{"pageNumber":"1272","pageRowStart":"31775","pageSize":"25","recordCount":165309,"records":[{"id":70132467,"text":"ofr20141201 - 2014 - Geologic and geophysical data for wells drilled at Raft River Valley, Cassia County, Idaho, in 1977-1978 and data for wells drilled previously","interactions":[],"lastModifiedDate":"2014-11-06T10:50:35","indexId":"ofr20141201","displayToPublicDate":"2014-11-04T10:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-1201","title":"Geologic and geophysical data for wells drilled at Raft River Valley, Cassia County, Idaho, in 1977-1978 and data for wells drilled previously","docAbstract":"<p>In order to better define the size of the thermal anomaly in the Raft River Valley, Idaho, the U.S. Geological Survey drilled a series of intermediate-depth (nominal 500-ft depth) wells in 1977 and 1978. &nbsp;This report presents geologic, geophysical, and temperature data for these drill holes, along with data for five wells drilled by the Idaho National Engineering Laboratory with U.S. Department of Energy Funding. &nbsp;Data previously reported for other drill holes are also included in order to make them available as digital files.</p>\n<p>&nbsp;</p>\n<p>For purposes of defining the thermal anomaly for the geothermal system, temperature gradients are calculated over long depth intervals on the basis of the appearance of reasonable linear segments on a temperature versus plot depth. &nbsp;Temperature versus depth data for some drill holes can be represented by a single gradient, whereas others require multiple gradients to match the data. &nbsp;Data for some drill holes clearly reflect vertical flows of water in the formation surrounding the drill holes, and water velocities are calculated for these drill holes. &nbsp;Within The Narrows area, temperature versus depth data show reversals at different depth in different drill holes. &nbsp;In the main thermal area, temperatures in intermediate-depth drill holes vary approximately linearly but with very high values of temperature gradient. &nbsp;Temperature gradients on a map of the area can be reasonable divided into a large area of regional gradients and smaller areas defining the thermal anomalies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20141201","usgsCitation":"Nathenson, M., Urban, T.C., and Covington, H., 2014, Geologic and geophysical data for wells drilled at Raft River Valley, Cassia County, Idaho, in 1977-1978 and data for wells drilled previously: U.S. Geological Survey Open-File Report 2014-1201, Report: iv, 30 p.; 2 Appendixes, https://doi.org/10.3133/ofr20141201.","productDescription":"Report: iv, 30 p.; 2 Appendixes","numberOfPages":"34","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-052136","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":295850,"rank":9,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20141201.JPG"},{"id":295822,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2014/1201/"},{"id":295844,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2014/1201/pdf/ofr20141201_appendixA.pdf"},{"id":295843,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2014/1201/pdf/ofr2014-1201.pdf"},{"id":295845,"rank":4,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2014/1201/pdf/ofr20141201_appendixB.pdf"},{"id":295846,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2014/1201/pdf/ofr20141201_appendixA_figs.pdf"},{"id":295847,"rank":6,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2014/1201/downloads/ofr20141201_appendixA_tables.zip"},{"id":295848,"rank":7,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2014/1201/pdf/ofr20141201_appendixB_figs.pdf"},{"id":295849,"rank":8,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2014/1201/downloads/ofr20141201_appendixB_tables.zip"}],"country":"United States","state":"Idaho","county":"Cassia County","otherGeospatial":"Raft River Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5459eaa1e4b009f8aec96fe4","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":522919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Urban, Thomas C.","contributorId":53949,"corporation":false,"usgs":true,"family":"Urban","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":522920,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Covington, Harry R.","contributorId":101309,"corporation":false,"usgs":true,"family":"Covington","given":"Harry R.","affiliations":[],"preferred":false,"id":522921,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70127080,"text":"sir20145182 - 2014 - Simulation of hydrologic conditions and suspended-sediment loads in the San Antonio River Basin downstream from San Antonio, Texas, 2000-12","interactions":[],"lastModifiedDate":"2016-08-05T12:08:21","indexId":"sir20145182","displayToPublicDate":"2014-11-04T09:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-5182","title":"Simulation of hydrologic conditions and suspended-sediment loads in the San Antonio River Basin downstream from San Antonio, Texas, 2000-12","docAbstract":"<p>Suspended sediment in rivers and streams can play an&nbsp;important role in ecological health of rivers and estuaries&nbsp;and consequently is an important issue for water-resource managers. To better understand suspended-sediment loads and transport in a watershed, the U.S. Geological Survey (USGS), in cooperation with the San Antonio River Authority, developed a Hydrological Simulation Program&mdash;FORTRAN model to simulate hydrologic conditions and suspended-sediment loads during&nbsp;2000&ndash;12 for four watersheds, which comprise the overall study area in the San Antonio River Basin (hereinafter referred to as the &ldquo;USGS&ndash;2014 model&rdquo;). The study area consists of approximately 2,150 square miles encompassing parts of Bexar, Guadalupe, Wilson, Karnes, DeWitt, Goliad, Victoria, and Refugio Counties. The USGS&ndash;2014 model was calibrated for hydrology and suspended sediment for 2006&ndash;12. Overall, model-fit statistics and graphic evaluations from the calibration and testing periods provided multiple lines of evidence indicating that the USGS&ndash;2014 model simulations of hydrologic and suspended-sediment conditions were mostly&nbsp;&ldquo;good&rdquo; to &ldquo;very good.&rdquo; Model simulation results indicated that approximately 1,230&nbsp;tons per day of suspended sediment exited the study area and were delivered to the Guadalupe River during 2006&ndash;12, of which approximately 62 percent originated upstream from the study area. Sample data and simulated model results indicate that most of the suspended-sediment load in the study area consisted of silt- and clay-sized particles (less than 0.0625&nbsp;millimeters). The Cibolo Creek watershed was the largest contributor of suspended sediment from the study area. For the entire study area, open/developed land and cropland exhibited the highest simulated soil erosion rates; however, the largest contributions of sediment (by land-cover type) were pasture and forest/rangeland/shrubland, which together composed approximately 80&nbsp;percent of the land cover of the study area and generated about 70 percent of the suspended-sediment load from the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20145182","collaboration":"Prepared in cooperation with the San Antonio River Authority","usgsCitation":"Banta, J., and Ockerman, D.J., 2014, Simulation of hydrologic conditions and suspended-sediment loads in the San Antonio River Basin downstream from San Antonio, Texas, 2000-12: U.S. Geological Survey Scientific Investigations Report 2014-5182, v, 46 p., https://doi.org/10.3133/sir20145182.","productDescription":"v, 46 p.","numberOfPages":"56","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2000-01-01","temporalEnd":"2012-12-31","ipdsId":"IP-056710","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":295842,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20145182.jpg"},{"id":295821,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2014/5182/"},{"id":295841,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2014/5182/pdf/sir2014-5182.pdf"}],"country":"United States","state":"Texas","city":"San Antonio","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5459eaa3e4b009f8aec97016","contributors":{"authors":[{"text":"Banta, J. Ryan 0000-0002-2226-7270 jbanta@usgs.gov","orcid":"https://orcid.org/0000-0002-2226-7270","contributorId":4723,"corporation":false,"usgs":true,"family":"Banta","given":"J. Ryan","email":"jbanta@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":522917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ockerman, Darwin J. 0000-0003-1958-1688 ockerman@usgs.gov","orcid":"https://orcid.org/0000-0003-1958-1688","contributorId":1579,"corporation":false,"usgs":true,"family":"Ockerman","given":"Darwin","email":"ockerman@usgs.gov","middleInitial":"J.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":522918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70127784,"text":"ofr20141215 - 2014 - Water-quality characteristics indicative of wastewater in selected streams in the upper Neuse River Basin, Durham and Orange Counties, North Carolina, from 2004 to 2013","interactions":[],"lastModifiedDate":"2016-12-08T16:58:12","indexId":"ofr20141215","displayToPublicDate":"2014-11-04T09:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-1215","title":"Water-quality characteristics indicative of wastewater in selected streams in the upper Neuse River Basin, Durham and Orange Counties, North Carolina, from 2004 to 2013","docAbstract":"<p>Data were collected during three time periods to assess the effects of wastewater treatment and disposal practices on the occurrence of selected contaminants indicative of wastewater in the upper Neuse River Basin, North Carolina. The first phase of data collection, December 2004 to June 2005, and the second phase, April to October 2008, addressed the effects of point and nonpoint sources of wastewater effluent on stream quality during baseflow conditions. Point-source effects were assessed by sampling a municipal wastewater treatment plant outfall and sites on the Eno River upstream and downstream from the outfall. Water-quality data suggest that the wastewater treatment plant effluent contributed to increases in concentrations of nitrogen and carbamazepine at the downstream site. Nonpoint source effects were assessed by sampling seven small streams that drained an undeveloped area and residential areas served by either centralized or onsite wastewater treatment systems. Samples were analyzed for inorganic constituents, including nutrients, ions, and metals; organic compounds considered indicative of wastewater contamination; antibiotics, optical brighteners, and fecal coliform bacteria. Hypothesized differences in water quality between the sites with primarily centralized and onsite wastewater treatment were not apparent, likely due to the relatively large heterogeneity of the sites within each category.