T12:13:11.151017","indexId":"70221099","displayToPublicDate":"2021-05-27T07:10:57","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1396,"text":"Diseases of Aquatic Organisms","active":true,"publicationSubtype":{"id":10}},"title":"Long-term shedding from fully convalesced individuals indicates that Pacific herring are a reservoir for viral hemorrhagic septicemia virus","docAbstract":"<p><span>Processes that allow viral hemorrhagic septicemia (VHS) virus to persist in the marine environment remain enigmatic, owing largely to the presence of covert and cryptic infections in marine fishes during typical sub-epizootic periods. As such, marine host reservoirs for VHS virus have not been fully demonstrated, nor have the mechanism(s) by which infected hosts contribute to virus perpetuation and transmission. Here, we demonstrate that after surviving VHS, convalesced Pacific herring continue to shed virus at a low rate for extended periods. Further, exposure of previously naïve conspecific sentinels to this shed virus can result in infections for at least 6 mo after cessation of overt disease. This transmission mechanism was not necessarily dependent on the magnitude of the disease outbreak, as prolonged transmission occurred from 2 groups of donor herring that experienced cumulative mortalities of 4 and 29%. The results further suggest that the virus persists in association with the gills of fully recovered individuals, and long-term viral shedding or shedding relapses are related to cooler or decreasing water temperatures. These results provide support for a new VHS virus perpetuation paradigm in the marine environment, whereby the virus can be maintained in convalesced survivors and trafficked from these carriers to sympatric susceptible individuals.</span></p>","language":"English","publisher":"Inter-Research","doi":"10.3354/dao03595","usgsCitation":"Hershberger, P., MacKenzie, A., Gregg, J.L., Wilmot, M.D., Powers, R., and Purcell, M.K., 2021, Long-term shedding from fully convalesced individuals indicates that Pacific herring are a reservoir for viral hemorrhagic septicemia virus: Diseases of Aquatic Organisms, v. 144, p. 245-252, https://doi.org/10.3354/dao03595.","productDescription":"8 p.","startPage":"245","endPage":"252","ipdsId":"IP-123287","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":386111,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"144","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hershberger, Paul 0000-0002-2261-7760","orcid":"https://orcid.org/0000-0002-2261-7760","contributorId":203322,"corporation":false,"usgs":true,"family":"Hershberger","given":"Paul","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":816761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacKenzie, Ashley 0000-0002-7402-7877 amackenzie@usgs.gov","orcid":"https://orcid.org/0000-0002-7402-7877","contributorId":150817,"corporation":false,"usgs":true,"family":"MacKenzie","given":"Ashley","email":"amackenzie@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":816762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gregg, Jacob L. 0000-0001-5328-5482 jgregg@usgs.gov","orcid":"https://orcid.org/0000-0001-5328-5482","contributorId":203912,"corporation":false,"usgs":true,"family":"Gregg","given":"Jacob","email":"jgregg@usgs.gov","middleInitial":"L.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":816763,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilmot, M. D.","contributorId":259184,"corporation":false,"usgs":false,"family":"Wilmot","given":"M.","email":"","middleInitial":"D.","affiliations":[{"id":36303,"text":"unknown","active":true,"usgs":false}],"preferred":false,"id":816764,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Powers, Rachel L. 0000-0001-6901-4361","orcid":"https://orcid.org/0000-0001-6901-4361","contributorId":190182,"corporation":false,"usgs":true,"family":"Powers","given":"Rachel L.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":816765,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Purcell, Maureen K. 0000-0003-0154-8433 mpurcell@usgs.gov","orcid":"https://orcid.org/0000-0003-0154-8433","contributorId":168475,"corporation":false,"usgs":true,"family":"Purcell","given":"Maureen","email":"mpurcell@usgs.gov","middleInitial":"K.