{"pageNumber":"427","pageRowStart":"10650","pageSize":"25","recordCount":184569,"records":[{"id":70225169,"text":"70225169 - 2022 - A stable isotope record of late Quaternary hydrologic change in the northwestern Brooks Range, Alaska (eastern Beringia)","interactions":[],"lastModifiedDate":"2023-03-24T17:01:40.985278","indexId":"70225169","displayToPublicDate":"2021-09-21T07:54:09","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2437,"text":"Journal of Quaternary Science","active":true,"publicationSubtype":{"id":10}},"title":"A stable isotope record of late Quaternary hydrologic change in the northwestern Brooks Range, Alaska (eastern Beringia)","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>A submillennial-resolution record of lake water oxygen isotope composition (δ<sup>18</sup>O) from chironomid head capsules is presented from Burial Lake, northwest Alaska. The record spans the Last Glacial Maximum (LGM; ~20–16k cal a<span>&nbsp;</span><span class=\"smallCaps\">bp</span>) to the present and shows a series of large lake δ<sup>18</sup>O shifts (~5‰). Relatively low δ<sup>18</sup>O values occurred during a period covering the LGM, when the lake was a shallow, closed-basin pond. Higher values characterize deglaciation (~16–11.5k cal a<span>&nbsp;</span><span class=\"smallCaps\">bp</span>) when the lake was still closed but lake levels were higher. A rapid decline between ~11 and 10.5k cal a<span>&nbsp;</span><span class=\"smallCaps\">bp</span><span>&nbsp;</span>indicates that lake levels rose to overflowing. Lake δ<sup>18</sup>O values are interpreted to reflect the combined effects of changes in lake hydrology, growing season temperature and meteoric source water as well as large-scale environmental changes impacting this site, including opening of the Bering Strait and shifts in atmospheric circulation patterns related to ice-sheet dynamics. The results indicate significant shifts in precipitation minus evaporation across the late Pleistocene to early Holocene transition, which are consistent with temporal patterns of vegetation change and paludification. This study provides new perspectives on the paleohydrology of eastern Beringia concomitant with human migration and major turnover in megafaunal assemblages.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1002/jqs.3368","usgsCitation":"King, A.L., Anderson, L., Abbott, M., Edwards, M., Finkenbinder, M.S., Finney, B., and Wooller, M.J., 2022, A stable isotope record of late Quaternary hydrologic change in the northwestern Brooks Range, Alaska (eastern Beringia): Journal of Quaternary Science, v. 37, no. 5, p. 928-943, https://doi.org/10.1002/jqs.3368.","productDescription":"16 p.","startPage":"928","endPage":"943","ipdsId":"IP-126888","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":449701,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.osti.gov/biblio/1981417","text":"External Repository"},{"id":390562,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -167.6953125,\n              64.51064316846676\n            ],\n            [\n              -140.9765625,\n              64.51064316846676\n            ],\n            [\n              -140.9765625,\n              71.11677038645317\n            ],\n            [\n              -167.6953125,\n              71.11677038645317\n            ],\n            [\n              -167.6953125,\n              64.51064316846676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"2021-09-21","publicationStatus":"PW","contributors":{"authors":[{"text":"King, Amanda L.","contributorId":267771,"corporation":false,"usgs":false,"family":"King","given":"Amanda","email":"","middleInitial":"L.","affiliations":[{"id":55492,"text":"University of Alaska Fairbanks; Alaska Pacific University","active":true,"usgs":false}],"preferred":false,"id":825236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Lesleigh 0000-0002-5264-089X land@usgs.gov","orcid":"https://orcid.org/0000-0002-5264-089X","contributorId":436,"corporation":false,"usgs":true,"family":"Anderson","given":"Lesleigh","email":"land@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":825237,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abbott, Mark B.","contributorId":267772,"corporation":false,"usgs":false,"family":"Abbott","given":"Mark B.","affiliations":[{"id":12465,"text":"University of Pittsburgh","active":true,"usgs":false}],"preferred":false,"id":825238,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Mary","contributorId":267773,"corporation":false,"usgs":false,"family":"Edwards","given":"Mary","affiliations":[{"id":37955,"text":"University of Southampton","active":true,"usgs":false}],"preferred":false,"id":825239,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Finkenbinder, Matthew S.","contributorId":267774,"corporation":false,"usgs":false,"family":"Finkenbinder","given":"Matthew","email":"","middleInitial":"S.","affiliations":[{"id":55493,"text":"Wilkes University","active":true,"usgs":false}],"preferred":false,"id":825240,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Finney, Bruce P.","contributorId":267775,"corporation":false,"usgs":false,"family":"Finney","given":"Bruce P.","affiliations":[{"id":38154,"text":"Idaho State University","active":true,"usgs":false}],"preferred":false,"id":825241,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wooller, Matthew J.","contributorId":267776,"corporation":false,"usgs":false,"family":"Wooller","given":"Matthew","middleInitial":"J.","affiliations":[{"id":6752,"text":"University of Alaska Fairbanks","active":true,"usgs":false}],"preferred":false,"id":825242,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70224923,"text":"70224923 - 2022 - Elevated levels of radiocarbon in methane dissolved in seawater reveal likely local contamination from nuclear powered vessels","interactions":[],"lastModifiedDate":"2021-10-05T12:30:09.816315","indexId":"70224923","displayToPublicDate":"2021-09-21T07:27:33","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Elevated levels of radiocarbon in methane dissolved in seawater reveal likely local contamination from nuclear powered vessels","docAbstract":"<div id=\"ab0005\" class=\"abstract author\" lang=\"en\"><div id=\"as0005\"><p id=\"sp0030\">Measurements of the natural radiocarbon content of methane (<sup>14</sup>C-CH<sub>4</sub>) dissolved in seawater and freshwater have been used to investigate sources and dynamics of methane. However, during investigations along the Atlantic, Pacific, and Arctic Ocean Margins of the United States, as well as in the North American Great Lakes, some samples revealed highly elevated<span>&nbsp;</span><sup>14</sup>C-CH<sub>4</sub><span>&nbsp;</span>values, as much as 4–5 times above contemporary atmospheric<span>&nbsp;</span><sup>14</sup>C-CH<sub>4</sub><span>&nbsp;</span>levels. Natural production of the<span>&nbsp;</span><sup>14</sup>CH<sub>4</sub><span>&nbsp;isotopologue is too low to cause these observations nor can it explain the variations in location and depth. Numerous lab and field validation tests and blanks, as well as the relatively small number of samples that display these elevated values, all suggest that these signals are not derived from an unknown procedural issue. Here we suggest that the byproducts of&nbsp;nuclear power generation&nbsp;include localized discharges of the&nbsp;</span><sup>14</sup>CH<sub>4</sub><span>&nbsp;isotopologue into marine and&nbsp;aquatic environments, severely altering the measured&nbsp;</span><sup>14</sup>C-CH<sub>4</sub><span>&nbsp;</span>isotopic signals. Since several of our sample sites are distant from on-land nuclear powerplants, we conduct further calculations concluding that the most elevated anomalies in<span>&nbsp;</span><sup>14</sup>C-CH<sub>4</sub><span>&nbsp;</span>likely originate with discharge from nuclear-powered vessels.</p></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2021.150456","usgsCitation":"Joung, D., Ruppel, C.D., Southon, J., and Kessler, J.D., 2022, Elevated levels of radiocarbon in methane dissolved in seawater reveal likely local contamination from nuclear powered vessels: Science of the Total Environment, v. 806, no. 2, 150456, 8 p., https://doi.org/10.1016/j.scitotenv.2021.150456.","productDescription":"150456, 8 p.","ipdsId":"IP-122795","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":449702,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://www.osti.gov/biblio/1977626","text":"Publisher Index Page"},{"id":390234,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, North Carolina, Oregon, Virginia, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.5078125,\n              44.96479793033101\n            ],\n            [\n              -121.28906250000001,\n              44.96479793033101\n            ],\n            [\n              -121.28906250000001,\n              49.38237278700955\n            ],\n            [\n              -125.5078125,\n              49.38237278700955\n            ],\n            [\n              -125.5078125,\n              44.96479793033101\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.78320312499999,\n              34.95799531086792\n            ],\n            [\n              -75.05859375,\n              34.95799531086792\n            ],\n            [\n              -75.05859375,\n              38.61687046392973\n            ],\n            [\n              -77.78320312499999,\n              38.61687046392973\n            ],\n            [\n              -77.78320312499999,\n              34.95799531086792\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"806","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Joung, D.J.","contributorId":267176,"corporation":false,"usgs":false,"family":"Joung","given":"D.J.","email":"","affiliations":[{"id":37381,"text":"University of Rochester","active":true,"usgs":false}],"preferred":false,"id":824618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruppel, Carolyn D. 0000-0003-2284-6632 cruppel@usgs.gov","orcid":"https://orcid.org/0000-0003-2284-6632","contributorId":195778,"corporation":false,"usgs":true,"family":"Ruppel","given":"Carolyn","email":"cruppel@usgs.gov","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":824619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Southon, J.","contributorId":267177,"corporation":false,"usgs":false,"family":"Southon","given":"J.","affiliations":[{"id":55429,"text":"University of Irvine","active":true,"usgs":false}],"preferred":false,"id":824620,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kessler, John D. 0000-0003-1097-6800","orcid":"https://orcid.org/0000-0003-1097-6800","contributorId":184241,"corporation":false,"usgs":false,"family":"Kessler","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":824621,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70229526,"text":"70229526 - 2022 - Multi-run migratory behavior of adult male lake sturgeon in a short river","interactions":[],"lastModifiedDate":"2022-03-10T21:43:23.802787","indexId":"70229526","displayToPublicDate":"2021-09-18T15:39:34","publicationYear":"2022","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":"Multi-run migratory behavior of adult male lake sturgeon in a short river","docAbstract":"<p><span>Lake sturgeon (</span><i>Acipenser fulvescens</i><span>) can migrate long distances to spawn, but many populations currently spawn in systems where the length of accessible riverine migratory habitat has been greatly reduced by&nbsp;dam construction. With the increased prevalence of shortened rivers, focusing on migratory dynamics in short rivers (&lt;30&nbsp;km) is beneficial to understanding the migratory needs of lake sturgeon populations. Here we document male lake sturgeon movements during the spawning period in the Winooski River, Vermont, USA; a river with only 17&nbsp;km to the first natural upstream barrier. Male lake sturgeon were acoustically tagged (n&nbsp;=&nbsp;25, 1215–1470&nbsp;mm TL) and tracked using five to nine stationary receivers from 2017 to 2019. River discharge, temperature, the lagged effect of temperature (3-day), and time of day were significant factors describing upstream movements of tagged fish. Migrating male lake sturgeon (n&nbsp;=&nbsp;10 in 2017, n&nbsp;=&nbsp;18 in 2018, and n&nbsp;=&nbsp;17 in 2019) displayed general movement patterns during the spawning period that included a single run upstream to the spawning site (60%), upstream and downstream movements throughout the river during the season (20%), or multiple runs made up the entire length of the spawning tributary to the spawning site (20%). No multi-run males were observed during 2018 when discharge was less flashy (i.e., fewer steep increases and declines in discharge) than in 2017 and 2019. These results suggest that the prevalence of multi-run spawning behavior of male lake sturgeon is related to flow conditions.</span></p>","language":"English","doi":"10.1016/j.jglr.2021.06.012","collaboration":"Vermont Department of Fish and Wildlife","usgsCitation":"Parrish, D.L., Izzo, L., and Zydlewski, G.B., 2022, Multi-run migratory behavior of adult male lake sturgeon in a short river: Journal of Great Lakes Research, v. 47, no. 5, p. 1400-1409, https://doi.org/10.1016/j.jglr.2021.06.012.","productDescription":"10 p.","startPage":"1400","endPage":"1409","ipdsId":"IP-126224","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":397004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Vermont","otherGeospatial":"Winooski River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.29116821289062,\n              44.395032825316115\n            ],\n            [\n              -72.95951843261719,\n              44.395032825316115\n            ],\n            [\n              -72.95951843261719,\n              44.56014191304745\n            ],\n            [\n              -73.29116821289062,\n              44.56014191304745\n            ],\n            [\n              -73.29116821289062,\n              44.395032825316115\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Parrish, Donna L. 0000-0001-9693-6329 dparrish@usgs.gov","orcid":"https://orcid.org/0000-0001-9693-6329","contributorId":138661,"corporation":false,"usgs":true,"family":"Parrish","given":"Donna","email":"dparrish@usgs.gov","middleInitial":"L.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":837761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Izzo, Lisa K.","contributorId":288330,"corporation":false,"usgs":false,"family":"Izzo","given":"Lisa K.","affiliations":[{"id":13253,"text":"University of Vermont","active":true,"usgs":false}],"preferred":false,"id":837762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zydlewski, Gayle Barbin","contributorId":288331,"corporation":false,"usgs":false,"family":"Zydlewski","given":"Gayle","email":"","middleInitial":"Barbin","affiliations":[{"id":7063,"text":"University of Maine","active":true,"usgs":false}],"preferred":false,"id":837763,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70224540,"text":"70224540 - 2022 - Targeted and non-targeted analysis of young-of-year smallmouth bass using comprehensive two-dimensional gas chromatography coupled with time-of-flight mass spectrometry","interactions":[],"lastModifiedDate":"2021-10-06T16:04:22.992337","indexId":"70224540","displayToPublicDate":"2021-09-16T10:03:58","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Targeted and non-targeted analysis of young-of-year smallmouth bass using comprehensive two-dimensional gas chromatography coupled with time-of-flight mass spectrometry","docAbstract":"<p><span>Smallmouth bass in the Susquehanna River Basin, Chesapeake Bay Watershed, USA, have been exhibiting clinical signs of disease and reproductive endocrine disruption (e.g., intersex, male plasma vitellogenin) for over fifteen years. Previous histological and targeted chemical analyses have identified infectious agents and pollutants in fish tissues including organic contaminants, mercury, and perfluorinated compounds, but a common causative link for the observed signs of disease across this widespread area has not been determined. This study examines 146 young-of-year smallmouth bass collected from 14 sampling sites in the Susquehanna River Basin, Pennsylvania, USA with varying levels of disease prevalence. Whole fish were extracted by a recently developed modification to the quick, easy, cheap, effective, rugged, and safe extraction method and analyzed by comprehensive two-dimensional gas chromatography coupled with time-of-flight mass spectrometry. A targeted analysis was conducted to identify the presence and quantity of 127 known contaminants, including polychlorinated biphenyls, brominated diphenyl ethers, organochlorinated pesticides, and pharmaceutical and personal care products. A non-targeted analysis was conducted on the same data set to identify analytes of interest not included on routine target compound lists. Chromatographic alignment through Statistical Compare (ChromaTOF GC) was followed by Fisher ratio and principal component analysis to reduce the data set from thousands of peaks per sample to a final data set of 65 analytes of interest. Comparisons of these 65 compounds between Normal (no observed health anomalies) and Lesioned (observed health anomaly at time of collection) fish revealed increased levels of three chemical families in Lesioned fish including esters, ketones, and nitrogen containing compounds.