</p>\n<p>&nbsp;</p>\n<p>During the third phase of data collection, May 2012 to January 2013, data were collected to address the suitability of optical brighteners as tracers of wastewater in small streams during streamflow recession. Samples were collected at five small streams following periods of rainfall and analyzed for optical brighteners, specific conductance nutrients, and selected hormones. Optical brighteners were absent in the undeveloped catchment but were present in the recession period after rainfall events in catchments with centralized though possibly leaky sewage treatment and areas with onsite treatment. Sand filter systems in areas with onsite treatment appear to change the effluent flow and retention characteristics such that optical brighteners were present both before and after rainfall events. Nitrate plus nitrite, as nitrogen concentrations in samples from this last study phase generally were larger than those collected during baseflow conditions in the previous phases of this study.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20141215","collaboration":"North Carolina Department of Environment and Natural Resources, Division of Environmental Health; Durham County Health Department; City of Durham Stormwater Department; City of Raleigh, North Carolina","usgsCitation":"Ferrell, G.M., Yearout, M.S., Grimes, B.H., Graves, A.K., Fitzgerald, S., and Meyer, M.T., 2014, Water-quality characteristics indicative of wastewater in selected streams in the upper Neuse River Basin, Durham and Orange Counties, North Carolina, from 2004 to 2013: U.S. Geological Survey Open-File Report 2014-1215, Report: xi, 62 p.; 10 Appendixes; 2 Tables, https://doi.org/10.3133/ofr20141215.","productDescription":"Report: xi, 62 p.; 10 Appendixes; 2 Tables","numberOfPages":"77","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2004-01-01","temporalEnd":"2013-12-31","ipdsId":"IP-052107","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":295840,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20141215.jpg"},{"id":295770,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2014/1215/"},{"id":295825,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2014/1215/pdf/ofr2014-1215.pdf"},{"id":295838,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2014/1215/appendix/"},{"id":295839,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2014/1215/table"}],"country":"United States","state":"North Carolina","county":"Durham County, Orange County","otherGeospatial":"Upper Neuse River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.4036865234375,\n              35.793310688351724\n            ],\n            [\n              -79.4036865234375,\n              36.22876574685929\n            ],\n            [\n              -78.63327026367188,\n              36.22876574685929\n            ],\n            [\n              -78.63327026367188,\n              35.793310688351724\n            ],\n            [\n              -79.4036865234375,\n              35.793310688351724\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5459eaa4e4b009f8aec97030","contributors":{"authors":[{"text":"Ferrell, Gloria M. gferrell@usgs.gov","contributorId":1595,"corporation":false,"usgs":true,"family":"Ferrell","given":"Gloria","email":"gferrell@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":521319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yearout, Matthew S.","contributorId":124564,"corporation":false,"usgs":false,"family":"Yearout","given":"Matthew","email":"","middleInitial":"S.","affiliations":[{"id":5039,"text":"Department of Environment, Land, and Infrastructure Engineering, Politecnico di Torino, Torino, Italy","active":true,"usgs":false}],"preferred":false,"id":521320,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grimes, Barbara H.","contributorId":124565,"corporation":false,"usgs":false,"family":"Grimes","given":"Barbara","email":"","middleInitial":"H.","affiliations":[{"id":5039,"text":"Department of Environment, Land, and Infrastructure Engineering, Politecnico di Torino, Torino, Italy","active":true,"usgs":false}],"preferred":false,"id":521321,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graves, Alexandria K.","contributorId":124566,"corporation":false,"usgs":false,"family":"Graves","given":"Alexandria","email":"","middleInitial":"K.","affiliations":[{"id":5039,"text":"Department of Environment, Land, and Infrastructure Engineering, Politecnico di Torino, Torino, Italy","active":true,"usgs":false}],"preferred":false,"id":521322,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fitzgerald, Sharon A. safitzge@usgs.gov","contributorId":4532,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"Sharon A.","email":"safitzge@usgs.gov","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":521318,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Meyer, Michael T. 0000-0001-6006-7985 mmeyer@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-7985","contributorId":866,"corporation":false,"usgs":true,"family":"Meyer","given":"Michael","email":"mmeyer@usgs.gov","middleInitial":"T.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":521323,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70127487,"text":"ofr20141206 - 2014 - Low-head hydropower assessment of the Brazilian State of São Paulo","interactions":[],"lastModifiedDate":"2017-01-18T11:27:29","indexId":"ofr20141206","displayToPublicDate":"2014-11-04T09:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-1206","title":"Low-head hydropower assessment of the Brazilian State of São Paulo","docAbstract":"<p>This study produced a comprehensive estimate of the magnitude of hydropower potential available in the streams that drain watersheds entirely within the State of S&atilde;o Paulo, Brazil. Because a large part of the contributing area is outside of S&atilde;o Paulo, the main stem of the Paran&aacute; River was excluded from the assessment. Potential head drops were calculated from the Digital Terrain Elevation Data,which has a 1-arc-second resolution (approximately 30-meter resolution at the equator). For the conditioning and validation of synthetic stream channels derived from the Digital Elevation Model datasets, hydrography data (in digital format) supplied by the S&atilde;o Paulo State Department of Energy and the Ag&ecirc;ncia Nacional de &Aacute;guas were used. Within the study area there were 1,424&nbsp;rain gages and 123 streamgages with long-term data records. To estimate average yearly streamflow, a hydrologic regionalization system that divides the State into 21 homogeneous basins was used. Stream segments, upstream areas, and mean annual rainfall were estimated using geographic information systems techniques. The accuracy of the flows estimated with the regionalization models was validated. Overall, simulated streamflows were significantly correlated with the observed flows but with a consistent underestimation bias. When the annual mean flows from the regionalization models were adjusted upward by 10 percent, average streamflow estimation bias was reduced from -13 percent to -4 percent. The sum of all the validated stream reach mean annual hydropower potentials in the 21 basins is 7,000 megawatts (MW). Hydropower potential is mainly concentrated near the Serra do Mar mountain range and along the Tiet&ecirc; River. The power potential along the Tiet&ecirc; River is mainly at sites with medium and high potentials, sites where hydropower has already been harnessed. In addition to the annual mean hydropower estimates, potential hydropower estimates with flow rates with exceedance probabilities of 40 percent, 60 percent, and 90&nbsp;percent were made.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20141206","usgsCitation":"Artan, G.A., Cushing, W.M., Mathis, M.L., and Tieszen, L.L., 2014, Low-head hydropower assessment of the Brazilian State of São Paulo: U.S. Geological Survey Open-File Report 2014-1206, v, 15 p., https://doi.org/10.3133/ofr20141206.","productDescription":"v, 15 p.","numberOfPages":"26","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-051675","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":295835,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20141206.jpg"},{"id":295834,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2014/1206/pdf/ofr2014-1206.pdf","text":"Report","size":"11.1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":295766,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2014/1206/"}],"country":"Brazil","city":"São Paulo","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5459eaa2e4b009f8aec96ffe","contributors":{"authors":[{"text":"Artan, Guleid A. 0000-0001-8409-6182 gartan@usgs.gov","orcid":"https://orcid.org/0000-0001-8409-6182","contributorId":2938,"corporation":false,"usgs":true,"family":"Artan","given":"Guleid","email":"gartan@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":521219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, W. Matthew 0000-0001-5209-6006 mcushing@usgs.gov","orcid":"https://orcid.org/0000-0001-5209-6006","contributorId":2980,"corporation":false,"usgs":true,"family":"Cushing","given":"W.","email":"mcushing@usgs.gov","middleInitial":"Matthew","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":521220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mathis, Melissa L. 0000-0003-4967-4770 mlmathis@usgs.gov","orcid":"https://orcid.org/0000-0003-4967-4770","contributorId":5461,"corporation":false,"usgs":true,"family":"Mathis","given":"Melissa","email":"mlmathis@usgs.gov","middleInitial":"L.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":521221,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tieszen, Larry L. tieszen@usgs.gov","contributorId":2831,"corporation":false,"usgs":true,"family":"Tieszen","given":"Larry","email":"tieszen@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":521222,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70131486,"text":"ofr20141229 - 2014 - Bull trout in the Boundary System: managing connectivity and the feasibility of a reintroduction in the lower Pend Oreille River, northeastern Washington","interactions":[],"lastModifiedDate":"2017-11-22T16:03:58","indexId":"ofr20141229","displayToPublicDate":"2014-11-04T09:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-1229","title":"Bull trout in the Boundary System: managing connectivity and the feasibility of a reintroduction in the lower Pend Oreille River, northeastern Washington","docAbstract":"<p>Many of the World&rsquo;s rivers are influenced by large dams (&gt;15 m high) most of which have fragmented formerly continuous habitats, and significantly altered fish passage, natural flow, temperature, and sediment fluxes (Nilsson and others, 2005; Arthington, 2012; Liermann and others, 2012). In the Pacific Northwest, dams on major rivers have been a major focus for fishery managers, primarily in regard to passage of anadromous salmonids (principally Pacific salmon and steelhead trout [<em>Oncorhynchus mykiss</em>], for example, Ferguson and others, 2011), but more recently other species, such as Pacific lamprey (<em>Entosphenus tridentatus</em>) and resident (non-anadromous) salmonids, are receiving more attention (Neraas and Spruell, 2001; Moser and others, 2002; Muhlfeld and others, 2012). In the case of resident salmonids, fish can adopt a wide range of migratory behaviors that often bring them into mainstem rivers where they can come into direct contact with large dams. When this occurs, some of the most important direct effects of dams on salmonids include barriers to upstream and downstream movement and mortality associated with entrainment within the dam or spill over dams. Biologically, these direct impacts can lead to (1) disruption of natural historical (pre-dam) genetic and demographic connectivity among local populations, (2) loss of access to historically used migratory destinations, (3) loss of individuals to the population through mortality associated with entrainment.