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":816766,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70222119,"text":"70222119 - 2021 - N supply mediates the radiative balance of N2O emissions and CO2 sequestration driven by N-fixing vs. non-fixing trees","interactions":[],"lastModifiedDate":"2021-08-17T15:11:39.429132","indexId":"70222119","displayToPublicDate":"2021-05-27T06:47:06","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"N supply mediates the radiative balance of N<sub>2</sub>O emissions and CO<sub>2</sub> sequestration driven by N-fixing vs. non-fixing trees","title":"N supply mediates the radiative balance of N2O emissions and CO2 sequestration driven by N-fixing vs. non-fixing trees","docAbstract":"<p><span>Forests are a significant CO</span><sub>2</sub><span>&nbsp;sink. However, CO</span><sub>2</sub><span>&nbsp;sequestration in forests is radiatively offset by emissions of nitrous oxide (N</span><sub>2</sub><span>O), a potent greenhouse gas, from forest soils. Reforestation, an important strategy for mitigating climate change, has focused on maximizing CO</span><sub>2</sub><span>&nbsp;sequestration in plant biomass without integrating N</span><sub>2</sub><span>O emissions from soils. Although nitrogen (N)-fixing trees are often recommended for reforestation because of their rapid growth on N-poor soil, they can stimulate significant N</span><sub>2</sub><span>O emissions from soils. Here, we first used a field experiment to show that a N-fixing tree (</span><i>Robinia pseudoacacia</i><span>) initially mitigated climate change more than a non-fixing tree (</span><i>Betula nigra</i><span>). We then used our field data to parameterize a theoretical model to investigate these effects over time. Under lower N supply, N-fixers continued to mitigate climate change more than non-fixers by overcoming N limitation of plant growth. However, under higher N supply, N-fixers ultimately mitigated climate change less than non-fixers by enriching soil N and stimulating N</span><sub>2</sub><span>O emissions from soils. These results have implications for reforestation, suggesting that N-fixing trees are more effective at mitigating climate change at lower N supply, whereas non-fixing trees are more effective at mitigating climate change at higher N supply.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/ecy.3414","usgsCitation":"Kou-Giesbrecht, S., Funk, J.L., Perakis, S.S., Wolf, A.A., and Menge, D., 2021, N supply mediates the radiative balance of N2O emissions and CO2 sequestration driven by N-fixing vs. non-fixing trees: Ecology, v. 102, no. 8, e03414, 8 p., https://doi.org/10.1002/ecy.3414.","productDescription":"e03414, 8 p.","ipdsId":"IP-123004","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":452122,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/ecy.3414","text":"Publisher Index Page"},{"id":387284,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Black Rock Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.0584945678711,\n              41.3791271230665\n            ],\n            [\n              -73.99017333984375,\n              41.3791271230665\n            ],\n            [\n              -73.99017333984375,\n              41.41737138589576\n            ],\n            [\n              -74.0584945678711,\n              41.41737138589576\n            ],\n            [\n              -74.0584945678711,\n              41.3791271230665\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"102","issue":"8","noUsgsAuthors":false,"publicationDate":"2021-07-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Kou-Giesbrecht, Sian 0000-0002-4086-0561","orcid":"https://orcid.org/0000-0002-4086-0561","contributorId":261258,"corporation":false,"usgs":false,"family":"Kou-Giesbrecht","given":"Sian","email":"","affiliations":[{"id":52786,"text":"Columbia U","active":true,"usgs":false}],"preferred":false,"id":819602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Funk, Jennifer L.","contributorId":260668,"corporation":false,"usgs":false,"family":"Funk","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[{"id":7214,"text":"University of California, Davis","active":true,"usgs":false}],"preferred":false,"id":819603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perakis, Steven S. 0000-0003-0703-9314 sperakis@usgs.gov","orcid":"https://orcid.org/0000-0003-0703-9314","contributorId":145528,"corporation":false,"usgs":true,"family":"Perakis","given":"Steven","email":"sperakis@usgs.gov","middleInitial":"S.