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2021.150378","usgsCitation":"Teehan, P., Schall, M., Blazer, V., and Dorman, F.L., 2022, Targeted and non-targeted analysis of young-of-year smallmouth bass using comprehensive two-dimensional gas chromatography coupled with time-of-flight mass spectrometry: Science of the Total Environment, v. 806, no. 2, 150378, 10 p., https://doi.org/10.1016/j.scitotenv.2021.150378.","productDescription":"150378, 10 p.","ipdsId":"IP-130510","costCenters":[{"id":50464,"text":"Eastern Ecological Science 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           [\n              -75.926513671875,\n              37.17782559332976\n            ],\n            [\n              -75.882568359375,\n              37.42252593456307\n            ],\n            [\n              -75.618896484375,\n              37.640334898059486\n            ],\n            [\n              -75.509033203125,\n              37.82280243352756\n            ],\n            [\n              -75.38818359375,\n              38.013476231041935\n            ],\n            [\n              -75.16845703124999,\n              38.272688535980976\n            ],\n            [\n              -75.1904296875,\n              38.41916639395372\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"806","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Teehan, Paige","contributorId":236874,"corporation":false,"usgs":false,"family":"Teehan","given":"Paige","email":"","affiliations":[{"id":6738,"text":"The Pennsylvania State University","active":true,"usgs":false}],"preferred":false,"id":823985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schall, Megan K.","contributorId":264767,"corporation":false,"usgs":false,"family":"Schall","given":"Megan K.","affiliations":[{"id":36985,"text":"Penn State University","active":true,"usgs":false}],"preferred":false,"id":823986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blazer, Vicki S. 0000-0001-6647-9614 vblazer@usgs.gov","orcid":"https://orcid.org/0000-0001-6647-9614","contributorId":150384,"corporation":false,"usgs":true,"family":"Blazer","given":"Vicki S.","email":"vblazer@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":823987,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dorman, Frank L","contributorId":236876,"corporation":false,"usgs":false,"family":"Dorman","given":"Frank","email":"","middleInitial":"L","affiliations":[{"id":6738,"text":"The Pennsylvania State University","active":true,"usgs":false}],"preferred":false,"id":823988,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70236513,"text":"70236513 - 2022 - The 6 May 1947 Milwaukee, Wisconsin, earthquake","interactions":[],"lastModifiedDate":"2022-09-09T11:58:51.284302","indexId":"70236513","displayToPublicDate":"2021-09-15T06:56:30","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"The 6 May 1947 Milwaukee, Wisconsin, earthquake","docAbstract":"<div id=\"132052947\" class=\"article-section-wrapper js-article-section js-content-section  \"><p>The State of Wisconsin is not known for earthquake activity. The authoritative public‐facing U.S. Geological Survey Comprehensive Catalog of earthquakes includes only three small (magnitude &lt; 2) earthquakes in the state, all instrumentally recorded. Although other catalogs include more events in Wisconsin, experience has shown that many types of events, such as explosions and cryoseisms, have made their way into earthquake catalogs in this region. In this short report, I summarize available information about an earthquake that was felt in eastern Wisconsin at 15:27 local time on 6 May 1947. As what appears to be the largest historical earthquake in the State of Wisconsin, it is of public interest, its modest size notwithstanding. It appears that no useful instrumental records exist, due in part to a teleseismic event that occurred approximately 3&nbsp;min later, generating surface waves that were recorded on early long‐period instruments in the region. Instrumental data may exist for this event but have not been found. Comparing the felt area with information from recent earthquakes in the region, I estimate an intensity magnitude of 3.8 for the event, with a subjectively estimated uncertainty range 3.5–4.1. Relatively strong effects, including reports of broken dishes in Milwaukee, and shaking described as short but especially sharp, suggest that the event may have been among the sprinkling of shallow earthquakes now known to occur in the upper Great Lakes region.</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0220210150","usgsCitation":"Hough, S.E., 2022, The 6 May 1947 Milwaukee, Wisconsin, earthquake: Seismological Research Letters, v. 93, no. 1, p. 402-412, https://doi.org/10.1785/0220210150.","productDescription":"11 p.","startPage":"402","endPage":"412","ipdsId":"IP-129832","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":406439,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Milwaukee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.07714843749999,\n              42.27730877423709\n            ],\n            [\n              -87.2314453125,\n              42.27730877423709\n            ],\n            [\n              -87.2314453125,\n              43.57243174740972\n            ],\n            [\n              -89.07714843749999,\n              43.57243174740972\n            ],\n            [\n              -89.07714843749999,\n              42.27730877423709\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"93","issue":"1","noUsgsAuthors":false,"publicationDate":"2021-09-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Hough, Susan E. 0000-0002-5980-2986","orcid":"https://orcid.org/0000-0002-5980-2986","contributorId":263442,"corporation":false,"usgs":true,"family":"Hough","given":"Susan","email":"","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":851287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70223912,"text":"70223912 - 2022 - Integrating seabird dietary and groundfish stock assessment data: Can puffins predict pollock spawning stock biomass in the North Pacific?","interactions":[],"lastModifiedDate":"2022-01-06T17:17:17.475902","indexId":"70223912","displayToPublicDate":"2021-09-13T07:13:44","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1652,"text":"Fish and Fisheries","active":true,"publicationSubtype":{"id":10}},"title":"Integrating seabird dietary and groundfish stock assessment data: Can puffins predict pollock spawning stock biomass in the North Pacific?","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Information on the annual variability in abundance and growth of juvenile groundfish can be useful for predicting fisheries stocks, but is often poorly known owing to difficulties in sampling fish in their first year of life. In the Western Gulf of Alaska (WGoA) and Eastern Bering Sea (EBS) ecosystems, three species of puffin (tufted and horned puffin,<span>&nbsp;</span><i>Fratercula cirrhata, Fratercula corniculata,</i><span>&nbsp;</span>and rhinoceros auklet<i>, Cerorhinca monocerata</i>, Alcidae), regularly prey upon (i.e., “sample”) age-0 groundfish, including walleye pollock (<i>Gadus chalcogramma</i>, Gadidae) and Pacific cod (<i>Gadus microcephalus</i>, Gadidae). Here, we test the hypothesis that integrating puffin dietary data with walleye pollock stock assessment data provides information useful for fisheries management, including indices of interannual variation in age-0 abundance and growth. To test this hypothesis, we conducted cross-correlation and regression analyses of puffin-based indices and spawning stock biomass (SSB) for the WGoA and EBS walleye pollock stocks. For the WGoA, SSB leads the abundance of age-0 fish in the puffin diet, indicating that puffins sample the downstream production of the WGoA spawning stock. By contrast, the abundance and growth of age-0 fish sampled by puffins lead SSB for the EBS stock by 1–3 years, indicating that the puffin diet proxies incoming year class strength for this stock. Our study indicates connectivity between the WGoA and EBS walleye pollock stocks. Integration of non-traditional data sources, such as seabird diet data, with stock assessment data appears useful to inform information gaps important for managing US fisheries in the North Pacific.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/faf.12611","usgsCitation":"Sydeman, W., Thompson, S.A., Piatt, J., Zador, S., and Dorn, M.W., 2022, Integrating seabird dietary and groundfish stock assessment data: Can puffins predict pollock spawning stock biomass in the North Pacific?: Fish and Fisheries, v. 23, no. 18, p. 213-226, https://doi.org/10.1111/faf.12611.","productDescription":"14 p.","startPage":"213","endPage":"226","ipdsId":"IP-123820","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"links":[{"id":449709,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/faf.12611","text":"Publisher Index Page"},{"id":389206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -171.123046875,\n              52.3755991766591\n            ],\n            [\n              -148.0517578125,\n              52.3755991766591\n            ],\n            [\n              -148.0517578125,\n              61.56457388515458\n            ],\n            [\n              -171.123046875,\n              61.56457388515458\n            ],\n            [\n              -171.123046875,\n              52.3755991766591\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"23","issue":"18","noUsgsAuthors":false,"publicationDate":"2021-09-13","publicationStatus":"PW","contributors":{"authors":[{"text":"Sydeman, William J.","contributorId":172574,"corporation":false,"usgs":false,"family":"Sydeman","given":"William J.","affiliations":[],"preferred":false,"id":823230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Sarah Ann","contributorId":198394,"corporation":false,"usgs":false,"family":"Thompson","given":"Sarah","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":823231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piatt, John F. 0000-0002-4417-5748","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":244053,"corporation":false,"usgs":true,"family":"Piatt","given":"John F.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":823232,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zador, Stephani","contributorId":60992,"corporation":false,"usgs":false,"family":"Zador","given":"Stephani","affiliations":[],"preferred":false,"id":823233,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dorn, Martin W.","contributorId":3517,"corporation":false,"usgs":false,"family":"Dorn","given":"Martin","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":823302,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70228989,"text":"70228989 - 2022 - Rapid colonisation post-displacement contributes to native fish resilience","interactions":[],"lastModifiedDate":"2022-03-28T16:56:04.603324","indexId":"70228989","displayToPublicDate":"2021-09-12T10:02:40","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1471,"text":"Ecology of Freshwater Fish","active":true,"publicationSubtype":{"id":10}},"title":"Rapid colonisation post-displacement contributes to native fish resilience","docAbstract":"<p><span>Native freshwater fish are experiencing global declines. Determining what drives native fish resilience to disturbance is crucial to understanding their persistence in the face of multiple stressors. Fish colonisation ability may be one factor affecting population resilience after disturbance. We conducted displacement experiments in headwater streams in Wyoming, USA, to evaluate mottled sculpin (</span><i>Cottus bairdii</i><span>) and mountain sucker (</span><i>Catostomus platyrhynchus</i><span>) colonisation ability. Specifically, we (1) determined whether fish could colonise sites rapidly after displacement, (2) evaluated site-level factors affecting colonisation, and (3) compared species-level differences in movement and colonisation capabilities. Mountain sucker recovered to pre-displacement abundances within 6–11&nbsp;weeks, but mottled sculpin were still at slightly reduced abundances. For both species, the majority of colonists were unmarked new individuals and size–structure was similar to pre-displacement size–structure. Fish colonisation was best predicted by pre-displacement abundance and an interaction between per cent riparian cover and species identity. The slower colonisation rate of mottled sculpin may relate to movement ability as average daily movement rate and movement extent were significantly greater for mountain sucker. Our results demonstrate that colonisation is one mechanism allowing fish populations to be resilient in the face of disturbance and that species' traits provide insight into fish colonisation capabilities. Experimental approaches provide mechanistic insight into colonisation dynamics, enhancing our understanding of native fish resilience in degraded stream ecosystems and their response to restoration actions.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/eff.12634","usgsCitation":"Alford, S.L., and Walters, A.W., 2022, Rapid colonisation post-displacement contributes to native fish resilience: Ecology of Freshwater Fish, v. 31, no. 2, p. 347-357, https://doi.org/10.1111/eff.12634.","productDescription":"11 p.","startPage":"347","endPage":"357","ipdsId":"IP-119943","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":436054,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9Z0W4IK","text":"USGS data release","linkHelpText":"Fish movement and colonization in the Wyoming Range 2018-2019"},{"id":396490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Green River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.93994140625,\n              41.04621681452063\n            ],\n            [\n              -108.6328125,\n              41.04621681452063\n            ],\n            [\n              -108.6328125,\n              42.24478535602799\n            ],\n            [\n              -110.93994140625,\n              42.24478535602799\n            ],\n            [\n              -110.93994140625,\n              41.04621681452063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationDate":"2021-09-12","publicationStatus":"PW","contributors":{"authors":[{"text":"Alford, Samantha L.","contributorId":280179,"corporation":false,"usgs":false,"family":"Alford","given":"Samantha","email":"","middleInitial":"L.","affiliations":[{"id":40829,"text":"uwy","active":true,"usgs":false}],"preferred":false,"id":836085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, Annika W. 0000-0002-8638-6682 awalters@usgs.gov","orcid":"https://orcid.org/0000-0002-8638-6682","contributorId":4190,"corporation":false,"usgs":true,"family":"Walters","given":"Annika","email":"awalters@usgs.gov","middleInitial":"W.