</p>\n<p>&nbsp;</p>\n<p>In this report, we address these issues for the case of Boundary Dam, located immediately south of the Canadian border on the lower Pend Oreille River in northeastern Washington (fig. 1). Specifically, we addressed the following objectives:</p>\n<p>&nbsp;</p>\n<ul>\n<li>Evaluate the justification for bull trout (<em>Salvelinus confluentus</em>) passing over Boundary Dam in the context of likely historical patterns of gene flow that occurred prior to dam construction, current patterns of movement, and status of existing populations.</li>\n<li>Assess the role of passage over Boundary Dam, in the context of other factors in the system that may influence the feasibility of establishing a self-sustaining bull trout population in the Boundary system.</li>\n</ul>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20141229","usgsCitation":"Dunham, J., Taylor, E.B., and Allendorf, F.W., 2014, Bull trout in the Boundary System: managing connectivity and the feasibility of a reintroduction in the lower Pend Oreille River, northeastern Washington: U.S. Geological Survey Open-File Report 2014-1229, iv, 28 p., https://doi.org/10.3133/ofr20141229.","productDescription":"iv, 28 p.","numberOfPages":"36","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-057086","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":295837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20141229.JPG"},{"id":295767,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2014/1229/"},{"id":295836,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2014/1229/pdf/ofr2014-1229.pdf"}],"country":"United States","state":"Washington","otherGeospatial":"Lower Pend Oreille River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5459ea9ee4b009f8aec96fa8","contributors":{"authors":[{"text":"Dunham, Jason B. 0000-0002-6268-0633 jdunham@usgs.gov","orcid":"https://orcid.org/0000-0002-6268-0633","contributorId":1808,"corporation":false,"usgs":true,"family":"Dunham","given":"Jason B.","email":"jdunham@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":false,"id":521253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Eric B. 0000-0002-3974-6315","orcid":"https://orcid.org/0000-0002-3974-6315","contributorId":124524,"corporation":false,"usgs":false,"family":"Taylor","given":"Eric","email":"","middleInitial":"B.","affiliations":[{"id":5083,"text":"University of British Columbia, Department of Zoology, Biodiversity Research Centre and Beaty Biodiversity  Museum","active":true,"usgs":false}],"preferred":false,"id":521254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allendorf, Fred W.","contributorId":124525,"corporation":false,"usgs":false,"family":"Allendorf","given":"Fred","email":"","middleInitial":"W.","affiliations":[{"id":5084,"text":"Division of Biological Sciences, University of Montana, Missoula, MT","active":true,"usgs":false}],"preferred":false,"id":521255,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70121352,"text":"sir20145164 - 2014 - Estimates of growth and mortality of under-yearling smallmouth bass in Spednic Lake, from 1970 through 2008","interactions":[],"lastModifiedDate":"2014-11-04T08:55:49","indexId":"sir20145164","displayToPublicDate":"2014-11-04T09:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-5164","title":"Estimates of growth and mortality of under-yearling smallmouth bass in Spednic Lake, from 1970 through 2008","docAbstract":"<p>This report is the product of a 2013 cooperative agreement between the U.S. Geological Survey, the International Joint Commission, and the Maine Bureau of Sea Run Fisheries and Habitat to quantify the effects of meteorological conditions (from 1970 through 2008) on the survival of smallmouth bass (<em>Micropterus dolomieu</em>) in the first year of life in Spednic Lake. This report documents the data and methods used to estimate historical daily mean lake surface-water temperatures from early spring through late autumn, which were used to estimate the dates of smallmouth bass spawning, young-of-the-year growth, and probable strength of each year class. Mortality of eggs and fry in nests was modeled and estimated to exceed 10 percent in 17 of 39 years; during those years, cold temperatures in the early part of the spawning period resulted in mortality to fish that were estimated to have had the longest growing season and attain the greatest length. Modeled length-dependent overwinter survival combined with early mortality identified 1986, 1994, 1996, and 2004 as the years in which temperature was likely to have presented the greatest challenge to year-class strength in the Spednic Lake fishery. Age distribution of bass in fisheries on lakes in the St. Croix and surrounding watersheds confirmed that conditions in 1986 and 1996 resulted in weak smallmouth bass year classes (age-four or age-five bass representing less than 15 percent of a 100-fish sample).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20145164","collaboration":"Prepared in cooperation with the International Joint Commission St. Croix River Watershed Board and the Maine Bureau of Sea Run Fisheries and Habitat","usgsCitation":"Dudley, R.W., and Trial, J.G., 2014, Estimates of growth and mortality of under-yearling smallmouth bass in Spednic Lake, from 1970 through 2008: U.S. Geological Survey Scientific Investigations Report 2014-5164, v, 15 p., https://doi.org/10.3133/sir20145164.","productDescription":"v, 15 p.","numberOfPages":"26","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"1970-01-01","temporalEnd":"2008-12-31","ipdsId":"IP-057932","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":295830,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20145164.jpg"},{"id":295761,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2014/5164/"},{"id":295762,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2014/5164/pdf/sir2014-5164.pdf","size":"1.42 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Universal Transverse Mercator projection","country":"Canada, United States","state":"Maine","otherGeospatial":"Spednic Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5459eaa1e4b009f8aec96fda","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":519251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trial, Joan G.","contributorId":91156,"corporation":false,"usgs":true,"family":"Trial","given":"Joan","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":519252,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70129335,"text":"ofr20141222 - 2014 - Long Valley Caldera 2003 through 2014: Overview of low level unrest in the past decade","interactions":[],"lastModifiedDate":"2019-03-15T10:13:55","indexId":"ofr20141222","displayToPublicDate":"2014-11-03T11:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2014-1222","title":"Long Valley Caldera 2003 through 2014: Overview of low level unrest in the past decade","docAbstract":"<p>Long Valley Caldera is located in California along the eastern escarpment of the Sierra Nevada Range. The caldera formed about 760,000 years ago as the eruption of 600 km<sup>3</sup> of rhyolite magma (Bishop Tuff) resulted in collapse of the partially evacuated magma chamber. Resurgent doming in the central part of the caldera occurred shortly afterwards, and the most recent eruptions inside the caldera occurred about 50,000 years ago. The caldera remains thermally active, with many hot springs and fumaroles, and has had significant deformation and seismicity since at least 1978. Periods of intense unrest in the 1980s to early 2000s are well documented in the literature (Hill and others, 2002; Ewert and others, 2010). In this poster, we extend the timeline forward, documenting seismicity and deformation over the past decade.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20141222","usgsCitation":"Wilkinson, S.K., Hill, D.P., Langbein, J.O., Lisowski, M., and Mangan, M.T., 2014, Long Valley Caldera 2003 through 2014: Overview of low level unrest in the past decade: U.S. Geological Survey Open-File Report 2014-1222, Sheet: 68.0 x 36.0 inches, https://doi.org/10.3133/ofr20141222.","productDescription":"Sheet: 68.0 x 36.0 inches","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2003-01-01","temporalEnd":"2014-06-30","ipdsId":"IP-051632","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":295823,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2014/1222/pdf/ofr2014-1222_report.pdf"},{"id":295826,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2014/1222/"},{"id":295824,"rank":3,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2014/1222/images/coverthbnew.gif"}],"country":"United States","state":"California","otherGeospatial":"Long Valley Caldera","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              37\n            ],\n            [\n              -118,\n              37\n            ],\n            [\n              -118,\n              38.75\n            ],\n            [\n              -120,\n              38.75\n            ],\n            [\n              -120,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54589917e4b009f8aec946ef","contributors":{"authors":[{"text":"Wilkinson, Stuart K. swilk@usgs.gov","contributorId":3401,"corporation":false,"usgs":true,"family":"Wilkinson","given":"Stuart","email":"swilk@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":522851,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, David P. hill@usgs.gov","contributorId":2600,"corporation":false,"usgs":true,"family":"Hill","given":"David","email":"hill@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":false,"id":522852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langbein, John O. 0000-0002-7821-8101 langbein@usgs.gov","orcid":"https://orcid.org/0000-0002-7821-8101","contributorId":3293,"corporation":false,"usgs":true,"family":"Langbein","given":"John","email":"langbein@usgs.gov","middleInitial":"O.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":522853,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lisowski, Michael 0000-0003-4818-2504 mlisowski@usgs.gov","orcid":"https://orcid.org/0000-0003-4818-2504","contributorId":637,"corporation":false,"usgs":true,"family":"Lisowski","given":"Michael","email":"mlisowski@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":522854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mangan, Margaret T. 0000-0002-5273-8053 mmangan@usgs.gov","orcid":"https://orcid.org/0000-0002-5273-8053","contributorId":3343,"corporation":false,"usgs":true,"family":"Mangan","given":"Margaret","email":"mmangan@usgs.gov","middleInitial":"T.