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":819604,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wolf, Amelia A.","contributorId":190685,"corporation":false,"usgs":false,"family":"Wolf","given":"Amelia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":819605,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Menge, Duncan 0000-0003-4736-9844","orcid":"https://orcid.org/0000-0003-4736-9844","contributorId":241126,"corporation":false,"usgs":false,"family":"Menge","given":"Duncan","email":"","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":819606,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70220727,"text":"sir20215028 - 2021 - Flow characteristics and salinity patterns in tidal rivers within the northern Ten Thousand Islands, southwest Florida, water years 2007–19","interactions":[],"lastModifiedDate":"2021-05-27T11:52:45.64841","indexId":"sir20215028","displayToPublicDate":"2021-05-26T13:37:00","publicationYear":"2021","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2021-5028","displayTitle":"Flow Characteristics and Salinity Patterns in Tidal Rivers Within the Northern Ten Thousand Islands, Southwest Florida, Water Years 2007–19","title":"Flow characteristics and salinity patterns in tidal rivers within the northern Ten Thousand Islands, southwest Florida, water years 2007–19","docAbstract":"<p>Freshwater flow to the Ten Thousand Islands (TTI) estuary has been altered by the construction of the Tamiami Trail and construction of features in the now defunct Southern Golden Gate Estates development. This development included four associated canals that combine into the Faka Union Canal, which discharges into the TTI estuary. The Picayune Strand Restoration Project (PSRP) was initiated in 2007 to improve freshwater delivery to the TTI estuary by removing hundreds of miles of roads, emplacing hundreds of canal plugs, removing exotic vegetation, and constructing three pump stations. Quantifying the tributary flows and salinity patterns prior to, during, and after the restoration is essential to assessing the effectiveness of upstream restoration efforts. The U.S. Geological Survey, in cooperation with U.S. Army Corps of Engineers, initiated an ongoing study in 2006 to assess flow and salinity patterns in the TTI estuary. This is the second report by the U.S. Geological Survey describing flow characteristics and salinity patterns in the TTI area as part of the PSRP. This report describes flow characteristics and salinity patterns for the monitoring stations at Faka Union River, Pumpkin River, and East River and includes an assessment of salinity data from the Faka Union Boundary and Blackwater River water-quality stations for water years 2007–19. A water year is defined as the 12-month period from October 1 for any given year to September 30 of the following year.</p><p>Annual and monthly variations in flow and salinity are often related to variations in rainfall with high and low annual flows (and below average and above average salinities) typically occurring during years with high and low annual rainfall, respectively. Monthly flows typically begin increasing in June and peak in September. Over the study period, positive trends in rainfall-adjusted monthly flow were detected at Faka Union River and East River, whereas no significant trend in flow was detected at Pumpkin River. Faka Union River is the largest contributor of freshwater to the TTI estuary, providing over 80 percent of the annual freshwater inflow to the estuary. The Faka Union Canal is expected to be the largest contributor of freshwater because until the PSRP is completed, the Faka Union Canal receives substantial drainage from multiple canals, which is not the case for Pumpkin and East Rivers. East River was the second largest contributor, followed by Pumpkin River. East River is downstream of the Fakahatchee Stand, which is a larger contributing area than the current contributing area for Pumpkin River. Monthly mean salinities were lowest at Faka Union River and East River, indicating that they received a greater amount of freshwater than the stations to the west. Negative trends in rainfall-adjusted salinity monthly means were observed at all monitoring stations during the study period. Increased trends in flow and decreased trends in salinity are attributed to increases in flow from upstream canals.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20215028","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Booth, A.C., and Knight, T.M., 2021, Flow characteristics and salinity patterns in tidal rivers within the northern Ten Thousand Islands, southwest Florida, water years 2007–19: U.S. Geological Survey Scientific Investigations Report 2021–5028, 21 p., https://doi.org/10.3133/sir20215028.","productDescription":"vii, 21 p.","numberOfPages":"34","ipdsId":"IP-122818","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":385935,"rank":3,"type":{"id":34,"text":"Image Folder"},"url":"https://pubs.usgs.gov/sir/2021/5028/images"},{"id":385934,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2021/5028/sir20215028.pdf","text":"Report","size":"4.31 