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":836084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70225541,"text":"70225541 - 2022 - Experimental design and data relevance in a volcanic ash-leachate health study: Letter to the Editor re. Barone et al. (2021) ‘Surface reactivity of Etna volcanic ash and evaluation of health risks’","interactions":[],"lastModifiedDate":"2021-10-21T11:55:06.839049","indexId":"70225541","displayToPublicDate":"2021-09-10T06:53:38","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Experimental design and data relevance in a volcanic ash-leachate health study: Letter to the Editor re. Barone et al. (2021) ‘Surface reactivity of Etna volcanic ash and evaluation of health risks’","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2021.150076","usgsCitation":"Stewart, C., Damby, D., Tomasek, I., and Horwell, C.J., 2022, Experimental design and data relevance in a volcanic ash-leachate health study: Letter to the Editor re. Barone et al. (2021) ‘Surface reactivity of Etna volcanic ash and evaluation of health risks’: Science of the Total Environment, v. 804, 150076, 4 p., https://doi.org/10.1016/j.scitotenv.2021.150076.","productDescription":"150076, 4 p.","ipdsId":"IP-128207","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":467215,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1016/j.scitotenv.2021.150076","text":"External Repository"},{"id":390718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"804","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stewart, Carol","contributorId":236960,"corporation":false,"usgs":false,"family":"Stewart","given":"Carol","email":"","affiliations":[{"id":47573,"text":"Massey University, NZ","active":true,"usgs":false}],"preferred":false,"id":825512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Damby, David 0000-0002-3238-3961","orcid":"https://orcid.org/0000-0002-3238-3961","contributorId":206614,"corporation":false,"usgs":true,"family":"Damby","given":"David","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":825513,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tomasek, Ines","contributorId":205741,"corporation":false,"usgs":false,"family":"Tomasek","given":"Ines","email":"","affiliations":[{"id":37158,"text":"Institute of Hazard, Risk & Resilience, Department of Earth Sciences, Durham University, UK","active":true,"usgs":false}],"preferred":false,"id":825514,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Horwell, Claire J.","contributorId":177455,"corporation":false,"usgs":false,"family":"Horwell","given":"Claire","email":"","middleInitial":"J.","affiliations":[{"id":16770,"text":"Dept. Earth Sciences, Durham University, UK","active":true,"usgs":false}],"preferred":false,"id":825515,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70229535,"text":"70229535 - 2022 - Urban proximity while breeding is not a predictor of perfluoroalkyl substance contamination in the eggs of brown pelicans","interactions":[],"lastModifiedDate":"2022-03-10T15:48:32.467149","indexId":"70229535","displayToPublicDate":"2021-09-09T09:43:09","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Urban proximity while breeding is not a predictor of perfluoroalkyl substance contamination in the eggs of brown pelicans","docAbstract":"<p><span>Identifying sources of exposure to chemical stressors is difficult when both target organisms and stressors are highly mobile. While previous studies have demonstrated that populations of some organisms proximal to urban centers may display increased burdens of human-created chemicals compared to more distal populations, this relationship may not be universal when applied to organisms and stressors capable of transboundary movements. We examined eggs of brown pelicans (</span><i>Pelecanus occidentalis</i><span>), a nearshore seabird with daily movements ranging from local to 50&nbsp;km and annual migrations ranging from year-round residency to 1500&nbsp;km. Thirty-six eggs from three&nbsp;breeding colonies&nbsp;located at increasing distances to a major urban center (Charleston, South Carolina, USA) were analyzed for concentrations of&nbsp;</span><i>per</i><span>- and polyfluoroalkyl substances (PFAS). Areas of high use for each colony during the breeding season were also assessed via the tracking of adult pelicans from each colony using GPS-PTT satellite transmitters and overlapped with measures of relative urbanization via land cover data. We report potentially significant ∑PFAS concentrations in the eggs of pelicans (175.4&nbsp;±&nbsp;120.1&nbsp;ng/g w wt. SD), driven largely by linear perfluorooctane&nbsp;sulfonate&nbsp;(n-PFOS) (48–546&nbsp;ng/g w wt.). Residues of the precursor compound perfluorooctane sulfonamide (FOSA) were also present in pelican eggs, suggesting continued exposure of local wildlife beyond implemented phaseouts of some PFAS. For most analytes, egg concentrations did not exhibit a significant spatial structure despite some differentiation in high-use areas unlike similar data for another regional apex predator, the bottlenose dolphin (</span><i>Tursiops truncatus</i><span>). We suggest that the partially migratory nature of brown pelicans during the non-breeding season, combined with daily ranges that may extend to 50&nbsp;km from local point sources, may have homogenized exposure across individuals. Charleston likely remains a major source for PFAS in the overall region, however, given the high concentrations observed as well as known releases of PFAS in the&nbsp;nearshore environment.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2021.150110","usgsCitation":"Wilkinson, B.P., Robuck, A., Lohman, R., Pickard, H.M., and Jodice, P.G., 2022, Urban proximity while breeding is not a predictor of perfluoroalkyl substance contamination in the eggs of brown pelicans: Science of the Total Environment, v. 803, 150110, 11 p., https://doi.org/10.1016/j.scitotenv.2021.150110.","productDescription":"150110, 11 p.","ipdsId":"IP-126746","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":449715,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.scitotenv.2021.150110","text":"Publisher Index Page"},{"id":396995,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.36911010742188,\n              32.48196313217176\n            ],\n            [\n              -80.30868530273438,\n              32.46690196868371\n            ],\n            [\n              -79.7662353515625,\n              32.690243035492266\n            ],\n            [\n              -79.66049194335938,\n              32.856518010109546\n            ],\n            [\n              -79.76211547851562,\n              32.99714648628775\n            ],\n            [\n              -79.95574951171875,\n              33.14100094401691\n            ],\n            [\n              -80.08758544921874,\n              33.17204260575893\n            ],\n            [\n              -80.32791137695312,\n              32.923402043498875\n            ],\n            [\n              -80.36911010742188,\n              32.48196313217176\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"803","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wilkinson, B. P.","contributorId":279808,"corporation":false,"usgs":false,"family":"Wilkinson","given":"B.","email":"","middleInitial":"P.","affiliations":[{"id":7084,"text":"Clemson University","active":true,"usgs":false}],"preferred":false,"id":837776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robuck, A. R.","contributorId":288354,"corporation":false,"usgs":false,"family":"Robuck","given":"A. R.","affiliations":[{"id":6922,"text":"University of Rhode Island","active":true,"usgs":false}],"preferred":false,"id":837777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lohman, R.","contributorId":288356,"corporation":false,"usgs":false,"family":"Lohman","given":"R.","email":"","affiliations":[{"id":6922,"text":"University of Rhode Island","active":true,"usgs":false}],"preferred":false,"id":837778,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pickard, H. M.","contributorId":288357,"corporation":false,"usgs":false,"family":"Pickard","given":"H.","email":"","middleInitial":"M.","affiliations":[{"id":16811,"text":"Harvard University","active":true,"usgs":false}],"preferred":false,"id":837779,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jodice, Patrick G.R. 0000-0001-8716-120X","orcid":"https://orcid.org/0000-0001-8716-120X","contributorId":219852,"corporation":false,"usgs":true,"family":"Jodice","given":"Patrick","middleInitial":"G.R.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":837780,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70236993,"text":"70236993 - 2022 - Effect of fixing earthquake depth in ShakeAlert algorithms on performance for intraslab earthquakes","interactions":[],"lastModifiedDate":"2022-09-27T12:23:25.206911","indexId":"70236993","displayToPublicDate":"2021-09-08T07:21:02","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Effect of fixing earthquake depth in ShakeAlert algorithms on performance for intraslab earthquakes","docAbstract":"<div id=\"132051794\" class=\"article-section-wrapper js-article-section js-content-section  \"><p>We investigate whether assuming a fixed shallow depth in the ShakeAlert network‐based earthquake early warning system is sufficient to produce accurate ground‐motion based alerts for intraslab earthquakes. ShakeAlert currently uses a fixed focal depth of 8&nbsp;km to estimate earthquake location and magnitude. This is an appropriate way to reduce computational costs without compromising alert accuracy in California, where earthquakes typically occur on shallow crustal faults. In the Pacific Northwest (PNW), however, the most common moderate‐magnitude events occur within the subducting Juan de Fuca slab at depths between ∼35 and 65&nbsp;km. Using a dataset of seismic recordings from 37<span>&nbsp;</span><span class=\"inline-formula no-formula-id\"><span class=\"MathJax_Preview\"><span id=\"MJXp-Span-1\" class=\"MJXp-math\"><span id=\"MJXp-Span-2\" class=\"MJXp-msub\"><span id=\"MJXp-Span-3\" class=\"MJXp-mi MJXp-italic\">M</span><span id=\"MJXp-Span-4\" class=\"MJXp-mi MJXp-script\">w</span></span></span></span></span>&nbsp;4.5+ intraslab earthquakes from the PNW and Chile, we replay events through the Earthquake Point‐Source Integrated Code and eqInfo2GM algorithms to estimate source parameters and compute modified Mercalli intensity (MMI) alert threshold contours. Each event is replayed twice—once using a fixed 8&nbsp;km depth and a second time using the actual catalog earthquake depth. For each depth scenario, we analyze MMI III and IV contours using various performance metrics to determine the number of correctly alerted sites and measure warning times. We determine that shallow depth replays are more likely to produce errors in location estimates of greater than 50&nbsp;km if the event is located outside of a seismic network. When located within a seismic network, shallow and catalog depth replays have similar epicenter estimates. Results show that applying catalog earthquake depth does not improve the accuracy of magnitude estimates or MMI alert threshold contours, or increase warning times. We conclude that using a fixed shallow earthquake depth for intraslab earthquakes will not significantly impact alert accuracy in the PNW.</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0220210056","usgsCitation":"Thompson, M., Hartog, J.R., and Wirth, E.A., 2022, Effect of fixing earthquake depth in ShakeAlert algorithms on performance for intraslab earthquakes: Seismological Research Letters, v. 93, no. 1, p. 277-287, https://doi.org/10.1785/0220210056.","productDescription":"11 p.","startPage":"277","endPage":"287","ipdsId":"IP-130727","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":407394,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.20019531249999,\n              39.80853604144591\n            ],\n            [\n              -120.89355468749999,\n              39.80853604144591\n            ],\n            [\n              -120.89355468749999,\n              49.32512199104001\n            ],\n            [\n              -125.20019531249999,\n              49.32512199104001\n            ],\n            [\n              -125.20019531249999,\n              39.80853604144591\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"93","issue":"1","noUsgsAuthors":false,"publicationDate":"2021-09-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, Mika","contributorId":245851,"corporation":false,"usgs":false,"family":"Thompson","given":"Mika","email":"","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":852961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hartog, J. Renate","contributorId":171724,"corporation":false,"usgs":false,"family":"Hartog","given":"J.","email":"","middleInitial":"Renate","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":852962,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wirth, Erin A. 0000-0002-8592-4442","orcid":"https://orcid.org/0000-0002-8592-4442","contributorId":207853,"corporation":false,"usgs":true,"family":"Wirth","given":"Erin","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":852963,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70223772,"text":"70223772 - 2022 - Post-fire temporal trends in soil-physical and -hydraulic properties and simulated runoff generation: Insights from different burn severities in the 2013 Black Forest Fire, CO, USA","interactions":[],"lastModifiedDate":"2021-09-07T15:38:48.544305","indexId":"70223772","displayToPublicDate":"2021-09-07T10:38:22","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Post-fire temporal trends in soil-physical and -hydraulic properties and simulated runoff generation: Insights from different burn severities in the 2013 Black Forest Fire, CO, USA","docAbstract":"Burn severity influences on post-fire recovery of soil-hydraulic properties controlling runoff generation are poorly understood despite the importance for parameterizing infiltration models. We measured soil-hydraulic properties of field-saturated hydraulic conductivity (Kfs), sorptivity (S), and wetting front potential (ψf) for four years after the 2013 Black Forest Fire, Colorado, USA at six sites across a gradient of initial remotely sensed burn severity using the change in the normalized burn ratio (dNBR). These measurements were correlated with soil-physical property measurements of bulk density (ρb), loss on ignition (LOI, a measure of soil organic matter), and ground cover composition to provide insight into causal factors for temporal changes in Kfs, S, and ψf . Modeled infiltration using the Smith-Parlange approach parameterized with measured Kfs, S, and ψf further discerned the role of precipitation intensity on runoff generation. \nTemporal trends of soil-physical properties and ground cover showed influences from initial burn severity. Trends in soil-hydraulic properties , surprisingly, were not strongly influenced by initial burn severity despite inferred effects of ρb, LOI, and ground cover on trends in Kfs and S. Calculations of dNBR at the time of sampling showed strong correlations with Kfs and S, demonstrating a new approach for estimating long-unburned Kfs and S values, infiltration model parameters after fire, and assessing the time of return to pre-fire values. Simulated infiltration-excess runoff, in contrast, did depend on initial burn severity. Time series of the ratio S2/Kfs ≈ ψf tended to converge between 1 to 10 mm four years after wildfire, potentially (i) defining a long-unburned forest domain of S2/Kfs and ψf from 1 to 10 mm with relatively high Kfs values, and (ii) providing a new post-fire soil-hydraulic property recovery metric (i.e. S2/Kfs ≈ ψf in the range of 1 to 10 mm) for sites in the Rocky Mountains of the USA.","language":"English","publisher":"Elsevier B.V.","doi":"10.1016/j.scitotenv.2021.149847","usgsCitation":"Ebel, B., Moody, J.A., and Martin, D.A., 2022, Post-fire temporal trends in soil-physical and -hydraulic properties and simulated runoff generation: Insights from different burn severities in the 2013 Black Forest Fire, CO, USA: Science of the Total Environment, v. 802, p. 1-14, https://doi.org/10.1016/j.scitotenv.2021.149847.","productDescription":"149847, 14 p.","startPage":"1","endPage":"14","ipdsId":"IP-128944","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":449719,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.scitotenv.2021.149847","text":"Publisher Index Page"},{"id":388879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Black Forest","otherGeospatial":"Black Forest Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.82467651367188,\n              38.92255806063647\n            ],\n            [\n              -104.56787109374999,\n              38.92255806063647\n            ],\n            [\n              -104.56787109374999,\n              39.09223254260029\n            ],\n            [\n              -104.82467651367188,\n              39.09223254260029\n            ],\n            [\n              -104.82467651367188,\n              38.92255806063647\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"802","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ebel, Brian A. 0000-0002-5413-3963","orcid":"https://orcid.org/0000-0002-5413-3963","contributorId":211845,"corporation":false,"usgs":true,"family":"Ebel","given":"Brian A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":822614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moody, John A. 0000-0003-2609-364X jamoody@usgs.gov","orcid":"https://orcid.org/0000-0003-2609-364X","contributorId":771,"corporation":false,"usgs":true,"family":"Moody","given":"John","email":"jamoody@usgs.gov","middleInitial":"A.