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":522855,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70129373,"text":"70129373 - 2014 - Invasive crayfish as vectors of mercury in freshwater food webs of the Pacific Northwest","interactions":[],"lastModifiedDate":"2018-09-04T16:51:09","indexId":"70129373","displayToPublicDate":"2014-11-01T14:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Invasive crayfish as vectors of mercury in freshwater food webs of the Pacific Northwest","docAbstract":"Invasive species are important drivers of environmental change in aquatic ecosystems and can alter habitat characteristics, community composition, and ecosystem energetics. Such changes have important implications for many ecosystem processes, including the bioaccumulation and biomagnification of contaminants through food webs. Mercury concentrations were measured in 2 nonnative and 1 native crayfish species from western Oregon (USA). Nonnative red swamp crayfish had mercury concentrations similar to those in native signal crayfish (0.29 ± 0.05 µg/g dry wt and 0.36 ± 0.06 µg/g dry wt, respectively), whereas the nonnative ringed crayfish had lower mercury concentrations (0.10 ± 0.02 µg/g dry wt) than either of the other species. The mean energy content of muscle was similar between the native signal crayfish and nonnative ringed crayfish but was significantly higher in the nonnative red swamp crayfish. Across species, mercury concentrations were negatively correlated with energy density. Such energetic differences could exacerbate changes in mercury transfer through trophic pathways of food webs, especially via alterations to the growth dynamics of consumers. Thus, it is important to consider the role of energy content in determining effective mercury exposure even when mercury concentrations on a per-unit mass basis do not differ between species.","language":"English","publisher":"Elsevier","doi":"10.1002/etc.2727","usgsCitation":"Johnson, B., Willacker, J.J., Eagles-Smith, C.A., Pearl, C.A., and Adams, M.J., 2014, Invasive crayfish as vectors of mercury in freshwater food webs of the Pacific Northwest: Environmental Toxicology and Chemistry, v. 33, no. 11, p. 2639-2645, https://doi.org/10.1002/etc.2727.","productDescription":"7 p.","startPage":"2639","endPage":"2645","numberOfPages":"7","ipdsId":"IP-056979","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":295589,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295552,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/etc.2727"}],"country":"United States","state":"Oregon","volume":"33","issue":"11","noUsgsAuthors":false,"publicationDate":"2014-08-20","publicationStatus":"PW","scienceBaseUri":"547ae028e4b0da0a54dbb5ff","chorus":{"doi":"10.1002/etc.2727","url":"http://dx.doi.org/10.1002/etc.2727","publisher":"Wiley-Blackwell","authors":"Johnson Branden L., Willacker James J., Eagles-Smith Collin A., Pearl Christopher A., Adams Michael J.","journalName":"Environmental Toxicology and Chemistry","publicationDate":"9/16/2014","auditedOn":"11/1/2014"},"contributors":{"authors":[{"text":"Johnson, Branden L. branden_johnson@usgs.gov","contributorId":4168,"corporation":false,"usgs":true,"family":"Johnson","given":"Branden L.","email":"branden_johnson@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":523225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willacker, James J. jwillacker@usgs.gov","contributorId":5614,"corporation":false,"usgs":true,"family":"Willacker","given":"James","email":"jwillacker@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":523226,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eagles-Smith, Collin A. 0000-0003-1329-5285 ceagles-smith@usgs.gov","orcid":"https://orcid.org/0000-0003-1329-5285","contributorId":505,"corporation":false,"usgs":true,"family":"Eagles-Smith","given":"Collin","email":"ceagles-smith@usgs.gov","middleInitial":"A.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":523222,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearl, Christopher A. 0000-0003-2943-7321 christopher_pearl@usgs.gov","orcid":"https://orcid.org/0000-0003-2943-7321","contributorId":3131,"corporation":false,"usgs":true,"family":"Pearl","given":"Christopher","email":"christopher_pearl@usgs.gov","middleInitial":"A.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":false,"id":523223,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Adams, M. J. 0000-0001-8844-042X mjadams@usgs.gov","orcid":"https://orcid.org/0000-0001-8844-042X","contributorId":3133,"corporation":false,"usgs":false,"family":"Adams","given":"M.","email":"mjadams@usgs.gov","middleInitial":"J.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":523224,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70134235,"text":"70134235 - 2014 - U.S. response to a report of infectious salmon anemia virus in Western North America","interactions":[],"lastModifiedDate":"2016-04-26T09:38:35","indexId":"70134235","displayToPublicDate":"2014-11-01T13:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"U.S. response to a report of infectious salmon anemia virus in Western North America","docAbstract":"<p><span>Federal, state, and tribal fishery managers, as well as the general public and their elected representatives in the United States, were concerned when infectious salmon anemia virus (ISAV) was suspected for the first time in free-ranging Pacific Salmon collected from the coastal areas of British Columbia, Canada. This article documents how national and regional fishery managers and fish health specialists of the U.S. worked together and planned and implemented actions in response to the reported finding of ISAV in British Columbia. To date, the reports by Simon Fraser University remain unconfirmed and preliminary results from collaborative U.S. surveillance indicate that there is no evidence of ISAV in U.S. populations of free-ranging or marine-farmed salmonids on the west coast of North America.</span></p>","language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1080/03632415.2014.967348","usgsCitation":"Amos, K.H., Gustafson, L., Warg, J., Whaley, J., Purcell, M., Rolland, J.B., Winton, J., Snekvik, K., Meyers, T., Stewart, B., Kerwin, J., Blair, M., Bader, J., and Evered, J., 2014, U.S. response to a report of infectious salmon anemia virus in Western North America: Fisheries, v. 39, no. 11, p. 501-506, https://doi.org/10.1080/03632415.2014.967348.","productDescription":"6 p.","startPage":"501","endPage":"506","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056893","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":296383,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"11","noUsgsAuthors":false,"publicationDate":"2014-11-20","publicationStatus":"PW","scienceBaseUri":"547ee2d4e4b09357f05f8a76","contributors":{"authors":[{"text":"Amos, Kevin H","contributorId":127570,"corporation":false,"usgs":false,"family":"Amos","given":"Kevin","email":"","middleInitial":"H","affiliations":[{"id":7054,"text":"NOAA/NMFS, Silver Spring, MD","active":true,"usgs":false}],"preferred":false,"id":525719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gustafson, Lori","contributorId":127571,"corporation":false,"usgs":false,"family":"Gustafson","given":"Lori","affiliations":[{"id":7055,"text":"Animal and Plant Health Inspection Service, U.S. Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":525720,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warg, Janet","contributorId":127572,"corporation":false,"usgs":false,"family":"Warg","given":"Janet","email":"","affiliations":[{"id":7056,"text":"Animal and Plant Health Insepction Service, U.S. Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":525721,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whaley, Janet","contributorId":127573,"corporation":false,"usgs":false,"family":"Whaley","given":"Janet","affiliations":[{"id":7055,"text":"Animal and Plant Health Inspection Service, U.S. Department of Agriculture","active":true,"usgs":false}],"preferred":false,"id":525722,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Purcell, Maureen K. mpurcell@usgs.gov","contributorId":3061,"corporation":false,"usgs":true,"family":"Purcell","given":"Maureen K.","email":"mpurcell@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":525723,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rolland, Jill B. jrolland@usgs.gov","contributorId":5389,"corporation":false,"usgs":true,"family":"Rolland","given":"Jill","email":"jrolland@usgs.gov","middleInitial":"B.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":525724,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Winton, James R. jwinton@usgs.gov","contributorId":127569,"corporation":false,"usgs":true,"family":"Winton","given":"James R.","email":"jwinton@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":525718,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Snekvik, Kevin","contributorId":127574,"corporation":false,"usgs":false,"family":"Snekvik","given":"Kevin","email":"","affiliations":[{"id":7057,"text":"Washington Animal Disease Diagnostic Laboratory, Washington State Univeristy","active":true,"usgs":false}],"preferred":false,"id":525725,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Meyers, Theodore","contributorId":127575,"corporation":false,"usgs":false,"family":"Meyers","given":"Theodore","affiliations":[{"id":7058,"text":"Alaska Department of Fish and Game","active":true,"usgs":false}],"preferred":false,"id":525726,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Stewart, Bruce","contributorId":127576,"corporation":false,"usgs":false,"family":"Stewart","given":"Bruce","email":"","affiliations":[{"id":7059,"text":"Northwest Indian Fisheries Commission","active":true,"usgs":false}],"preferred":false,"id":525727,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Kerwin, John","contributorId":127577,"corporation":false,"usgs":false,"family":"Kerwin","given":"John","email":"","affiliations":[{"id":7060,"text":"Washington State Department of Fish and Wildlife","active":true,"usgs":false}],"preferred":false,"id":525728,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Blair, Marilyn","contributorId":44388,"corporation":false,"usgs":true,"family":"Blair","given":"Marilyn","affiliations":[],"preferred":false,"id":525730,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Bader, Joel","contributorId":127578,"corporation":false,"usgs":false,"family":"Bader","given":"Joel","email":"","affiliations":[{"id":7061,"text":"U.S. FWS, DOI","active":true,"usgs":false}],"preferred":false,"id":525729,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Evered, Joy","contributorId":127579,"corporation":false,"usgs":false,"family":"Evered","given":"Joy","affiliations":[{"id":7061,"text":"U.S. FWS, DOI","active":true,"usgs":false}],"preferred":false,"id":525731,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70133182,"text":"70133182 - 2014 - Quantifying fall migration of Ross's gulls (Rhodostethia rosea) past Point Barrow, Alaska","interactions":[],"lastModifiedDate":"2020-12-31T20:25:13.964435","indexId":"70133182","displayToPublicDate":"2014-11-01T13:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3093,"text":"Polar Biology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Quantifying fall migration of Ross's gulls (<i>Rhodostethia rosea</i>) past Point Barrow, Alaska","title":"Quantifying fall migration of Ross's gulls (Rhodostethia rosea) past Point Barrow, Alaska","docAbstract":"<p><span>The Ross’s gull (</span><i>Rhodostethia rosea</i><span>) is a poorly known seabird of the circumpolar Arctic. The only place in the world where Ross’s gulls are known to congregate is in the near-shore waters around Point Barrow, Alaska, where they undertake an annual passage in late fall. Ross’s gulls seen at Point Barrow are presumed to originate from nesting colonies in Siberia, but neither their origin nor their destination has been confirmed. Current estimates of the global population of Ross’s gulls are based largely on expert opinion, and the only reliable population estimate is derived from extrapolations from previous counts conducted at Point Barrow, but these data are now over 25&nbsp;years old. In order to update and clarify the status of this species in Alaska, our study quantified the timing, number, and flight direction of Ross’s gulls passing Point Barrow in 2011. We recorded up to two-thirds of the estimated global population of Ross’s gulls (≥27,000 individuals) over 39&nbsp;days with numbers peaking on 16 October when we observed over 7,000 birds during a 3-h period.