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2021–5028"},{"id":385933,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2021/5028/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Northern Ten Thousand Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.67304992675781,\n              25.852426562716428\n            ],\n            [\n              -81.47941589355469,\n              25.852426562716428\n            ],\n            [\n              -81.47941589355469,\n              25.972243398901558\n            ],\n            [\n              -81.67304992675781,\n              25.972243398901558\n            ],\n            [\n              -81.67304992675781,\n              25.852426562716428\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, <a data-mce-href=\"https://www2.usgs.gov/water/caribbeanflorida/index.html\" href=\"https://www2.usgs.gov/water/caribbeanflorida/index.html\">Caribbean-Florida Water Science Center (CFWSC)</a> <br><a data-mce-href=\"https://www.usgs.gov/\" href=\"https://www.usgs.gov/\">U.S. Geological Survey</a> <br>4446 Pet Lane, Suite 108 <br>Lutz, FL 33559</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Methods of Investigation</li><li>Annual and Monthly Variability and Trends in Rainfall</li><li>Flow Characteristics and Salinity Patterns in the Ten Thousand Islands</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"publishedDate":"2021-05-26","noUsgsAuthors":false,"publicationDate":"2021-05-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Booth, Amanda C. 0000-0002-2666-2366 acbooth@usgs.gov","orcid":"https://orcid.org/0000-0002-2666-2366","contributorId":258448,"corporation":false,"usgs":true,"family":"Booth","given":"Amanda C.","email":"acbooth@usgs.gov","affiliations":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"preferred":true,"id":816443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knight, Travis M. 0000-0002-0472-8141 tknight@usgs.gov","orcid":"https://orcid.org/0000-0002-0472-8141","contributorId":5433,"corporation":false,"usgs":true,"family":"Knight","given":"Travis","email":"tknight@usgs.gov","middleInitial":"M.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":816444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221849,"text":"70221849 - 2021 - Satellite remote sensing to assess cyanobacterial bloom frequency across the United States at multiple spatial scales","interactions":[],"lastModifiedDate":"2021-07-12T17:45:19.948532","indexId":"70221849","displayToPublicDate":"2021-05-26T12:41:34","publicationYear":"2021","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1456,"text":"Ecological Indicators","active":true,"publicationSubtype":{"id":10}},"title":"Satellite remote sensing to assess cyanobacterial bloom frequency across the United States at multiple spatial scales","docAbstract":"<p><span>Cyanobacterial blooms can have negative effects on human health and local ecosystems. Field monitoring of cyanobacterial blooms can be costly, but&nbsp;<a class=\"topic-link\" title=\"Learn more about satellite remote sensing from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/satellite-remote-sensing\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/satellite-remote-sensing\">satellite remote sensing</a>&nbsp;has shown utility for more efficient spatial and temporal monitoring across the United States. Here, satellite imagery was used to assess the annual frequency of surface cyanobacterial blooms, defined for each satellite pixel as the percentage of images for that pixel throughout the year exhibiting detectable&nbsp;</span><a class=\"topic-link\" title=\"Learn more about cyanobacteria from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/agricultural-and-biological-sciences/cyanobacteria\" data-mce-href=\"https://www.sciencedirect.com/topics/agricultural-and-biological-sciences/cyanobacteria\">cyanobacteria</a><span>. Cyanobacterial frequency was assessed across 2,196 large lakes in 46 states across the continental United States (CONUS) using imagery from the European Space Agency’s Ocean and Land Colour Instrument for the years 2017 through 2019. In 2019, across all satellite pixels considered, annual bloom frequency had a median value of 4% and a maximum value of 100%, the latter indicating that for those satellite pixels, a cyanobacterial bloom was detected by the&nbsp;<a class=\"topic-link\" title=\"Learn more about satellite sensor from ScienceDirect's AI-generated Topic Pages\" href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/satellite-sensor\" data-mce-href=\"https://www.sciencedirect.com/topics/earth-and-planetary-sciences/satellite-sensor\">satellite