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":822615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, Deborah A. 0000-0001-8237-0838 damartin@usgs.gov","orcid":"https://orcid.org/0000-0001-8237-0838","contributorId":168662,"corporation":false,"usgs":true,"family":"Martin","given":"Deborah","email":"damartin@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":822616,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70223773,"text":"70223773 - 2022 - Evidence for interannual persistence of infectious influenza A viruses in Alaska wetlands","interactions":[],"lastModifiedDate":"2021-09-15T13:27:32.133001","indexId":"70223773","displayToPublicDate":"2021-09-07T09:34:56","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for interannual persistence of infectious influenza A viruses in Alaska wetlands","docAbstract":"<p>Influenza A viruses (IAVs) deposited by wild birds into the environment may lead to sporadic mortality events and economically costly outbreaks among domestic birds. There is a paucity of information, however, regarding the persistence of infectious IAVs within the environment following deposition. In this investigation, we assessed the persistence of 12 IAVs that were present in the cloaca and/or oropharynx of naturally infected ducks. Infectivity of these IAVs were monitored over approximately one year when held in five water types: (1) distilled water held in the lab at 4 ºC and (2–5) filtered surface water from each of four Alaska sites and maintained in the field at ambient temperature. By evaluating infectivity of IAVs in ovo following sample retrieval at four successive time points, we observed successive declines in IAV infectivity through time. Many viruses persisted for extended periods, as evidenced by ≥ 25% of IAVs remaining infectious in replicate samples for each treatment type through three sampling time points (144–155 days post-sample collection) and two viruses remaining viable in a single replicate sample each when tested upon collection at a fourth time point (361–377 days post-sample collection). The estimated probability of persistence of infectious IAVs in all five water types was estimated to be between 0.25–0.75 during days 50–200 post-sample collection as inferred through Kaplan-Meier survival analysis. Our results provide evidence that IAVs may remain infectious for extended periods, up to or even exceeding one year, when maintained in surface waters under ambient temperatures. Therefore, wetlands may represent an important medium in which infectious IAVs may reside outside of a biotic reservoir.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.scitotenv.2021.150078","usgsCitation":"Ramey, A.M., Reeves, A.B., Lagasse, B.J., Patil, V.P., Hubbard, L.E., Kolpin, D., McCleskey, R., Repert, D.A., Stallknecht, D., and Poulson, R., 2022, Evidence for interannual persistence of infectious influenza A viruses in Alaska wetlands: Science of the Total Environment, v. 803, 150078, 9 p., https://doi.org/10.1016/j.scitotenv.2021.150078.","productDescription":"150078, 9 p.","ipdsId":"IP-130156","costCenters":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":449722,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.scitotenv.2021.150078","text":"Publisher Index Page"},{"id":436056,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P98L6ASV","text":"USGS data release","linkHelpText":"Temporal Viral Viability Data from Avian Influenza A Viruses Maintained in Alaska Wetlands Under Experimental and Environmental Conditions"},{"id":388876,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bluebill Lake, Izembek National Wildlife Refuge, Proxy Pond, Red Salmon Lake, Rescue Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -163.44085693359375,\n              55.076794905148105\n            ],\n            [\n              -163.42437744140625,\n              55.020149969057954\n            ],\n            [\n              -163.3392333984375,\n              55.06421406528486\n            ],\n            [\n              -163.32000732421875,\n              55.02802211299252\n            ],\n            [\n              -163.19091796875,\n              55.03431871502809\n            ],\n            [\n              -163.157958984375,\n              55.079939497082805\n            ],\n            [\n              -163.08380126953125,\n              55.095658749067766\n            ],\n            [\n              -162.97119140625,\n              55.0217245215306\n            ],\n            [\n              -162.70202636718747,\n              55.08937178977164\n            ],\n            [\n              -162.784423828125,\n              55.25877293644583\n            ],\n            [\n              -162.85858154296875,\n              55.294756169220264\n            ],\n            [\n              -162.96295166015625,\n              55.2963199179754\n            ],\n            [\n              -163.44085693359375,\n              55.076794905148105\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"803","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ramey, Andrew M. 0000-0002-3601-8400 aramey@usgs.gov","orcid":"https://orcid.org/0000-0002-3601-8400","contributorId":1872,"corporation":false,"usgs":true,"family":"Ramey","given":"Andrew","email":"aramey@usgs.gov","middleInitial":"M.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":822617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, Andrew B. 0000-0002-7526-0726 areeves@usgs.gov","orcid":"https://orcid.org/0000-0002-7526-0726","contributorId":167362,"corporation":false,"usgs":true,"family":"Reeves","given":"Andrew","email":"areeves@usgs.gov","middleInitial":"B.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":822618,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lagasse, Benjamin Joel 0000-0003-2565-5284","orcid":"https://orcid.org/0000-0003-2565-5284","contributorId":247509,"corporation":false,"usgs":true,"family":"Lagasse","given":"Benjamin","email":"","middleInitial":"Joel","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":822628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patil, Vijay P. 0000-0002-9357-194X vpatil@usgs.gov","orcid":"https://orcid.org/0000-0002-9357-194X","contributorId":203676,"corporation":false,"usgs":true,"family":"Patil","given":"Vijay","email":"vpatil@usgs.gov","middleInitial":"P.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":false,"id":822620,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hubbard, Laura E. 0000-0003-3813-1500 lhubbard@usgs.gov","orcid":"https://orcid.org/0000-0003-3813-1500","contributorId":4221,"corporation":false,"usgs":true,"family":"Hubbard","given":"Laura","email":"lhubbard@usgs.gov","middleInitial":"E.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":822629,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kolpin, Dana W. 0000-0002-3529-6505","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":204154,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana W.","affiliations":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":822622,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McCleskey, R. Blaine 0000-0002-2521-8052","orcid":"https://orcid.org/0000-0002-2521-8052","contributorId":205663,"corporation":false,"usgs":true,"family":"McCleskey","given":"R. Blaine","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":822623,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Repert, Deborah A. 0000-0001-7284-1456 darepert@usgs.gov","orcid":"https://orcid.org/0000-0001-7284-1456","contributorId":2578,"corporation":false,"usgs":true,"family":"Repert","given":"Deborah","email":"darepert@usgs.gov","middleInitial":"A.","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":822624,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Stallknecht, David E.","contributorId":225107,"corporation":false,"usgs":false,"family":"Stallknecht","given":"David E.","affiliations":[{"id":36701,"text":"Southeastern Cooperative Wildlife Disease Study, Department of Population Health, College of Veterinary Medicine, University of Georgia","active":true,"usgs":false}],"preferred":false,"id":822630,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Poulson, Rebecca L.","contributorId":198807,"corporation":false,"usgs":false,"family":"Poulson","given":"Rebecca L.","affiliations":[{"id":7125,"text":"Southeastern Cooperative Wildlife Disease Study, College of Veterinary Medicine, University of Georgia, Athens, GA 30602, USA.","active":true,"usgs":false}],"preferred":false,"id":822631,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70231633,"text":"70231633 - 2022 - Nearshore microfossil assemblages in a Caribbean reef environment show variable rates of recovery following Hurricane Irma","interactions":[],"lastModifiedDate":"2022-05-18T13:52:57.365425","indexId":"70231633","displayToPublicDate":"2021-09-07T07:14:32","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3369,"text":"Sedimentology","active":true,"publicationSubtype":{"id":10}},"title":"Nearshore microfossil assemblages in a Caribbean reef environment show variable rates of recovery following Hurricane Irma","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Modern microfossil distributions reflect site-specific habitats and provide an opportunity to assess sediment transport pathways in the nearshore environment. When applied to overwash deposits in the geological record, they provide insight into sediment provenance and transport, factors important for understanding patterns of frequency and intensity of past storms and tsunamis. Modern distribution studies are rare and often the first established ones occur immediately after an overwash event as part of a post-event field survey. This is problematic because it is unclear what effect overwash events have on nearshore microfossil assemblages and what time interval is necessary for them to return to pre-event conditions. This study documents the impacts of Hurricane Irma on nearshore sediments off the coast of Anegada, British Virgin Islands, using distributions of<span>&nbsp;</span><i>Homotrema rubrum</i>, an encrusting foraminifer with a defined provenance in coral reefs. At four sampling intervals spanning two years, from six months pre-Hurricane Irma to eighteen months after, surface sediment was collected from three transects on the northern and southern shores of the island. Partitioning Around Medoids cluster analysis revealed that Hurricane Irma introduced an influx of well-preserved fragments into the reef flat and made the sediments more uniform, limiting the foraminifer’s utility as a known sediment transport indicator. The mixing of sediments along the two northern transects (reef proximal) persisted for seven to eighteen months before returning to near pre-hurricane conditions. However, the southern transect (absence of reef), where<span>&nbsp;</span><i>Homotrema rubrum</i><span>&nbsp;</span>concentrations are significantly less, failed to recover within the time period assessed by this study, indicating a variable recovery period between Atlantic Ocean and Caribbean Sea facing shorelines. Results from this study suggest that a waiting period of at least eighteen months after a major storm is recommended before collecting surface sediment from the nearshore environments of reef-dominated coastlines.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/sed.12944","usgsCitation":"Mitchell, S., Pilarczyk, J., Spiske, M., and Jaffe, B.E., 2022, Nearshore microfossil assemblages in a Caribbean reef environment show variable rates of recovery following Hurricane Irma: Sedimentology, v. 69, no. 3, p. 1209-1230, https://doi.org/10.1111/sed.12944.","productDescription":"22 p.","startPage":"1209","endPage":"1230","ipdsId":"IP-126895","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":449727,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/sed.12944","text":"Publisher Index Page"},{"id":400688,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Virgin Islands","otherGeospatial":"British Virgin Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.050048828125,\n              18.2397859708389\n            ],\n            [\n              -64.171142578125,\n              18.2397859708389\n            ],\n            [\n              -64.171142578125,\n              18.620218991632978\n            ],\n            [\n              -65.050048828125,\n              18.620218991632978\n            ],\n            [\n              -65.050048828125,\n              18.2397859708389\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"3","noUsgsAuthors":false,"publicationDate":"2021-10-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Mitchell, Stephen","contributorId":291831,"corporation":false,"usgs":false,"family":"Mitchell","given":"Stephen","email":"","affiliations":[{"id":38697,"text":"University of Southern Mississippi","active":true,"usgs":false}],"preferred":false,"id":843160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pilarczyk, Jessica","contributorId":291832,"corporation":false,"usgs":false,"family":"Pilarczyk","given":"Jessica","affiliations":[{"id":36678,"text":"Simon Fraser University","active":true,"usgs":false}],"preferred":false,"id":843161,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spiske, Michaela","contributorId":291834,"corporation":false,"usgs":false,"family":"Spiske","given":"Michaela","affiliations":[{"id":62763,"text":"Universitat Basel","active":true,"usgs":false}],"preferred":false,"id":843162,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":843163,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70223844,"text":"70223844 - 2022 - First documentation of long-distance travel by a Florida manatee to the Mexican Caribbean","interactions":[],"lastModifiedDate":"2023-06-09T13:56:13.151527","indexId":"70223844","displayToPublicDate":"2021-09-03T07:20:28","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":9339,"text":"Ethology, Ecology and Evolution","active":true,"publicationSubtype":{"id":10}},"title":"First documentation of long-distance travel by a Florida manatee to the Mexican Caribbean","docAbstract":"<div class=\"abstractSection abstractInFull\"><p>West Indian manatees (<i>Trichechus manatus</i>) are separated into two allopatric subspecies: the Florida manatee (<i>T. m. latirostris</i>) and the Antillean manatee (<i>T. m. manatus</i>). In the winter of 2020–2021, an adult manatee was sighted off the coast of Cancun, Quintana Roo, Mexico, in areas where Antillean manatees are not typically seen. The individual had distinct watercraft scars on its body, which were matched using photo-identification to a known male Florida manatee (PE424) that had been repeatedly photographed in Florida since 1998. This is the first record of a Florida manatee visiting the Mexican Caribbean. Previous reports of individuals from this subspecies in Cuba, combined with genetic evidence, suggest some level of connectivity among geographically separated manatee populations.