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s00300-014-1552-4","usgsCitation":"Maftei, M., Davis, S.E., Uher-Koch, B.D., Gesmundo, C., Suydam, R., and Mallory, M.L., 2014, Quantifying fall migration of Ross's gulls (Rhodostethia rosea) past Point Barrow, Alaska: Polar Biology, v. 37, no. 11, p. 1705-1710, https://doi.org/10.1007/s00300-014-1552-4.","productDescription":"6 p.","startPage":"1705","endPage":"1710","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056953","costCenters":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":296078,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Point Barrow","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.3626708984375,\n              71.21430638639127\n            ],\n            [\n              -155.665283203125,\n              71.21430638639127\n            ],\n            [\n              -155.665283203125,\n              71.60134862675986\n            ],\n            [\n              -157.3626708984375,\n              71.60134862675986\n            ],\n            [\n              -157.3626708984375,\n              71.21430638639127\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"11","noUsgsAuthors":false,"publicationDate":"2014-07-31","publicationStatus":"PW","scienceBaseUri":"5465d636e4b04d4b7dbd6641","contributors":{"authors":[{"text":"Maftei, Mark","contributorId":127435,"corporation":false,"usgs":false,"family":"Maftei","given":"Mark","email":"","affiliations":[],"preferred":false,"id":525152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Shanti E.","contributorId":127436,"corporation":false,"usgs":false,"family":"Davis","given":"Shanti","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":525151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Uher-Koch, Brian D. 0000-0002-1885-0260 buher-koch@usgs.gov","orcid":"https://orcid.org/0000-0002-1885-0260","contributorId":5117,"corporation":false,"usgs":true,"family":"Uher-Koch","given":"Brian","email":"buher-koch@usgs.gov","middleInitial":"D.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":524850,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gesmundo, Callie","contributorId":127437,"corporation":false,"usgs":false,"family":"Gesmundo","given":"Callie","email":"","affiliations":[],"preferred":false,"id":525153,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Suydam, R.S.","contributorId":74213,"corporation":false,"usgs":true,"family":"Suydam","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":525154,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mallory, Mark L.","contributorId":127438,"corporation":false,"usgs":false,"family":"Mallory","given":"Mark","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":525155,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70138189,"text":"70138189 - 2014 - An objective and parsimonious approach for classifying natural flow regimes at a continental scale","interactions":[],"lastModifiedDate":"2015-01-15T12:44:06","indexId":"70138189","displayToPublicDate":"2014-11-01T12:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3301,"text":"River Research and Applications","active":true,"publicationSubtype":{"id":10}},"title":"An objective and parsimonious approach for classifying natural flow regimes at a continental scale","docAbstract":"<p>Hydro-ecological stream classification-the process of grouping streams by similar hydrologic responses and, by extension, similar aquatic habitat-has been widely accepted and is considered by some to be one of the first steps towards developing ecological flow targets. A new classification of 1543 streamgauges in the contiguous USA is presented by use of a novel and parsimonious approach to understand similarity in ecological streamflow response. This novel classification approach uses seven fundamental daily streamflow statistics (FDSS) rather than winnowing down an uncorrelated subset from 200 or more ecologically relevant streamflow statistics (ERSS) commonly used in hydro-ecological classification studies. The results of this investigation demonstrate that the distributions of 33 tested ERSS are consistently different among the classification groups derived from the seven FDSS. It is further shown that classification based solely on the 33 ERSS generally does a poorer job in grouping similar streamgauges than the classification based on the seven FDSS. This new classification approach has the additional advantages of overcoming some of the subjectivity associated with the selection of the classification variables and provides a set of robust continental-scale classes of US streamgauges. Published 2013. This article is a U.S. Government work and is in the public domain in the USA.</p>","language":"English","publisher":"John Wiley & Sons","publisherLocation":"Chichester, West Sussex, UK","doi":"10.1002/rra.2710","collaboration":"USGS National Water Census","usgsCitation":"Archfield, S.A., Kennen, J., Carlisle, D.M., and Wolock, D.M., 2014, An objective and parsimonious approach for classifying natural flow regimes at a continental scale: River Research and Applications, v. 30, no. 9, p. 1166-1183, https://doi.org/10.1002/rra.2710.","productDescription":"18 p.","startPage":"1166","endPage":"1183","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-050605","costCenters":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"links":[{"id":297295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297285,"type":{"id":15,"text":"Index Page"},"url":"https://onlinelibrary.wiley.com/doi/10.1002/rra.2710/full"}],"volume":"30","issue":"9","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2013-09-30","publicationStatus":"PW","scienceBaseUri":"54dd2b30e4b08de9379b329e","contributors":{"authors":[{"text":"Archfield, Stacey A. 0000-0002-9011-3871 sarch@usgs.gov","orcid":"https://orcid.org/0000-0002-9011-3871","contributorId":1874,"corporation":false,"usgs":true,"family":"Archfield","given":"Stacey","email":"sarch@usgs.gov","middleInitial":"A.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":538563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennen, Jonathan G. 0000-0002-5426-4445 jgkennen@usgs.gov","orcid":"https://orcid.org/0000-0002-5426-4445","contributorId":574,"corporation":false,"usgs":true,"family":"Kennen","given":"Jonathan G.","email":"jgkennen@usgs.gov","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":538564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlisle, Daren M. 0000-0002-7367-348X dcarlisle@usgs.gov","orcid":"https://orcid.org/0000-0002-7367-348X","contributorId":513,"corporation":false,"usgs":true,"family":"Carlisle","given":"Daren","email":"dcarlisle@usgs.gov","middleInitial":"M.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":538565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wolock, David M. 0000-0002-6209-938X dwolock@usgs.gov","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":540,"corporation":false,"usgs":true,"family":"Wolock","given":"David","email":"dwolock@usgs.gov","middleInitial":"M.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":538566,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70157371,"text":"70157371 - 2014 - Using mark-recapture distance sampling methods on line transect surveys","interactions":[],"lastModifiedDate":"2017-11-24T17:47:57","indexId":"70157371","displayToPublicDate":"2014-11-01T12:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2717,"text":"Methods in Ecology and Evolution","active":true,"publicationSubtype":{"id":10}},"title":"Using mark-recapture distance sampling methods on line transect surveys","docAbstract":"<ol id=\"mee312294-list-0001\" class=\"numbered\">\n<li>Mark&ndash;recapture distance sampling (MRDS) methods are widely used for density and abundance estimation when the conventional DS assumption of certain detection at distance zero fails, as they allow detection at distance zero to be estimated and incorporated into the overall probability of detection to better estimate density and abundance. However, incorporating MR data in DS models raises survey and analysis issues not present in conventional DS. Conversely, incorporating DS assumptions in MR models raises issues not present in conventional MR. As a result, being familiar with either conventional DS methods or conventional MR methods does not on its own put practitioners in good a position to apply MRDS methods appropriately. This study explains the sometimes subtly different varieties of MRDS survey methods and the associated concepts underlying MRDS models. This is done as far as possible without giving mathematical details &ndash; in the hope that this will make the key concepts underlying the methods accessible to a wider audience than if we were to present the concepts via equations.</li>\n<li>We illustrate use of the two main types of MRDS model by using data collected on two different types of survey: a survey of ungulate faecal pellets where two observers searched independently of each other; and a cetacean survey that used a search protocol that could accommodate responsive movement, with only one observer searching independently and the other being aware of all detections.</li>\n<li><i>Synthesis and applications</i>. Mark&ndash;recapture DS is a widely used method for estimating animal density and abundance when detection of animals at distance zero is not certain. Two observer configurations and three statistical models are described, and it is important to choose the most appropriate model for the observer configuration and target species in question. By way of making the methods more accessible to practicing ecologists, we describe the key ideas underlying MRDS methods, the sometimes subtle differences between them, and we illustrate these by applying different kinds of MRDS method to surveys of two different target species using different survey configurations.