sensor</a>&nbsp;for every satellite image considered. In addition to annual pixel-scale cyanobacterial frequency, results were summarized at the lake- and state-scales by averaging annual pixel-scale results across each lake and state. For 2019, average annual lake-scale frequencies also had a maximum value of 100%, and Oregon and Ohio had the highest average annual state-scale frequencies at 65% and 52%. Pixel-scale frequency results can assist in identifying portions of a lake that are more prone to cyanobacterial blooms, while lake- and state-scale frequency results can assist in the prioritization of sampling resources and mitigation efforts. Satellite imagery is limited by the presence of snow and ice, as imagery collected in these conditions are quality flagged and discarded. Thus, annual bloom frequencies within nine climate regions were investigated to determine whether missing data biased results in climate regions more prone to snow and ice, given that their annual summaries would be weighted toward the summer months when cyanobacterial blooms tend to occur. Results were unbiased by the time period selected in most climate regions, but a large bias was observed for the Northwest Rockies and Plains climate region. Moderate biases were observed for the Ohio Valley and the Southeast climate regions. Finally, a clustering analysis was used to identify areas of high and low cyanobacterial frequency across CONUS based on average annual lake-scale cyanobacterial frequencies for 2019. Several clusters were identified that transcended state, watershed, and eco-regional boundaries. Combined with additional data, results from the clustering analysis may offer insight regarding large-scale drivers of cyanobacterial blooms.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ecolind.2021.107822","usgsCitation":"Coffer, M.M., Schaeffer, B., Salls, W.B., Urquhart, E., Loftin, K.A., Stumpf, R.P., Werdell, P.J., and Darling, J., 2021, Satellite remote sensing to assess cyanobacterial bloom frequency across the United States at multiple spatial scales: Ecological Indicators, v. 128, 107822, 12 p., https://doi.org/10.1016/j.ecolind.2021.107822.","productDescription":"107822, 12 p.","ipdsId":"IP-126524","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":452125,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.ecolind.2021.107822","text":"Publisher Index Page"},{"id":387135,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coffer, Megan M. 0000-0003-3188-4729","orcid":"https://orcid.org/0000-0003-3188-4729","contributorId":260857,"corporation":false,"usgs":false,"family":"Coffer","given":"Megan","email":"","middleInitial":"M.","affiliations":[{"id":37230,"text":"EPA","active":true,"usgs":false}],"preferred":false,"id":818980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaeffer, Blake 0000-0001-9794-3977","orcid":"https://orcid.org/0000-0001-9794-3977","contributorId":245603,"corporation":false,"usgs":false,"family":"Schaeffer","given":"Blake","email":"","affiliations":[{"id":37230,"text":"EPA","active":true,"usgs":false}],"preferred":false,"id":818981,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Salls, Wilson B. 0000-0001-7505-0828","orcid":"https://orcid.org/0000-0001-7505-0828","contributorId":260858,"corporation":false,"usgs":false,"family":"Salls","given":"Wilson","email":"","middleInitial":"B.","affiliations":[{"id":37230,"text":"EPA","active":true,"usgs":false}],"preferred":false,"id":818982,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Urquhart, Erin 0000-0001-7141-9499","orcid":"https://orcid.org/0000-0001-7141-9499","contributorId":260859,"corporation":false,"usgs":false,"family":"Urquhart","given":"Erin","email":"","affiliations":[{"id":38788,"text":"NASA","active":true,"usgs":false}],"preferred":false,"id":818983,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Loftin, Keith A. 0000-0001-5291-876X","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":221964,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","middleInitial":"A.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":818984,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stumpf, Richard P. 0000-0001-5531-6860","orcid":"https://orcid.org/0000-0001-5531-6860","contributorId":222357,"corporation":false,"usgs":false,"family":"Stumpf","given":"Richard","email":"","middleInitial":"P.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":818985,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Werdell, P. 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