</p></div><div class=\"abstractSection abstractInFull\"><ul class=\"NLM_list NLM_list-list_type-bullet\"><li><p class=\"inline\">We present the first evidence of along-distance movement by amanatee from Florida to the Yucatan Peninsula (Quintana Roo, Mexican Caribbean).</p></li><li><p class=\"inline\">This case, previous reports of Florida manatees in Cuba, and genetic evidence, suggest acertain degree of genetic mixture among the two subspecies.</p></li></ul></div>","language":"English","publisher":"Taylor and Francis","doi":"10.1080/03949370.2021.1967457","usgsCitation":"Castelblanco-Martinez, N., Álvarez-Alemán, A., Torres, R., Teague, A.L., Barton, S., Rood, K.A., Ramos, E.A., and Mignucci-Giannoni, A.A., 2022, First documentation of long-distance travel by a Florida manatee to the Mexican Caribbean: Ethology, Ecology and Evolution, v. 34, no. 5, p. 545-556, https://doi.org/10.1080/03949370.2021.1967457.","productDescription":"12 p.; Data Release","startPage":"545","endPage":"556","ipdsId":"IP-127533","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":389051,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":417860,"rank":2,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9J34MCR"}],"country":"Mexico","otherGeospatial":"Yucatan Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -86.9737129167707,\n              21.690309852040613\n            ],\n            [\n              -86.9737129167707,\n              20.838915529759802\n            ],\n            [\n              -85.98039513060182,\n              20.838915529759802\n            ],\n            [\n              -85.98039513060182,\n              21.690309852040613\n            ],\n            [\n              -86.9737129167707,\n              21.690309852040613\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"34","issue":"5","noUsgsAuthors":false,"publicationDate":"2021-09-03","publicationStatus":"PW","contributors":{"authors":[{"text":"Castelblanco-Martinez, Nataly","contributorId":265538,"corporation":false,"usgs":false,"family":"Castelblanco-Martinez","given":"Nataly","email":"","affiliations":[{"id":54718,"text":"Consejo Nacional de Ciencia y Tecnología/Universidad de Quintana Rooand 2Fundación Internacional para la Naturaleza y la Sustentabilidad","active":true,"usgs":false}],"preferred":false,"id":822905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Álvarez-Alemán, Anmari","contributorId":265539,"corporation":false,"usgs":false,"family":"Álvarez-Alemán","given":"Anmari","affiliations":[{"id":54719,"text":"Clearwater Marine Aquarium Research Institute","active":true,"usgs":false}],"preferred":false,"id":822906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Torres, Raul","contributorId":265540,"corporation":false,"usgs":false,"family":"Torres","given":"Raul","email":"","affiliations":[{"id":54720,"text":"Delphinus","active":true,"usgs":false}],"preferred":false,"id":822907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Teague, Amy L. 0000-0003-3433-9291 ateague@usgs.gov","orcid":"https://orcid.org/0000-0003-3433-9291","contributorId":4697,"corporation":false,"usgs":true,"family":"Teague","given":"Amy","email":"ateague@usgs.gov","middleInitial":"L.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":822908,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barton, Sheri","contributorId":265541,"corporation":false,"usgs":false,"family":"Barton","given":"Sheri","email":"","affiliations":[{"id":13147,"text":"Mote Marine Laboratory","active":true,"usgs":false}],"preferred":false,"id":822909,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rood, Kari A","contributorId":265542,"corporation":false,"usgs":false,"family":"Rood","given":"Kari","email":"","middleInitial":"A","affiliations":[{"id":12556,"text":"Florida Fish and Wildlife Conservation Commission","active":true,"usgs":false}],"preferred":false,"id":822910,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ramos, Eric A","contributorId":265543,"corporation":false,"usgs":false,"family":"Ramos","given":"Eric","email":"","middleInitial":"A","affiliations":[{"id":54721,"text":"Fundación Internacional para la Naturaleza y la Sustentabilidad","active":true,"usgs":false}],"preferred":false,"id":822911,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mignucci-Giannoni, Antonio A.","contributorId":201773,"corporation":false,"usgs":false,"family":"Mignucci-Giannoni","given":"Antonio","email":"","middleInitial":"A.","affiliations":[{"id":36251,"text":"Interamerican University of Puerto Rico","active":true,"usgs":false}],"preferred":false,"id":822912,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70223823,"text":"70223823 - 2022 - Identifying climate-resistant vernal pools: Hydrologic refugia for amphibian reproduction under droughts and climate change","interactions":[],"lastModifiedDate":"2022-08-01T16:47:26.011836","indexId":"70223823","displayToPublicDate":"2021-09-02T07:41:04","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1447,"text":"Ecohydrology","active":true,"publicationSubtype":{"id":10}},"title":"Identifying climate-resistant vernal pools: Hydrologic refugia for amphibian reproduction under droughts and climate change","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Vernal pools of the northeastern United States provide important breeding habitat for amphibians but may be sensitive to droughts and climate change. These seasonal wetlands typically fill by early spring and dry by mid-to-late summer. Because climate change may produce earlier and stronger growing-season evapotranspiration combined with increasing droughts and shifts in precipitation timing, management concerns include the possibility that some pools will increasingly become dry earlier in the year, potentially interfering with amphibian life-cycle completion. In this context, a subset of pools that continue to provide wetland habitat later into the year under relatively dry conditions might function as ecohydrologic refugia, potentially supporting species persistence even as summer conditions become warmer and droughts more frequent. We used approximately 3,000 field observations of inundation from 449 pools to train machine-learning models that predict the likelihood of pool inundation based on pool size, day of the year, climate conditions, short-term weather patterns, and soil, geologic, and landcover attributes. Models were then used to generate predictions of pool wetness across five seasonal time points, three short-term weather scenarios, and four sets of downscaled climate projections. Model outputs are available through a website allowing users to choose the inundation thresholds, time points, weather scenarios, and future climate projections most relevant to their management needs. Together with long-term monitoring of individual pools at the site scale, this regional-scale study can support amphibian conservation by helping to identify which pools may be most likely to function as ecohydrologic refugia from droughts and climate change.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1002/eco.2354","usgsCitation":"Cartwright, J.M., Morelli, T.L., and Campbell Grant, E.H., 2022, Identifying climate-resistant vernal pools: Hydrologic refugia for amphibian reproduction under droughts and climate change: Ecohydrology, v. 15, no. 5, e2354, 23 p., https://doi.org/10.1002/eco.2354.","productDescription":"e2354, 23 p.","ipdsId":"IP-122474","costCenters":[{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"links":[{"id":449730,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/eco.2354","text":"Publisher Index Page"},{"id":388994,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"5","noUsgsAuthors":false,"publicationDate":"2021-10-04","publicationStatus":"PW","contributors":{"authors":[{"text":"Cartwright, Jennifer M. 0000-0003-0851-8456 jmcart@usgs.gov","orcid":"https://orcid.org/0000-0003-0851-8456","contributorId":5386,"corporation":false,"usgs":true,"family":"Cartwright","given":"Jennifer","email":"jmcart@usgs.gov","middleInitial":"M.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true},{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true}],"preferred":true,"id":822794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":822795,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell Grant, Evan H. 0000-0003-4401-6496 ehgrant@usgs.gov","orcid":"https://orcid.org/0000-0003-4401-6496","contributorId":150443,"corporation":false,"usgs":true,"family":"Campbell Grant","given":"Evan","email":"ehgrant@usgs.gov","middleInitial":"H.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":822796,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70224638,"text":"70224638 - 2022 - Diffuse deformation and surface faulting distribution from sub-metric image correlation along the 2019 Ridgecrest ruptures (California, USA)","interactions":[],"lastModifiedDate":"2022-08-01T16:49:21.983328","indexId":"70224638","displayToPublicDate":"2021-08-31T11:24:13","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Diffuse deformation and surface faulting distribution from sub-metric image correlation along the 2019 Ridgecrest ruptures (California, USA)","docAbstract":"<p><span>The 2019&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>w</mi></msub></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"msub\"><span id=\"MathJax-Span-4\" class=\"mi\"><i>M</i><sub>w</sub></span></span></span></span></span></span></span><span>&nbsp;6.4 and 7.1 Ridgecrest, California, earthquake sequence (July 2019) ruptured consecutively a system of high‐angle strike‐slip cross faults (northeast‐ and northwest‐trending) within 34&nbsp;hr. The complex rupture mechanism was illuminated by seismological and geodetic data, bringing forward the issue of the interdependency of the two fault systems both at depth and at the surface, and of its effect on the final surface displacement pattern. Here, we use high‐resolution (WorldView and Pleiades) optical satellite image correlation to measure the near‐fault horizontal and vertical surface displacement fields at 0.5&nbsp;m ground resolution for the two earthquakes. We point out significant differences with previous geodetic‐ and geologic‐based measurements, and document the essential role of distributed faulting and diffuse deformation in producing the observed surface displacement patterns. We derive strain fields from the horizontal displacement maps, and highlight the predominant role of rotation and shear strain in the surface rupture process. We discuss the segmentation of the rupture based on the fault geometry and along‐strike slip variations. We also image several northeast‐trending faults with similar orientation to the deeply embedded shear fabric identified in aftershock studies, and show that these cross faults are present all along the rupture, including at a scale &lt;100&nbsp;m. Finally, we compare our results to kinematic slip inversions, and show that the surface diffuse deformation is primarily associated with areas of shallow slip deficit; however, this diffuse deformation cannot be explained using elastic modeling. We conclude that inelastic processes play an important role in contributing to the total surface deformation associated with the 2019 Ridgecrest sequence.</span></p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120210036","usgsCitation":"Antoine, S.L., Klinger, Y., Delorme, A., Wang, K., Burgmann, R., and Gold, R.D., 2022, Diffuse deformation and surface faulting distribution from sub-metric image correlation along the 2019 Ridgecrest ruptures (California, USA): Bulletin of the Seismological Society of America, v. 111, no. 5, p. 2275-2302, https://doi.org/10.1785/0120210036.","productDescription":"28 p.","startPage":"2275","endPage":"2302","ipdsId":"IP-129938","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":390260,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Ridgecrest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119,\n              34\n            ],\n            [\n              -116,\n              34\n            ],\n            [\n              -116,\n              37\n            ],\n            [\n              -119,\n              37\n            ],\n            [\n              -119,\n              34\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"111","issue":"5","noUsgsAuthors":false,"publicationDate":"2021-08-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Antoine, Solene L.","contributorId":266165,"corporation":false,"usgs":false,"family":"Antoine","given":"Solene","email":"","middleInitial":"L.","affiliations":[{"id":30776,"text":"Institut de Physique du Globe de Paris","active":true,"usgs":false}],"preferred":false,"id":824479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klinger, Yann","contributorId":266166,"corporation":false,"usgs":false,"family":"Klinger","given":"Yann","affiliations":[{"id":30776,"text":"Institut de Physique du Globe de Paris","active":true,"usgs":false}],"preferred":false,"id":824480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Delorme, Arthur","contributorId":266167,"corporation":false,"usgs":false,"family":"Delorme","given":"Arthur","email":"","affiliations":[{"id":30776,"text":"Institut de Physique du Globe de Paris","active":true,"usgs":false}],"preferred":false,"id":824481,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wang, Kang","contributorId":197483,"corporation":false,"usgs":false,"family":"Wang","given":"Kang","email":"","affiliations":[],"preferred":false,"id":824482,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burgmann, Roland 0000-0002-3560-044X","orcid":"https://orcid.org/0000-0002-3560-044X","contributorId":264610,"corporation":false,"usgs":false,"family":"Burgmann","given":"Roland","email":"","affiliations":[{"id":54514,"text":"Berkeley Seismological Laboratory, University of California, Berkeley","active":true,"usgs":false}],"preferred":false,"id":824483,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gold, Ryan D. 0000-0002-4464-6394 rgold@usgs.gov","orcid":"https://orcid.org/0000-0002-4464-6394","contributorId":3883,"corporation":false,"usgs":true,"family":"Gold","given":"Ryan","email":"rgold@usgs.gov","middleInitial":"D.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":824484,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70226210,"text":"70226210 - 2022 - Risk-based wellhead protection decision support: A repeatable workﬂow approach","interactions":[],"lastModifiedDate":"2022-01-25T17:15:23.798251","indexId":"70226210","displayToPublicDate":"2021-08-31T07:41:55","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Risk-based wellhead protection decision support: A repeatable workﬂow approach","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Environmental water management often benefits from a risk-based approach where information on the area of interest is characterized, assembled, and incorporated into a decision model considering uncertainty. This includes prior information from literature, field measurements, professional interpretation, and data assimilation resulting in a decision tool with a posterior uncertainty assessment accounting for prior understanding and what is learned through model development and data assimilation. Model construction and data assimilation are time consuming and prone to errors, which motivates a repeatable workflow where revisions resulting from new interpretations or discovery of errors can be addressed and the analyses repeated efficiently and rigorously. In this work, motivated by the real world application of delineating risk-based (probabilistic) sources of water to supply wells in a humid temperate climate, a scripted workflow was generated for groundwater model construction, data assimilation, particle-tracking and post-processing. The workflow leverages existing datasets describing hydrogeology, hydrography, water use, recharge, and lateral boundaries. These specific data are available in the United States but the tools can be applied to similar datasets worldwide. The workflow builds the model, performs ensemble-based history matching, and uses a posterior Monte Carlo approach to provide probabilistic capture zones describing source water to wells in a risk-based framework. The water managers can then select areas of varying levels of protection based on their tolerance for risk of potential wrongness of the underlying models. All the tools in this workflow are open-source and free, which facilitates testing of this repeatable and transparent approach to other environmental problems.