</li>\n</ol>","language":"English","publisher":"British Ecological Society","doi":"10.1111/2041-210X.12294","usgsCitation":"Burt, L.M., Borchers, D., Jenkins, K.J., and Marques, T.A., 2014, Using mark-recapture distance sampling methods on line transect surveys: Methods in Ecology and Evolution, v. 5, no. 11, p. 1180-1191, https://doi.org/10.1111/2041-210X.12294.","productDescription":"12 p.","startPage":"1180","endPage":"1191","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059999","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":472656,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/2041-210x.12294","text":"Publisher Index Page"},{"id":308436,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"11","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2014-11-12","publicationStatus":"PW","scienceBaseUri":"5603cd5de4b03bc34f544b49","chorus":{"doi":"10.1111/2041-210x.12294","url":"http://dx.doi.org/10.1111/2041-210x.12294","publisher":"Wiley-Blackwell","authors":"Burt Mary Louise, Borchers David L., Jenkins Kurt J., Marques Tiago A.","journalName":"Methods in Ecology and Evolution","publicationDate":"11/2014"},"contributors":{"authors":[{"text":"Burt, Louise M.","contributorId":147848,"corporation":false,"usgs":false,"family":"Burt","given":"Louise","email":"","middleInitial":"M.","affiliations":[{"id":16945,"text":"St. Andrews University, UK","active":true,"usgs":false}],"preferred":false,"id":572899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Borchers, David L.","contributorId":31106,"corporation":false,"usgs":true,"family":"Borchers","given":"David L.","affiliations":[],"preferred":false,"id":572900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenkins, Kurt J. 0000-0003-1415-6607 kurt_jenkins@usgs.gov","orcid":"https://orcid.org/0000-0003-1415-6607","contributorId":3415,"corporation":false,"usgs":true,"family":"Jenkins","given":"Kurt","email":"kurt_jenkins@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":572898,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marques, Tigao A","contributorId":147849,"corporation":false,"usgs":false,"family":"Marques","given":"Tigao","email":"","middleInitial":"A","affiliations":[{"id":16945,"text":"St. Andrews University, UK","active":true,"usgs":false}],"preferred":false,"id":572901,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70157379,"text":"70157379 - 2014 - Attenuation and scattering tomography of the deep plumbing system of Mount St. Helens","interactions":[],"lastModifiedDate":"2019-03-05T09:51:38","indexId":"70157379","displayToPublicDate":"2014-11-01T12:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Attenuation and scattering tomography of the deep plumbing system of Mount St. Helens","docAbstract":"<p><span>We present a combined 3-D&nbsp;</span><i>P</i><span>&nbsp;wave attenuation, 2-D&nbsp;</span><i>S</i><span>&nbsp;coda attenuation, and 3-D&nbsp;</span><i>S</i><span>&nbsp;coda scattering tomography model of fluid pathways, feeding systems, and sediments below Mount St. Helens (MSH) volcano between depths of 0 and 18 km. High-scattering and high-attenuation shallow anomalies are indicative of magma and fluid-rich zones within and below the volcanic edifice down to 6 km depth, where a high-scattering body outlines the top of deeper aseismic velocity anomalies. Both the volcanic edifice and these structures induce a combination of strong scattering and attenuation on any seismic wavefield, particularly those recorded on the northern and eastern flanks of the volcanic cone. North of the cone between depths of 0 and 10 km, a low-velocity, high-scattering, and high-attenuation north-south trending trough is attributed to thick piles of Tertiary marine sediments within the St. Helens Seismic Zone. A laterally extended 3-D scattering contrast at depths of 10 to 14 km is related to the boundary between upper and lower crust and caused in our interpretation by the large-scale interaction of the Siletz terrane with the Cascade arc crust. This contrast presents a low-scattering, 4&ndash;6 km</span><span>2</span><span>&nbsp;&ldquo;hole&rdquo; under the northeastern flank of the volcano. We infer that this section represents the main path of magma ascent from depths greater than 6 km at MSH, with a small north-east shift in the lower plumbing system of the volcano. We conclude that combinations of different nonstandard tomographic methods, leading toward full-waveform tomography, represent the future of seismic volcano imaging.</span></p>","language":"English","publisher":"American Geophysical Union","publisherLocation":"Richmond, VA","doi":"10.1002/2014JB011372","usgsCitation":"De Siena, L., Thomas, C., Waite, G., Moran, S.C., and Klemme, S., 2014, Attenuation and scattering tomography of the deep plumbing system of Mount St. Helens: Journal of Geophysical Research B: Solid Earth, v. 119, no. 11, p. 8223-8238, https://doi.org/10.1002/2014JB011372.","productDescription":"16 p.","startPage":"8223","endPage":"8238","numberOfPages":"16","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054945","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":472658,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014jb011372","text":"Publisher Index Page"},{"id":308432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","county":"Skamania","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.35,\n              46.0833\n            ],\n            [\n              -122,\n              46.0833\n            ],\n            [\n              -122,\n              46.3\n            ],\n            [\n              -122.35,\n              46.3\n            ],\n            [\n              -122.35,\n              46.0833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"119","issue":"11","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-11-07","publicationStatus":"PW","scienceBaseUri":"5603cd32e4b03bc34f544aee","contributors":{"authors":[{"text":"De Siena, Luca","contributorId":147853,"corporation":false,"usgs":false,"family":"De Siena","given":"Luca","email":"","affiliations":[{"id":16948,"text":"Institut fur Geophysik, University of Munster, Germany","active":true,"usgs":false}],"preferred":false,"id":572924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Christine","contributorId":84988,"corporation":false,"usgs":true,"family":"Thomas","given":"Christine","affiliations":[],"preferred":false,"id":572925,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waite, Greg P.","contributorId":147854,"corporation":false,"usgs":false,"family":"Waite","given":"Greg P.","affiliations":[{"id":16203,"text":"Michigan Technological university","active":true,"usgs":false}],"preferred":false,"id":572926,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moran, Seth C. 0000-0001-7308-9649 smoran@usgs.gov","orcid":"https://orcid.org/0000-0001-7308-9649","contributorId":548,"corporation":false,"usgs":true,"family":"Moran","given":"Seth","email":"smoran@usgs.gov","middleInitial":"C.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":572923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klemme, Stefan","contributorId":147855,"corporation":false,"usgs":false,"family":"Klemme","given":"Stefan","email":"","affiliations":[{"id":16949,"text":"Institut fur Mineralogie, University of Munster, Germany","active":true,"usgs":false}],"preferred":false,"id":572927,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70134233,"text":"70134233 - 2014 - Differential susceptibility in steelhead trout populations to an emergent MD strain of infectious hematopoietic necrosis virus","interactions":[],"lastModifiedDate":"2020-12-23T15:22:14.785559","indexId":"70134233","displayToPublicDate":"2014-11-01T12:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1396,"text":"Diseases of Aquatic Organisms","active":true,"publicationSubtype":{"id":10}},"title":"Differential susceptibility in steelhead trout populations to an emergent MD strain of infectious hematopoietic necrosis virus","docAbstract":"<p>A significant emergence of trout-adapted MD subgroup infectious hematopoietic necrosis virus (IHNV) began in the coastal region of Washington State, USA, in 2007. This emergence event lasted until 2011 and caused both asymptomatic adult fish infection and symptomatic epidemic disease and mortality in juvenile fish. Incidence of virus during this emergence demonstrated a heterogeneous distribution among rivers of the coastal region, leaving fish populations of some rivers apparently untouched while others suffered significant and recurrent infection and mortality (Breyta et. al. 2013; Dis Aquat Org 104:179-195). In this study, we examined the possible contribution of variations in susceptibility of fish populations, age-related resistance, and virus virulence to the observed landscape heterogeneity. We found that the most significant variable was host susceptibility: by controlled experimental challenge studies steelhead trout populations with no history of IHNV infection were 1 to 3 orders of magnitude more sensitive than a fish population with a long history of IHNV infection. In addition, 2 fish populations from the same river, which descended relatively recently from a common ancestral population, demonstrated 1 to 2 orders of magnitude difference in susceptibility. Fish age-related development of resistance was most evident in the more susceptible of 2 related fish populations. Finally, the strain of virus involved in the 2007 coastal Washington emergence had high virulence but was within the range of other known M group viruses tested. These results suggest that one major driver of landscape heterogeneity in the 2007 coastal Washington IHNV emergence was variation in fish population susceptibility and that this trait may have a heritable component.</p>","language":"English","publisher":"Inter-Research Science Center","publisherLocation":"Oldendorf/Luhe, Germany","doi":"10.3354/dao02781","usgsCitation":"Breyta, R., Jones, A., and Kurath, G., 2014, Differential susceptibility in steelhead trout populations to an emergent MD strain of infectious hematopoietic necrosis virus: Diseases of Aquatic Organisms, v. 112, no. 1, p. 17-28, https://doi.org/10.3354/dao02781.","productDescription":"12 p.","startPage":"17","endPage":"28","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-055167","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":472659,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/dao02781","text":"Publisher Index Page"},{"id":296378,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.87060546874999,\n              45.81348649679973\n            ],\n            [\n              -122.18994140624999,\n              45.81348649679973\n            ],\n            [\n              -122.18994140624999,\n              48.99463598353405\n            ],\n            [\n              -124.87060546874999,\n              48.99463598353405\n            ],\n            [\n              -124.87060546874999,\n              45.81348649679973\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"112","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"547ee2bde4b09357f05f8a44","contributors":{"authors":[{"text":"Breyta, R.","contributorId":92949,"corporation":false,"usgs":true,"family":"Breyta","given":"R.","email":"","affiliations":[],"preferred":false,"id":526092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Amelia","contributorId":127565,"corporation":false,"usgs":false,"family":"Jones","given":"Amelia","email":"","affiliations":[{"id":7053,"text":"Volunteer, USGS, WFRC, Seattle, WA","active":true,"usgs":false}],"preferred":false,"id":525706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":2629,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":525707,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70156785,"text":"70156785 - 2014 - Development of the Coastal Storm Modeling System (CoSMoS) for predicting the impact of storms on high-energy, active-margin coasts","interactions":[],"lastModifiedDate":"2015-08-31T10:51:57","indexId":"70156785","displayToPublicDate":"2014-11-01T12:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2822,"text":"Natural Hazards","active":true,"publicationSubtype":{"id":10}},"title":"Development of the Coastal Storm Modeling System (CoSMoS) for predicting the impact of storms on high-energy, active-margin coasts","docAbstract":"<p><span>The Coastal Storm Modeling System (CoSMoS) applies a predominantly deterministic framework to make detailed predictions (meter scale) of storm-induced coastal flooding, erosion, and cliff failures over large geographic scales (100s of kilometers). CoSMoS was developed for hindcast studies, operational applications (i.e., nowcasts and multiday forecasts), and future climate scenarios (i.e., sea-level rise&nbsp;+&nbsp;storms) to provide emergency responders and coastal planners with critical storm hazards information that may be used to increase public safety, mitigate physical damages, and more effectively manage and allocate resources within complex coastal settings. The prototype system, developed for the California coast, uses the global WAVEWATCH III wave model, the TOPEX/Poseidon satellite altimetry-based global tide model, and atmospheric-forcing data from either the US National Weather Service (operational mode) or Global Climate Models (future climate mode), to determine regional wave and water-level boundary conditions. These physical processes are dynamically downscaled using a series of nested Delft3D-WAVE (SWAN) and Delft3D-FLOW (FLOW) models and linked at the coast to tightly spaced XBeach (eXtreme Beach) cross-shore profile models and a Bayesian probabilistic cliff failure model. Hindcast testing demonstrates that, despite uncertainties in preexisting beach morphology over the ~500&nbsp;km alongshore extent of the pilot study area, CoSMoS effectively identifies discrete sections of the coast (100s of meters) that are vulnerable to coastal hazards under a range of current and future oceanographic forcing conditions, and is therefore an effective tool for operational and future climate scenario planning.</span></p>","language":"English","publisher":"International Society for the Prevention and Mitigation of Natural Hazards","publisherLocation":"Dordrecht","doi":"10.1007/s11069-014-1236-y","usgsCitation":"Barnard, P., van Ormondt, M., Erikson, L., Eshleman, J., Hapke, C.J., Peter Ruggiero, Adams, P., and Foxgrover, A.C., 2014, Development of the Coastal Storm Modeling System (CoSMoS) for predicting the impact of storms on high-energy, active-margin coasts: Natural Hazards, v. 74, no. 2, p. 1095-1125, https://doi.org/10.1007/s11069-014-1236-y.","productDescription":"31 p.","startPage":"1095","endPage":"1125","numberOfPages":"31","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054533","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":307716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"2","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-05-21","publicationStatus":"PW","scienceBaseUri":"55e57aace4b05561fa20868b","contributors":{"authors":[{"text":"Barnard, Patrick L. 0000-0003-1414-6476 pbarnard@usgs.gov","orcid":"https://orcid.org/0000-0003-1414-6476","contributorId":147147,"corporation":false,"usgs":true,"family":"Barnard","given":"Patrick L.","email":"pbarnard@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":570535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"van Ormondt, Maarten","contributorId":147148,"corporation":false,"usgs":false,"family":"van Ormondt","given":"Maarten","affiliations":[{"id":12474,"text":"Deltares, Netherlands","active":true,"usgs":false}],"preferred":false,"id":570536,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erikson, Li H. 0000-0002-8607-7695 lerikson@usgs.gov","orcid":"https://orcid.org/0000-0002-8607-7695","contributorId":147149,"corporation":false,"usgs":true,"family":"Erikson","given":"Li H.","email":"lerikson@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":570537,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eshleman, Jodi","contributorId":147150,"corporation":false,"usgs":false,"family":"Eshleman","given":"Jodi","email":"","affiliations":[{"id":6924,"text":"National Park Service, Upper Columbia Basin Network","active":true,"usgs":false}],"preferred":false,"id":570538,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hapke, Cheryl J. 0000-0002-2753-4075 chapke@usgs.gov","orcid":"https://orcid.org/0000-0002-2753-4075","contributorId":2981,"corporation":false,"usgs":true,"family":"Hapke","given":"Cheryl","email":"chapke@usgs.gov","middleInitial":"J.","affiliations":[{"id":6676,"text":"USGS (retired)","active":true,"usgs":false}],"preferred":true,"id":570539,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Peter Ruggiero","contributorId":147151,"corporation":false,"usgs":false,"family":"Peter Ruggiero","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":570540,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Adams, Peter","contributorId":147152,"corporation":false,"usgs":false,"family":"Adams","given":"Peter","email":"","affiliations":[{"id":12557,"text":"University of Florida, FLREC","active":true,"usgs":false}],"preferred":false,"id":570541,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Foxgrover, Amy C. 0000-0003-0638-5776 afoxgrover@usgs.gov","orcid":"https://orcid.org/0000-0003-0638-5776","contributorId":3261,"corporation":false,"usgs":true,"family":"Foxgrover","given":"Amy","email":"afoxgrover@usgs.gov","middleInitial":"C.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":570542,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70155173,"text":"70155173 - 2014 - Lattice Boltzmann methods applied to large-scale three-dimensional virtual cores constructed from digital optical borehole images of the karst carbonate Biscayne aquifer in southeastern Florida","interactions":[],"lastModifiedDate":"2015-07-31T10:48:13","indexId":"70155173","displayToPublicDate":"2014-11-01T12:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"seriesNumber":"2015-1133","title":"Lattice Boltzmann methods applied to large-scale three-dimensional virtual cores constructed from digital optical borehole images of the karst carbonate Biscayne aquifer in southeastern Florida","docAbstract":"<p><span>Digital optical borehole images at approximately 2 mm vertical resolution and borehole caliper data were used to create three-dimensional renderings of the distribution of (1) matrix porosity and (2) vuggy megaporosity for the karst carbonate Biscayne aquifer in southeastern Florida. The renderings based on the borehole data were used as input into Lattice Boltzmann methods to obtain intrinsic permeability estimates for this extremely transmissive aquifer, where traditional aquifer test methods may fail due to very small drawdowns and non-Darcian flow that can reduce apparent hydraulic conductivity. Variogram analysis of the borehole data suggests a nearly isotropic rock structure at lag lengths up to the nominal borehole diameter. A strong correlation between the diameter of the borehole and the presence of vuggy megaporosity in the data set led to a bias in the variogram where the computed horizontal spatial autocorrelation is strong at lag distances greater than the nominal borehole size. Lattice Boltzmann simulation of flow across a 0.4 &times; 0.4 &times; 17 m (2.72 m</span><span>3</span><span>&nbsp;volume) parallel-walled column of rendered matrix and vuggy megaporosity indicates a high hydraulic conductivity of 53 m s</span><sup><span>&minus;1</span></sup><span>. This value is similar to previous Lattice Boltzmann calculations of hydraulic conductivity in smaller limestone samples of the Biscayne aquifer. The development of simulation methods that reproduce dual-porosity systems with higher resolution and fidelity and that consider flow through horizontally longer renderings could provide improved estimates of the hydraulic conductivity and help to address questions about the importance of scale.</span></p>","language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1002/2014WR015465","collaboration":"None","usgsCitation":"Michael Sukop, and Cunningham, K.J., 2014, Lattice Boltzmann methods applied to large-scale three-dimensional virtual cores constructed from digital optical borehole images of the karst carbonate Biscayne aquifer in southeastern Florida: Water Resources Research, v. 50, no. 11, p. 8807-8825, https://doi.org/10.1002/2014WR015465.","productDescription":"19 p.","startPage":"8807","endPage":"8825","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-049416","costCenters":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"links":[{"id":472657,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014wr015465","text":"Publisher Index Page"},{"id":306287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"11","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2014-11-17","publicationStatus":"PW","scienceBaseUri":"55bc9c2de4b033ef52100f2f","contributors":{"authors":[{"text":"Michael Sukop","contributorId":145653,"corporation":false,"usgs":false,"family":"Michael Sukop","affiliations":[{"id":7017,"text":"Florida International University","active":true,"usgs":false}],"preferred":false,"id":564970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, Kevin J. 0000-0002-2179-8686 kcunning@usgs.gov","orcid":"https://orcid.org/0000-0002-2179-8686","contributorId":1689,"corporation":false,"usgs":true,"family":"Cunningham","given":"Kevin","email":"kcunning@usgs.gov","middleInitial":"J.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":564969,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70133249,"text":"70133249 - 2014 - Competition between introduced and native spiders (Araneae: Linyphiidae)","interactions":[],"lastModifiedDate":"2020-12-21T17:54:17.955847","indexId":"70133249","displayToPublicDate":"2014-11-01T11:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1018,"text":"Biological Invasions","active":true,"publicationSubtype":{"id":10}},"title":"Competition between introduced and native spiders (Araneae: Linyphiidae)","docAbstract":"<p>The European sheet-web spider <em>Linyphia triangularis</em> (Araneae: Linyphiidae) has become established in Maine, where it often reaches very high densities. Two lines of evidence from previous work suggest that <em>L. triangularis</em> affects populations of the native linyphiid spider <em>Frontinella communis</em>. First, <em>F. communis</em> individuals are relatively scarce in both forest and coastal habitat where <em>L. triangularis</em> is common, but more common where <em>L. triangularis</em> is at low density. Second, in field experiments, <em>F. communis</em> species are less likely to settle in experimental plots when <em>L. triangularis</em> is present, and <em>F. communis</em> disappears from study plots when <em>L. triangularis</em> is introduced. Here we test two mechanisms that may underlie these patterns. First, we tested whether <em>L. triangularis</em> invades and usurps the webs of <em>F. communis</em>. When spiders were released onto webs of heterospecifics, <em>L. triangularis</em> was more likely to take over or share webs of <em>F. communis</em> than the reverse. We also observed natural takeovers of <em>F. communis</em> webs. Second, we explored the hypothesis that <em>L. triangularis</em> reduces prey availability for native species. We sampled flying prey in areas with <em>L. triangularis</em> and those where it had been removed, and found no effect of spider presence on measured prey density. We also found no effect of prey supplementation on web tenacity in <em>F. communis</em>, suggesting that <em>F. communis</em> movements are not highly dependent on prey availability. We conclude that web takeover is likely more important than prey reduction in driving negative effects of <em>L. triangularis</em> on <em>F. communis</em>.