</p></div></div>","language":"English","publisher":"National Ground Water Association","doi":"10.1111/gwat.13129","usgsCitation":"Fienen, M., Corson-Dosch, N., White, J., Leaf, A.T., and Hunt, R., 2022, Risk-based wellhead protection decision support: A repeatable workﬂow approach: Groundwater, v. 60, no. 1, p. 71-86, https://doi.org/10.1111/gwat.13129.","productDescription":"16 p.","startPage":"71","endPage":"86","ipdsId":"IP-127914","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":436057,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9HWSOHP","text":"USGS data release","linkHelpText":"Groundwater Model Archive and Workflow for Neversink/Rondout Basin, New York, Source Water Delineation"},{"id":391793,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"1","noUsgsAuthors":false,"publicationDate":"2021-09-25","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":826891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Corson-Dosch, Nicholas 0000-0002-6776-6241","orcid":"https://orcid.org/0000-0002-6776-6241","contributorId":202630,"corporation":false,"usgs":true,"family":"Corson-Dosch","given":"Nicholas","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":826892,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Jeremy T. 0000-0002-4950-1469","orcid":"https://orcid.org/0000-0002-4950-1469","contributorId":248830,"corporation":false,"usgs":false,"family":"White","given":"Jeremy T.","affiliations":[{"id":50032,"text":"GNS New Zealand","active":true,"usgs":false}],"preferred":false,"id":826893,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":826894,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hunt, Randall J. 0000-0001-6465-9304","orcid":"https://orcid.org/0000-0001-6465-9304","contributorId":16118,"corporation":false,"usgs":true,"family":"Hunt","given":"Randall J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":826895,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70230329,"text":"70230329 - 2022 - A big problem for small earthquakes: Benchmarking routine magnitudes and conversion relationships with coda-envelope-derived Mw in southern Kansas and northern Oklahoma","interactions":[],"lastModifiedDate":"2022-04-07T11:58:37.794763","indexId":"70230329","displayToPublicDate":"2021-08-31T06:51:45","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":10539,"text":"Bulletin of the Seismological Society of America (BSSA)","active":true,"publicationSubtype":{"id":10}},"title":"A big problem for small earthquakes: Benchmarking routine magnitudes and conversion relationships with coda-envelope-derived Mw in southern Kansas and northern Oklahoma","docAbstract":"<p><span>Earthquake magnitudes are widely relied upon measures of earthquake size. Although moment magnitude (</span><span class=\"inline-formula no-formula-id\">⁠<span id=\"MathJax-Element-3-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>w</mi></msub></math>\"><span id=\"MathJax-Span-11\" class=\"math\"><span><span id=\"MathJax-Span-12\" class=\"mrow\"><span id=\"MathJax-Span-13\" class=\"msub\"><span id=\"MathJax-Span-14\" class=\"mi\">M</span><span id=\"MathJax-Span-15\" class=\"mi\">w</span></span></span></span></span><span class=\"MJX_Assistive_MathML\">Mw</span></span>⁠</span><span>) has become the established standard for moderate and large earthquakes, difficulty in reliably measuring seismic moments for small (generally&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>w</mi></msub><mo xmlns=&quot;&quot;>&amp;lt;</mo><mn xmlns=&quot;&quot;>4</mn></math>\"><span id=\"MathJax-Span-16\" class=\"math\"><span><span id=\"MathJax-Span-17\" class=\"mrow\"><span id=\"MathJax-Span-18\" class=\"msub\"><span id=\"MathJax-Span-19\" class=\"mi\">M</span><span id=\"MathJax-Span-20\" class=\"mi\">w</span></span><span id=\"MathJax-Span-21\" class=\"mo\">&lt;</span><span id=\"MathJax-Span-22\" class=\"mn\">4</span></span></span></span><span class=\"MJX_Assistive_MathML\">Mw&lt;4</span></span>⁠</span><span>) earthquakes has meant that magnitudes for these events remain plagued by a patchwork of inconsistent measurement scales. Because of this, magnitudes of small earthquakes and statistics derived from them can be biased. Furthermore, because small earthquakes are much more numerous than large ones, many applications, such as seismic hazard modeling, depend critically on analysis of events characterized by magnitudes other than&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>w</mi></msub></math>\"><span id=\"MathJax-Span-23\" class=\"math\"><span><span id=\"MathJax-Span-24\" class=\"mrow\"><span id=\"MathJax-Span-25\" class=\"msub\"><span id=\"MathJax-Span-26\" class=\"mi\">M</span><span id=\"MathJax-Span-27\" class=\"mi\">w</span></span></span></span></span><span class=\"MJX_Assistive_MathML\">Mw</span></span>⁠</span><span>. To assess this problem, we apply coda envelope analysis to reliably determine moment magnitudes for a case study of small earthquakes from northern Oklahoma and southern Kansas. Not surprisingly, we find significant differences among&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>L</mi></msub></math>\"><span id=\"MathJax-Span-28\" class=\"math\"><span><span id=\"MathJax-Span-29\" class=\"mrow\"><span id=\"MathJax-Span-30\" class=\"msub\"><span id=\"MathJax-Span-31\" class=\"mi\">M</span><span id=\"MathJax-Span-32\" class=\"mi\">L</span></span></span></span></span><span class=\"MJX_Assistive_MathML\">ML</span></span>⁠</span><span>,&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-7-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>m</mi><mrow><mi mathvariant=&quot;normal&quot;>b</mi><mi>L</mi><mi>g</mi></mrow></msub></math>\"><span id=\"MathJax-Span-33\" class=\"math\"><span><span id=\"MathJax-Span-34\" class=\"mrow\"><span id=\"MathJax-Span-35\" class=\"msub\"><span id=\"MathJax-Span-36\" class=\"mi\">m</span><span id=\"MathJax-Span-37\" class=\"mrow\"><span id=\"MathJax-Span-38\" class=\"mi\">b</span><span id=\"MathJax-Span-39\" class=\"mi\">L</span><span id=\"MathJax-Span-40\" class=\"mi\">g</span></span></span></span></span></span><span class=\"MJX_Assistive_MathML\">mbLg</span></span>⁠</span><span>, and&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-8-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>w</mi></msub></math>\"><span id=\"MathJax-Span-41\" class=\"math\"><span><span id=\"MathJax-Span-42\" class=\"mrow\"><span id=\"MathJax-Span-43\" class=\"msub\"><span id=\"MathJax-Span-44\" class=\"mi\">M</span><span id=\"MathJax-Span-45\" class=\"mi\">w</span></span></span></span></span><span class=\"MJX_Assistive_MathML\">Mw</span></span></span><span>&nbsp;for M ∼2–4 earthquakes examined here. More troublingly, we find that relations designed to convert other magnitudes to&nbsp;</span><span class=\"inline-formula no-formula-id\"><span id=\"MathJax-Element-9-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msub xmlns=&quot;&quot;><mi>M</mi><mi mathvariant=&quot;normal&quot;>w</mi></msub></math>\"><span id=\"MathJax-Span-46\" class=\"math\"><span><span id=\"MathJax-Span-47\" class=\"mrow\"><span id=\"MathJax-Span-48\" class=\"msub\"><span id=\"MathJax-Span-49\" class=\"mi\">M</span><span id=\"MathJax-Span-50\" class=\"mi\">w</span></span></span></span></span><span class=\"MJX_Assistive_MathML\">Mw</span></span>⁠</span><span>, which are relied upon for important applications such as seismic hazard analysis, often increase rather than decrease this bias for our dataset. In our case study, we find that converted magnitudes can result in a systematic bias sometimes exceeding 0.5 magnitude units, a difference that typically corresponds to a factor of ∼3 in seismicity rate. Moreover, we find a correspondingly large bias in Gutenberg–Richter&nbsp;</span><i>b</i><span>‐values, controlled primarily by inaccurate magnitude scaling in the conversion relationships. Although this study focuses on a relatively small geographic area, we can expect that similar issues exist with varying severity in other regions. Therefore, magnitudes of small earthquakes and their associated statistics, including seismicity rates and&nbsp;</span><i>b</i><span>‐values, should be treated with caution.</span></p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120210115","usgsCitation":"Shelly, D.R., Mayeda, K., Barno, J., Whidden, K.M., Moschetti, M.P., Llenos, A.L., Rubinstein, J., Yeck, W.L., Earle, P.S., Gok, R., and Walter, W.R., 2022, A big problem for small earthquakes: Benchmarking routine magnitudes and conversion relationships with coda-envelope-derived Mw in southern Kansas and northern Oklahoma: Bulletin of the Seismological Society of America (BSSA), v. 112, no. 1, p. 210-225, https://doi.org/10.1785/0120210115.","productDescription":"16 p.","startPage":"210","endPage":"225","ipdsId":"IP-130008","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":449735,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.osti.gov/biblio/1868860","text":"External Repository"},{"id":398302,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas, Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.8876953125,\n              35.31736632923788\n            ],\n            [\n              -94.7021484375,\n              35.31736632923788\n            ],\n            [\n              -94.7021484375,\n              38.34165619279595\n            ],\n            [\n              -99.8876953125,\n              38.34165619279595\n            ],\n            [\n              -99.8876953125,\n              35.31736632923788\n            ]\n          ]\n        ]\n      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Justin","contributorId":289897,"corporation":false,"usgs":false,"family":"Barno","given":"Justin","email":"","affiliations":[{"id":62279,"text":"Lawrence Livermore National Laboratory, Livermore, CA, USA","active":true,"usgs":false}],"preferred":false,"id":839992,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whidden, Katherine M.","contributorId":289898,"corporation":false,"usgs":false,"family":"Whidden","given":"Katherine","email":"","middleInitial":"M.","affiliations":[{"id":62280,"text":"University of Utah Seismograph Stations, University of Utah, USA","active":true,"usgs":false}],"preferred":false,"id":839993,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moschetti, Morgan P. 0000-0001-7261-0295 mmoschetti@usgs.gov","orcid":"https://orcid.org/0000-0001-7261-0295","contributorId":1662,"corporation":false,"usgs":true,"family":"Moschetti","given":"Morgan","email":"mmoschetti@usgs.gov","middleInitial":"P.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":839994,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Llenos, Andrea L. 0000-0002-4088-6737 allenos@usgs.gov","orcid":"https://orcid.org/0000-0002-4088-6737","contributorId":4455,"corporation":false,"usgs":true,"family":"Llenos","given":"Andrea","email":"allenos@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":839995,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rubinstein, Justin 0000-0003-1274-6785","orcid":"https://orcid.org/0000-0003-1274-6785","contributorId":215341,"corporation":false,"usgs":true,"family":"Rubinstein","given":"Justin","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":839996,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Yeck, William L. 0000-0002-2801-8873 wyeck@usgs.gov","orcid":"https://orcid.org/0000-0002-2801-8873","contributorId":147558,"corporation":false,"usgs":true,"family":"Yeck","given":"William","email":"wyeck@usgs.gov","middleInitial":"L.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":839997,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Earle, Paul S. 0000-0002-3500-017X pearle@usgs.gov","orcid":"https://orcid.org/0000-0002-3500-017X","contributorId":173551,"corporation":false,"usgs":true,"family":"Earle","given":"Paul","email":"pearle@usgs.gov","middleInitial":"S.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":839998,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Gok, Rengin","contributorId":289899,"corporation":false,"usgs":false,"family":"Gok","given":"Rengin","email":"","affiliations":[{"id":62279,"text":"Lawrence Livermore National Laboratory, Livermore, CA, USA","active":true,"usgs":false}],"preferred":false,"id":839999,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Walter, William R.","contributorId":289900,"corporation":false,"usgs":false,"family":"Walter","given":"William","email":"","middleInitial":"R.","affiliations":[{"id":62279,"text":"Lawrence Livermore National Laboratory, Livermore, CA, USA","active":true,"usgs":false}],"preferred":false,"id":840000,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70229532,"text":"70229532 - 2022 - Factors affecting nest success of colonial nesting waterbirds in southwest Louisiana","interactions":[],"lastModifiedDate":"2022-03-28T16:57:27.539992","indexId":"70229532","displayToPublicDate":"2021-08-27T09:49:21","publicationYear":"2022","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":"Factors affecting nest success of colonial nesting waterbirds in southwest Louisiana","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Subsidence and accelerated sea level rise impact nesting area availability and flood probabilities of breeding islands for colonial nesting waterbirds. In 2017 and 2018, we monitored 855 nests of four species of colonial nesting waterbirds on Rabbit Island, LA, to determine factors affecting nest and chick success. Based on logistic exposure models of nests, tricolored herons had the greatest likelihood of survival to hatch (mean&nbsp;(95% confidence interval))&nbsp;(77% (65.9–83.1%)), followed by brown pelicans (70% (59.9–98.5%)), roseate spoonbills (70% (38.9–83.8%)), and Forster’s terns (12% (10.7–12.2%)). Likelihood of survival to fledge was highest for tricolored herons (32% (12.8–40.7%)), followed by brown pelicans (28% (19.5–28.6%)), roseate spoonbills (47% (43.7–53.3%)), and Forster’s terns (0% (0.005–0.01%)). Nesting strategy and nest timing impacted survival rate; however, the effect depended on timing of inundation events as the timing of inundation events varied across years. Flooding was the primary cause of nest failure for most species. In 2003–2012, rapid expansion in brown pelican colony numbers and significant chick production occurred at Rabbit Island, but hydrologic records indicate no island inundation occurred during the breeding season from the beginning of the hydrologic record (2006) through 2011. Thus, our results contrast with those of previous studies conducted under different hydrologic conditions and demonstrate the challenges of short-term studies informing coastal restoration in a system that is influenced by multi-year to multi-decadal climatic cycles.</p></div></div><div id=\"cobranding-and-download-availability-text\" class=\"note test-pdf-link\"><br></div>","language":"English","publisher":"Springer Link","doi":"10.1007/s12237-021-00993-4","usgsCitation":"Ritenour, K., King, S.L., Collins, S.M., and Kaller, M., 2022, Factors affecting nest success of colonial nesting waterbirds in southwest Louisiana: Estuaries and Coasts, v. 45, p. 897-912, https://doi.org/10.1007/s12237-021-00993-4.","productDescription":"16 p.","startPage":"897","endPage":"912","ipdsId":"IP-126736","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":489112,"rank":0,"type":{"id":41,"text":"Open Access External Repository 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 \"}}]}","volume":"45","noUsgsAuthors":false,"publicationDate":"2021-08-27","publicationStatus":"PW","contributors":{"authors":[{"text":"Ritenour, K.","contributorId":288348,"corporation":false,"usgs":false,"family":"Ritenour","given":"K.","affiliations":[{"id":5115,"text":"Louisiana State University","active":true,"usgs":false}],"preferred":false,"id":837772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Sammy L. 0000-0002-5364-6361 sking@usgs.gov","orcid":"https://orcid.org/0000-0002-5364-6361","contributorId":557,"corporation":false,"usgs":true,"family":"King","given":"Sammy","email":"sking@usgs.gov","middleInitial":"L.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":837773,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, S. M.","contributorId":273184,"corporation":false,"usgs":false,"family":"Collins","given":"S.","email":"","middleInitial":"M.","affiliations":[{"id":7122,"text":"University of Wisconsin","active":true,"usgs":false}],"preferred":false,"id":837774,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kaller, M.D.","contributorId":288351,"corporation":false,"usgs":false,"family":"Kaller","given":"M.D.","affiliations":[{"id":5115,"text":"Louisiana State University","active":true,"usgs":false}],"preferred":false,"id":837775,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70227377,"text":"70227377 - 2022 - Basin and site effects in the U.S. Pacific Northwest estimated from small‐magnitude earthquakes","interactions":[],"lastModifiedDate":"2022-02-15T16:24:50.654097","indexId":"70227377","displayToPublicDate":"2021-08-24T07:03:29","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Basin and site effects in the U.S. Pacific Northwest estimated from small‐magnitude earthquakes","docAbstract":"<div class=\"article-section-wrapper js-article-section js-content-section  \"><p>Earthquake hazards in the U.S. Pacific Northwest (PNW) are increased by the presence of deep sedimentary basins that amplify and prolong ground shaking. To better understand basin and site effects on ground motions, we compile a database of recordings from crustal and intraslab earthquakes. We process 8028 records with magnitudes from 3.5 to 6.8 and hypocentral depths up to 62&nbsp;km to compute Fourier amplitude spectra of ground acceleration for frequencies of 0–20&nbsp;Hz. We compute residuals relative to the<span>&nbsp;</span>Bayless and Abrahamson (2019; hereafter, BA18) ground‐motion model and perform a series of linear, crossed, mixed‐effects regressions. In addition to estimating the bias, event, and site terms, we incorporate groupings for broad regionalized site response in three different regions (Seattle basin, Puget Lowland, non‐Puget Lowland), for effects from seismotectonic regime (crustal and intraslab sources), and for interactions between the regions and seismotectonic regimes. We find that the scaling of site response with respect to<span>&nbsp;</span><span class=\"inline-formula no-formula-id\"><span class=\"MathJax_Preview\"><span id=\"MJXp-Span-1\" class=\"MJXp-math\"><span id=\"MJXp-Span-2\" class=\"MJXp-msub\"><span id=\"MJXp-Span-3\" class=\"MJXp-mi MJXp-italic\">V</span><span id=\"MJXp-Span-4\" class=\"MJXp-mrow MJXp-script\"><span id=\"MJXp-Span-5\" class=\"MJXp-mi MJXp-italic\">S</span><span id=\"MJXp-Span-6\" class=\"MJXp-mn\">30</span></span></span></span></span></span><span>&nbsp;</span>(time‐averaged shear‐wave velocity from the surface to a depth of 30&nbsp;m) and to basin depth indicators<span>&nbsp;</span><span class=\"inline-formula no-formula-id\"><span class=\"MathJax_Preview\"><span id=\"MJXp-Span-7\" class=\"MJXp-math\"><span id=\"MJXp-Span-8\" class=\"MJXp-msub\"><span id=\"MJXp-Span-9\" class=\"MJXp-mi MJXp-italic\">Z</span><span id=\"MJXp-Span-10\" class=\"MJXp-mn MJXp-script\">1.0</span></span></span></span></span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"inline-formula no-formula-id\"><span class=\"MathJax_Preview\"><span id=\"MJXp-Span-11\" class=\"MJXp-math\"><span id=\"MJXp-Span-12\" class=\"MJXp-msub\"><span id=\"MJXp-Span-13\" class=\"MJXp-mi MJXp-italic\">Z</span><span id=\"MJXp-Span-14\" class=\"MJXp-mn MJXp-script\">2.5</span></span></span></span></span><span>&nbsp;</span>(depths to the 1.0 and 2.5&nbsp;km/s shear‐wave velocity horizons) is generally consistent with BA18; however, the region terms display strong spatial amplification patterns. For frequencies less than 5&nbsp;Hz, the Seattle basin amplifies ground motions up to a factor of four, relative to the non‐Puget Lowland, with a maximum amplification around near 0.5&nbsp;Hz. Sites in the Puget Lowland amplify low frequencies up to a factor of 2.5. At higher frequencies (<span class=\"inline-formula no-formula-id\">⁠<span class=\"MathJax_Preview\"><span id=\"MJXp-Span-15\" class=\"MJXp-math\"><span id=\"MJXp-Span-16\" class=\"MJXp-mi MJXp-italic\">f</span><span id=\"MJXp-Span-17\" class=\"MJXp-mo\">&gt;</span><span id=\"MJXp-Span-18\" class=\"MJXp-mn\">5</span><span id=\"MJXp-Span-19\" class=\"MJXp-mtext\">  </span><span id=\"MJXp-Span-20\" class=\"MJXp-mi\">Hz</span></span></span>⁠</span>), the Puget Lowland and Seattle basin show regional deamplification of ground motions, with the smallest average amplification factor of 0.65 occurring at 10.0&nbsp;Hz. Although we observe slight differences in the seismotectonic regime terms, we find that the region terms are significantly more important for modeling earthquake hazard in the PNW.</p></div>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120210029","usgsCitation":"Rekoske, J., Moschetti, M.P., and Thompson, E.M., 2022, Basin and site effects in the U.S. Pacific Northwest estimated from small‐magnitude earthquakes: Bulletin of the Seismological Society of America, v. 112, no. 1, p. 438-456, https://doi.org/10.1785/0120210029.","productDescription":"19 p.","startPage":"438","endPage":"456","ipdsId":"IP-129686","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":436058,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9BUCRF7","text":"USGS data release","linkHelpText":"Database of horizontal component Fourier amplitude spectra of acceleration ground motions from Pacific Northwest earthquakes"},{"id":394240,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, 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 \"}}]}","volume":"112","issue":"1","noUsgsAuthors":false,"publicationDate":"2021-08-24","publicationStatus":"PW","contributors":{"authors":[{"text":"Rekoske, John 0000-0003-0539-2069","orcid":"https://orcid.org/0000-0003-0539-2069","contributorId":220108,"corporation":false,"usgs":true,"family":"Rekoske","given":"John","email":"","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":830664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moschetti, Morgan P. 0000-0001-7261-0295 mmoschetti@usgs.gov","orcid":"https://orcid.org/0000-0001-7261-0295","contributorId":1662,"corporation":false,"usgs":true,"family":"Moschetti","given":"Morgan","email":"mmoschetti@usgs.gov","middleInitial":"P.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":830665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, Eric M. 0000-0002-6943-4806 emthompson@usgs.gov","orcid":"https://orcid.org/0000-0002-6943-4806","contributorId":150897,"corporation":false,"usgs":true,"family":"Thompson","given":"Eric","email":"emthompson@usgs.gov","middleInitial":"M.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":830666,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70223709,"text":"70223709 - 2022 - Physiological and nutritional constraints on zooplankton productivity due to eutrophication and climate change predicted using a resource-based modeling approach","interactions":[],"lastModifiedDate":"2022-03-15T15:59:58.012303","indexId":"70223709","displayToPublicDate":"2021-08-23T07:40:11","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Physiological and nutritional constraints on zooplankton productivity due to eutrophication and climate change predicted using a resource-based modeling approach","docAbstract":"<div id=\"abstracts\"><div class=\"core-container\"><div>Emerging evidence suggests that zooplankton production is affected by physiological and nutritional constraints due to climate change and eutrophication, which in turn could have broad implications for food-web dynamics and fisheries production. In this study, we developed a resource-based zooplankton production dynamics model that causally links freshwater cladoceran and copepod daily production-to-biomass (P/B) ratios with water temperature, phytoplankton biomass and community composition, and zooplankton feeding selectivity. This model was used to evaluate constraints on zooplankton growth under four hypothetical scenarios: involving natural plankton community seasonal succession; lake fertilization to enhance fisheries production; eutrophication; and climatic warming. Our novel modeling approach predicts zooplankton production is strongly dependent on seasonal variation in resource availability and quality, which results in more complex zooplankton dynamics than predicted by simpler temperature dependent models. For mesotrophic and hypereutrophic lakes, our study suggests that the ultimate control over zooplankton P/B ratios shifts from physiological control during colder periods to strong resource control during warmer periods. Our resource-based model provided important insights into the nature of biophysical control of zooplankton under a changing climate that has crucial implications for food web energy transfer and fisheries production.</div></div></div>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/cjfas-2021-0071","usgsCitation":"Zhang, C., Brett, M.T., Nielsen, J.M., Arhonditsis, G.B., Ballantyne, A.P., Carter, J.L., Kann, J., Muller-Navarra, D.C., Schindler, D., Stockwell, J.D., Winder, M., and Beauchamp, D., 2022, Physiological and nutritional constraints on zooplankton productivity due to eutrophication and climate change predicted using a resource-based modeling approach: Canadian Journal of Fisheries and Aquatic Sciences, v. 79, no. 3, p. 472-486, https://doi.org/10.1139/cjfas-2021-0071.","productDescription":"15 p.","startPage":"472","endPage":"486","ipdsId":"IP-107589","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":449738,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://www.nrcresearchpress.com/doi/abs/10.1139/cjfas-2021-0071","text":"External Repository"},{"id":388799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zhang, Chen","contributorId":265168,"corporation":false,"usgs":false,"family":"Zhang","given":"Chen","email":"","affiliations":[{"id":54619,"text":"Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington 98195, USA","active":true,"usgs":false}],"preferred":false,"id":822397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brett, Michael T.","contributorId":261402,"corporation":false,"usgs":false,"family":"Brett","given":"Michael","email":"","middleInitial":"T.","affiliations":[{"id":52844,"text":"Civil and Environmental Engineering, University of Washington, Seattle, USA","active":true,"usgs":false}],"preferred":false,"id":822398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nielsen, Jens M","contributorId":265169,"corporation":false,"usgs":false,"family":"Nielsen","given":"Jens","email":"","middleInitial":"M","affiliations":[{"id":54619,"text":"Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington 98195, USA","active":true,"usgs":false}],"preferred":false,"id":822399,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arhonditsis, George B","contributorId":265170,"corporation":false,"usgs":false,"family":"Arhonditsis","given":"George","email":"","middleInitial":"B","affiliations":[{"id":54621,"text":"Ecological Modeling Laboratory, Department of Physical & Environmental Sciences, University of Toronto, Toronto, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":822400,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ballantyne, Ashley P","contributorId":166784,"corporation":false,"usgs":false,"family":"Ballantyne","given":"Ashley","email":"","middleInitial":"P","affiliations":[{"id":24513,"text":"Department of Ecosystem and Conservation Sciences, University of Montana, Missoula, MT 59812, USA","active":true,"usgs":false}],"preferred":false,"id":822401,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carter, Jackie L","contributorId":265171,"corporation":false,"usgs":false,"family":"Carter","given":"Jackie","email":"","middleInitial":"L","affiliations":[{"id":54623,"text":"School of Aquatic and Fishery Sciences, University of Washington, Seattle, Washington 98195, USA","active":true,"usgs":false}],"preferred":false,"id":822402,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kann, Jacob","contributorId":265172,"corporation":false,"usgs":false,"family":"Kann","given":"Jacob","email":"","affiliations":[{"id":54624,"text":"Aquatic Ecosystem Sciences, LLC, 295 East Main St., Suite 7, Ashland, OR 97520, USA","active":true,"usgs":false}],"preferred":false,"id":822403,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Muller-Navarra, Dorthe C","contributorId":265173,"corporation":false,"usgs":false,"family":"Muller-Navarra","given":"Dorthe","email":"","middleInitial":"C","affiliations":[{"id":54625,"text":"University of Hamburg, Aquatic Ecology, Hamburg, Germany","active":true,"usgs":false}],"preferred":false,"id":822404,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schindler, Daniel E.","contributorId":223885,"corporation":false,"usgs":false,"family":"Schindler","given":"Daniel E.","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":822405,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Stockwell, Jason D. 0000-0003-3393-6799","orcid":"https://orcid.org/0000-0003-3393-6799","contributorId":61004,"corporation":false,"usgs":false,"family":"Stockwell","given":"Jason","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":822406,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Winder, Monika","contributorId":196556,"corporation":false,"usgs":false,"family":"Winder","given":"Monika","email":"","affiliations":[],"preferred":false,"id":822407,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Beauchamp, David 0000-0002-3592-8381","orcid":"https://orcid.org/0000-0002-3592-8381","contributorId":217816,"corporation":false,"usgs":true,"family":"Beauchamp","given":"David","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":822408,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70229452,"text":"70229452 - 2022 - Connecting regional-scale tree distribution models with seed dispersal kernels","interactions":[],"lastModifiedDate":"2022-03-09T15:55:47.176117","indexId":"70229452","displayToPublicDate":"2021-08-22T09:50:01","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":10270,"text":"Applied Mathematics and Computation","active":true,"publicationSubtype":{"id":10}},"title":"Connecting regional-scale tree distribution models with seed dispersal kernels","docAbstract":"<p><span>Regional scale forest distribution models are important tools for biogeography and understanding the structure of forest communities in space. These models take climate and geographic variables as input and are therefore helpful for long-term decision support and climate adaptation planning. Generally, local processes of tree germination and seedling survival are resolved probabilistically with explanatory variables such as elevation, latitude, exposure, soil type, moisture availability, climate and weather inputs and `trained’ using landscape and regional presence-absence data and machine learning techniques. How seeds are distributed in these models, that is, determining the dispersal kernel, is far more problematic. The challenge is that variables conditioning vertebrate seed dispersal (motility and probability of utilization or caching in response to cover type) are not represented in large scale distribution models, and in fact vary on scales (10-100 meters) that are much smaller than the smallest pixel size for the distribution model (1-10 kilometers). We present a homogenized seed digestion kernel (HSDK) which incorporates this scale separation. Homogenization naturally links highly variable small-scale processes (like seed foraging and caching by birds and rodents) with large scale effects (like dispersal of seeds over tens of kilometers). We develop a homogenization strategy to predict seed dispersal on landscape scales, analytically linking small-scale variables (landscape fraction cover by tree type, gut residence times and cover type utilization by frugivorous birds) with large scale behaviors. Closed form approximations are developed in two dimensions for two limiting cases of seed handling behavior, and the approach is illustrated using landscape data and piñon-pine dispersal in a 630,000 square kilometer region in the southwestern US.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.amc.2021.126591","usgsCitation":"Neupane, R.C., Powell, J., and Edwards, T., 2022, Connecting regional-scale tree distribution models with seed dispersal kernels: Applied Mathematics and Computation, v. 412, 126591, 17 p., https://doi.org/10.1016/j.amc.2021.126591.","productDescription":"126591, 17 p.","ipdsId":"IP-124972","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":449740,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.amc.2021.126591","text":"Publisher Index Page"},{"id":396921,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"412","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Neupane, Ram C.","contributorId":288149,"corporation":false,"usgs":false,"family":"Neupane","given":"Ram","email":"","middleInitial":"C.","affiliations":[{"id":61709,"text":"ta&m","active":true,"usgs":false}],"preferred":false,"id":837519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, James A.","contributorId":288150,"corporation":false,"usgs":false,"family":"Powell","given":"James A.","affiliations":[{"id":28050,"text":"USU","active":true,"usgs":false}],"preferred":false,"id":837520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Thomas C. Jr. 0000-0002-0773-0909 tce@usgs.gov","orcid":"https://orcid.org/0000-0002-0773-0909","contributorId":191916,"corporation":false,"usgs":true,"family":"Edwards","given":"Thomas C.","suffix":"Jr.","email":"tce@usgs.gov","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":837518,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70224338,"text":"70224338 - 2022 - Solutions in microbiome engineering: Prioritizing barriers to organism establishment","interactions":[],"lastModifiedDate":"2022-01-25T16:50:53.459975","indexId":"70224338","displayToPublicDate":"2021-08-21T07:11:49","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":9357,"text":"The ISME Journal: Multidisciplinary Journal of Microbial Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Solutions in microbiome engineering: Prioritizing barriers to organism establishment","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Microbiome engineering is increasingly being employed as a solution to challenges in health, agriculture, and climate. Often manipulation involves inoculation of new microbes designed to improve function into a preexisting microbial community. Despite, increased efforts in microbiome engineering inoculants frequently fail to establish and/or confer long-lasting modifications on ecosystem function. We posit that one underlying cause of these shortfalls is the failure to consider barriers to organism establishment. This is a key challenge and focus of macroecology research, specifically invasion biology and restoration ecology. We adopt a framework from invasion biology that summarizes establishment barriers in three categories: (1) propagule pressure, (2) environmental filtering, and (3) biotic interactions factors. We suggest that biotic interactions is the most neglected factor in microbiome engineering research, and we recommend a number of actions to accelerate engineering solutions.</p></div></div>","language":"English","publisher":"Nature","doi":"10.1038/s41396-021-01088-5","usgsCitation":"Albright, M., Louca, S., Winkler, D.E., Feeser, K.L., Haig, S., Whiteson, K.L., Emerson, J.B., and Dunbar, J.M., 2022, Solutions in microbiome engineering: Prioritizing barriers to organism establishment: The ISME Journal: Multidisciplinary Journal of Microbial Ecology, v. 16, p. 331-338, https://doi.org/10.1038/s41396-021-01088-5.","productDescription":"8 p.","startPage":"331","endPage":"338","ipdsId":"IP-127565","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":449741,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/s41396-021-01088-5","text":"Publisher Index Page"},{"id":389634,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","noUsgsAuthors":false,"publicationDate":"2021-08-21","publicationStatus":"PW","contributors":{"authors":[{"text":"Albright, Michaeline B.N.","contributorId":265940,"corporation":false,"usgs":false,"family":"Albright","given":"Michaeline B.N.","affiliations":[{"id":54832,"text":"Bioscience Division, Los Alamos National Laboratory, NM","active":true,"usgs":false}],"preferred":false,"id":823814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Louca, Stilianos","contributorId":195708,"corporation":false,"usgs":false,"family":"Louca","given":"Stilianos","email":"","affiliations":[],"preferred":false,"id":823815,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winkler, Daniel E. 0000-0003-4825-9073","orcid":"https://orcid.org/0000-0003-4825-9073","contributorId":206786,"corporation":false,"usgs":true,"family":"Winkler","given":"Daniel","email":"","middleInitial":"E.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":823816,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Feeser, Kelli L.","contributorId":265941,"corporation":false,"usgs":false,"family":"Feeser","given":"Kelli","email":"","middleInitial":"L.","affiliations":[{"id":54832,"text":"Bioscience Division, Los Alamos National Laboratory, NM","active":true,"usgs":false}],"preferred":false,"id":823817,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haig, Sarah-Jane","contributorId":265942,"corporation":false,"usgs":false,"family":"Haig","given":"Sarah-Jane","email":"","affiliations":[{"id":54833,"text":"Department of Civil and Environmental Engineering, University of Pittsburg, PA","active":true,"usgs":false}],"preferred":false,"id":823818,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whiteson, Katrine L.","contributorId":265943,"corporation":false,"usgs":false,"family":"Whiteson","given":"Katrine","email":"","middleInitial":"L.","affiliations":[{"id":54834,"text":"Department of Molecular Biology and Biochemistry, University of California, Irvine, CA","active":true,"usgs":false}],"preferred":false,"id":823819,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Emerson, Joanne B.","contributorId":265944,"corporation":false,"usgs":false,"family":"Emerson","given":"Joanne","email":"","middleInitial":"B.","affiliations":[{"id":54835,"text":"Department of Plant Pathology, University of California, Davis, CA","active":true,"usgs":false}],"preferred":false,"id":823820,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Dunbar, John M.","contributorId":105778,"corporation":false,"usgs":false,"family":"Dunbar","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":823821,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70228693,"text":"70228693 - 2022 - Mg/Ca ratios in ostracode genera Sarsicytheridea and Paracyprideis: A potential paleotemperature proxy for Arctic and subarctic continental shelf and slope waters","interactions":[],"lastModifiedDate":"2022-06-16T15:18:01.516771","indexId":"70228693","displayToPublicDate":"2021-08-19T11:30:39","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Mg/Ca ratios in ostracode genera <i>Sarsicytheridea</i> and <i>Paracyprideis</i>: A potential paleotemperature proxy for Arctic and subarctic continental shelf and slope waters","title":"Mg/Ca ratios in ostracode genera Sarsicytheridea and Paracyprideis: A potential paleotemperature proxy for Arctic and subarctic continental shelf and slope waters","docAbstract":"We evaluate the potential utility of Mg/Ca ratios in the sublittoral ostracode genera Sarsicytheridea and Paracyprideis as a paleotemperature proxy for continental shelf and upper slope waters of the Arctic Ocean and adjacent seas. Using sediment core-top and surface sediment samples, the shells of three species, S. bradii, S. punctillata, and P. pseudopunctillata, were analyzed from Arctic Ocean sites ranging in water depth from 7 to 200 meters and bottom-water temperatures (BWT) of -1.5 °C to 12 °C. Generally, Mg/Ca ratios range from 4 to 9 mmol/mol. The results show excellent agreement with the range of Mg/Ca ratios obtained in a previous study by Ingram (1998) of core-top shells of Sarsicytheridea from the sub-polar North Atlantic Ocean and adjacent seas, with BWT ranging from 1 to 11.4 °C. However, unlike this previous study of Sarsicytheridea, and previous work on the Arctic ostracode marine genus Krithe showing strong correlations between Mg/Ca and BWT, Mg/Ca ratios in Arctic specimens analyzed here are not correlated with BWT below 0°C. We hypothesize that this has to do with uncertainty regarding the actual ambient BWT at the time of shell secretion.  As with many continental shelf sites, the individual sites used in the study have large interannual and seasonal variations in BWT, in some cases >5-8 °C. Thus, there is considerable difficulty in assigning a proper shell secretion temperature and, in turn, fully assessing the utility of Sarsicytheridea Mg/Ca ratios as a paleotemperature proxy below 0 °C. There are a number of possible solutions, such as laboratory culturing of these genera under controlled conditions, adding additional sites with a range of maximal and minimal bottom water temperatures, and pairing other geochemical or isotopic measures of temperature, among others. Regardless, the good overall calibration of Mg/Ca results from samples with temperatures above 0 °C is encouraging and justifies continued evaluation of this potential paleothermometer for Arctic continental shelf and upper slope environments.","language":"English","publisher":"Elsevier","doi":"10.1016/j.marmicro.2021.102035","usgsCitation":"Cronin, T.M., Dwyer, G.S., Keller, K., Gemery, L., and Farmer, J., 2022, Mg/Ca ratios in ostracode genera Sarsicytheridea and Paracyprideis: A potential paleotemperature proxy for Arctic and subarctic continental shelf and slope waters: Marine Micropaleontology, v. 174, 102035, 8 p., https://doi.org/10.1016/j.marmicro.2021.102035.","productDescription":"102035, 8 p.","ipdsId":"IP-125258","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":396120,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Arctic Ocean","volume":"174","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cronin, Thomas M. 0000-0002-2643-0979 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":2579,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":835090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dwyer, Gary S.","contributorId":197070,"corporation":false,"usgs":false,"family":"Dwyer","given":"Gary","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":835091,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keller, Katherine 0000-0001-6915-5455","orcid":"https://orcid.org/0000-0001-6915-5455","contributorId":218048,"corporation":false,"usgs":false,"family":"Keller","given":"Katherine","email":"","affiliations":[{"id":39732,"text":"Natural Systems Analysts, Harvard University","active":true,"usgs":false}],"preferred":false,"id":835092,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gemery, Laura 0000-0003-1966-8732 lgemery@usgs.gov","orcid":"https://orcid.org/0000-0003-1966-8732","contributorId":279524,"corporation":false,"usgs":true,"family":"Gemery","given":"Laura","email":"lgemery@usgs.gov","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":835093,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Farmer, Jesse R.","contributorId":279525,"corporation":false,"usgs":false,"family":"Farmer","given":"Jesse R.","affiliations":[{"id":6644,"text":"Princeton University","active":true,"usgs":false}],"preferred":false,"id":835094,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70223849,"text":"70223849 - 2022 - Incorporating antenna detections into abundance estimates of fish","interactions":[],"lastModifiedDate":"2022-03-15T16:01:40.457204","indexId":"70223849","displayToPublicDate":"2021-08-18T06:57:14","publicationYear":"2022","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Incorporating antenna detections into abundance estimates of fish","docAbstract":"<div id=\"abstracts\"><div class=\"core-container\"><div>Autonomous passive integrated transponder (PIT) tag antennas are commonly used to detect fish marked with PIT tags but cannot detect unmarked fish, creating challenges for abundance estimation. Here we describe an approach to estimate abundance from paired physical capture and antenna detection data in closed and open mark-recapture models. Additionally, for open models, we develop an approach that incorporates uncertainty in fish size, because fish size changes through time (as fish grow bigger) but is unknown if fish are not physically captured (e.g., only detected on antennas). Incorporation of size uncertainty allows for estimation of size-specific abundances and demonstrates a generally useful method for obtaining state-specific abundances estimates under state uncertainty. Simulation studies comparing models with and without antenna detections illustrate that the benefit of our approach increases as a larger proportion of the population is marked. When applied to two field data sets, our approach to incorporating antenna detections reduced uncertainty in abundance substantially. We conclude that PIT antennas hold great potential for improving abundance estimation, despite the challenges they present.</div></div></div>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/cjfas-2021-0003","usgsCitation":"Dzul, M.C., Yackulic, C., Kendall, W.L., Winkelman, D.L., Conner, M.M., and Yard, M.D., 2022, Incorporating antenna detections into abundance estimates of fish: Canadian Journal of Fisheries and Aquatic Sciences, v. 79, no. 3, p. 436-447, https://doi.org/10.1139/cjfas-2021-0003.","productDescription":"12 p.","startPage":"436","endPage":"447","ipdsId":"IP-125707","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":449745,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1807/109444","text":"External Repository"},{"id":436059,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9ZCNR6X","text":"USGS data release","linkHelpText":"Humpback chub (Gila cypha) capture history data (2009-2020), Grand Canyon, Arizona"},{"id":389049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dzul, Maria C. 0000-0002-4798-5930 mdzul@usgs.gov","orcid":"https://orcid.org/0000-0002-4798-5930","contributorId":5469,"corporation":false,"usgs":true,"family":"Dzul","given":"Maria","email":"mdzul@usgs.gov","middleInitial":"C.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":822926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yackulic, Charles B. 0000-0001-9661-0724","orcid":"https://orcid.org/0000-0001-9661-0724","contributorId":218825,"corporation":false,"usgs":true,"family":"Yackulic","given":"Charles","middleInitial":"B.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":822927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kendall, William L. 0000-0003-0084-9891","orcid":"https://orcid.org/0000-0003-0084-9891","contributorId":204844,"corporation":false,"usgs":true,"family":"Kendall","given":"William","email":"","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":822928,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winkelman, Dana L. 0000-0002-5247-0114 danaw@usgs.gov","orcid":"https://orcid.org/0000-0002-5247-0114","contributorId":4141,"corporation":false,"usgs":true,"family":"Winkelman","given":"Dana","email":"danaw@usgs.gov","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":822929,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Conner, Mary M","contributorId":222152,"corporation":false,"usgs":false,"family":"Conner","given":"Mary","email":"","middleInitial":"M","affiliations":[{"id":6682,"text":"Utah State University","active":true,"usgs":false}],"preferred":false,"id":822930,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Yard, Michael D. 0000-0002-6580-6027 myard@usgs.gov","orcid":"https://orcid.org/0000-0002-6580-6027","contributorId":169281,"corporation":false,"usgs":true,"family":"Yard","given":"Michael","email":"myard@usgs.gov","middleInitial":"D.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":822931,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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