</p>","language":"English","publisher":"Springer","doi":"10.1007/s10530-014-0679-0","usgsCitation":"Houser, J., Ginsberg, H.S., and Jakob, E.M., 2014, Competition between introduced and native spiders (Araneae: Linyphiidae): Biological Invasions, v. 16, no. 11, p. 2479-2488, https://doi.org/10.1007/s10530-014-0679-0.","productDescription":"10 p.","startPage":"2479","endPage":"2488","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054677","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":488439,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.uri.edu/pls_facpubs/146","text":"External Repository"},{"id":296070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","county":"Hancock County","otherGeospatial":"Arcadia National Park, Schoodic Point","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -68.08502197265625,\n              44.328023358092224\n            ],\n            [\n              -68.03695678710938,\n              44.328023358092224\n            ],\n            [\n              -68.03695678710938,\n              44.39576876734357\n            ],\n            [\n              -68.08502197265625,\n              44.39576876734357\n            ],\n            [\n              -68.08502197265625,\n              44.328023358092224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","issue":"11","noUsgsAuthors":false,"publicationDate":"2014-04-03","publicationStatus":"PW","scienceBaseUri":"5465d630e4b04d4b7dbd65a5","contributors":{"authors":[{"text":"Houser, J.D.","contributorId":127387,"corporation":false,"usgs":false,"family":"Houser","given":"J.D.","email":"","affiliations":[{"id":6932,"text":"University of Massachusetts, Amherst","active":true,"usgs":false}],"preferred":false,"id":524977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ginsberg, Howard S. 0000-0002-4933-2466 hginsberg@usgs.gov","orcid":"https://orcid.org/0000-0002-4933-2466","contributorId":3204,"corporation":false,"usgs":true,"family":"Ginsberg","given":"Howard","email":"hginsberg@usgs.gov","middleInitial":"S.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":524976,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jakob, Elizabeth M.","contributorId":90602,"corporation":false,"usgs":true,"family":"Jakob","given":"Elizabeth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":524978,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70158919,"text":"70158919 - 2014 - Confocal microscopy as a useful approach to describe gill rakers of Asian species of carp and native filter-feeding fishes of the upper Mississippi River system","interactions":[],"lastModifiedDate":"2015-10-07T10:37:36","indexId":"70158919","displayToPublicDate":"2014-11-01T11:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Confocal microscopy as a useful approach to describe gill rakers of Asian species of carp and native filter-feeding fishes of the upper Mississippi River system","docAbstract":"<p><span>To better understand potential diet overlap among exotic Asian species of carp and native species of filter-feeding fishes of the upper Mississippi River system, microscopy was used to document morphological differences in the gill rakers. Analysing samples first with light microscopy and subsequently with confocal microscopy, the three-dimensional structure of gill rakers in&nbsp;</span><i>Hypophthalmichthys molitrix</i><span>,</span><i>Hypophthalmichthys nobilis</i><span>&nbsp;and&nbsp;</span><i>Dorosoma cepedianum</i><span>&nbsp;was more thoroughly described and illustrated than previous work with traditional microscopy techniques. The three-dimensional structure of gill rakers in&nbsp;</span><i>Ictiobus cyprinellus</i><span>&nbsp;was described and illustrated for the first time.</span></p>","language":"English","publisher":"The Fisheries Society of the British Isles","publisherLocation":"London","doi":"10.1111/jfb.12504","collaboration":"University of Wisconsin-La Crosse","usgsCitation":"Liza R. Walleser, Howard, D., Sandheinrich, M.B., Gaikowski, M.P., and Amberg, J.J., 2014, Confocal microscopy as a useful approach to describe gill rakers of Asian species of carp and native filter-feeding fishes of the upper Mississippi River system: Journal of Fish Biology, v. 85, no. 5, p. 1777-1784, https://doi.org/10.1111/jfb.12504.","productDescription":"8 p.","startPage":"1777","endPage":"1784","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059402","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":309717,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"5","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationDate":"2014-08-20","publicationStatus":"PW","scienceBaseUri":"56164233e4b0ba4884c6147f","chorus":{"doi":"10.1111/jfb.12504","url":"http://dx.doi.org/10.1111/jfb.12504","publisher":"Wiley-Blackwell","authors":"Walleser L. R., Howard D. R., Sandheinrich M. B., Gaikowski M. P., Amberg J. J.","journalName":"Journal of Fish Biology","publicationDate":"8/20/2014","auditedOn":"11/1/2014"},"contributors":{"authors":[{"text":"Liza R. Walleser","contributorId":149082,"corporation":false,"usgs":false,"family":"Liza R. Walleser","affiliations":[{"id":17632,"text":"University of Wisconsin-La Crosse and former UMESC employee","active":true,"usgs":false}],"preferred":false,"id":576840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, D.R.","contributorId":149083,"corporation":false,"usgs":false,"family":"Howard","given":"D.R.","email":"","affiliations":[{"id":17633,"text":"University of Wisconin-La Crosse","active":true,"usgs":false}],"preferred":false,"id":576841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandheinrich, Mark B.","contributorId":149084,"corporation":false,"usgs":false,"family":"Sandheinrich","given":"Mark","email":"","middleInitial":"B.","affiliations":[{"id":12793,"text":"University of Wisconsin-La Crosse","active":true,"usgs":false}],"preferred":false,"id":576842,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gaikowski, Mark P. 0000-0002-6507-9341 mgaikowski@usgs.gov","orcid":"https://orcid.org/0000-0002-6507-9341","contributorId":147779,"corporation":false,"usgs":true,"family":"Gaikowski","given":"Mark","email":"mgaikowski@usgs.gov","middleInitial":"P.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":576843,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Amberg, Jon J. jamberg@usgs.gov","contributorId":147776,"corporation":false,"usgs":true,"family":"Amberg","given":"Jon","email":"jamberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":false,"id":576839,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70170987,"text":"70170987 - 2014 - An 8700 year paleoclimate reconstruction from the southern Maya lowlands","interactions":[],"lastModifiedDate":"2016-05-17T10:42:33","indexId":"70170987","displayToPublicDate":"2014-11-01T11:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3219,"text":"Quaternary Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"An 8700 year paleoclimate reconstruction from the southern Maya lowlands","docAbstract":"<p><span>Analysis of a sediment core from Lago Puerto Arturo, a closed basin lake in northern Peten, Guatemala, has provided an &sim;8700&nbsp;cal&nbsp;year record of climate change and human activity in the southern Maya lowlands. Stable isotope, magnetic susceptibility, and pollen analyses were used to reconstruct environmental change in the region. Results indicate a relatively wet early to middle Holocene followed by a drier late Holocene, which we interpret as reflecting long-term changes in insolation (precession). Higher frequency variability is more likely attributable to changes in ocean/atmosphere circulation in both the North Atlantic and the Pacific Oceans. Pollen and isotope data show that most of the period of prehispanic agricultural settlement, i.e. &sim;5000&ndash;1000&nbsp;cal&nbsp;yr&nbsp;BP, was characterized by drier conditions than previous or subsequent periods. The presence of</span><i>Zea</i><span>&nbsp;(corn) pollen through peak aridity during the Terminal Classic period (&sim;1250&ndash;1130&nbsp;cal&nbsp;yr&nbsp;BP) suggests that drought may not have had as negative an impact as previously proposed. A dramatic negative shift in isotope values indicates an increase in precipitation after &sim;950&nbsp;cal&nbsp;yr&nbsp;BP (hereafter BP).</span></p>","language":"English","publisher":"Elsevier","publisherLocation":"New York, NY","doi":"10.1016/j.quascirev.2014.08.004","usgsCitation":"Wahl, D.B., Byrne, R., and Anderson, L., 2014, An 8700 year paleoclimate reconstruction from the southern Maya lowlands: Quaternary Science Reviews, v. 103, p. 19-25, https://doi.org/10.1016/j.quascirev.2014.08.004.","productDescription":"7 p.","startPage":"19","endPage":"25","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-053384","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":321292,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"103","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d643be4b07e28b66834a0","contributors":{"authors":[{"text":"Wahl, David B. 0000-0002-0451-3554 dwahl@usgs.gov","orcid":"https://orcid.org/0000-0002-0451-3554","contributorId":3433,"corporation":false,"usgs":true,"family":"Wahl","given":"David","email":"dwahl@usgs.gov","middleInitial":"B.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":24693,"text":"Climate Research and Development","active":true,"usgs":true}],"preferred":true,"id":629341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byrne, Roger","contributorId":13630,"corporation":false,"usgs":true,"family":"Byrne","given":"Roger","email":"","affiliations":[],"preferred":false,"id":629342,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Lysanna 0000-0001-5650-9744 landerson@usgs.gov","orcid":"https://orcid.org/0000-0001-5650-9744","contributorId":5339,"corporation":false,"usgs":true,"family":"Anderson","given":"Lysanna","email":"landerson@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":629343,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70155265,"text":"70155265 - 2014 - La Niña diversity and Northwest Indian Ocean Rim teleconnections","interactions":[],"lastModifiedDate":"2017-01-18T11:28:00","indexId":"70155265","displayToPublicDate":"2014-11-01T11:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1248,"text":"Climate Dynamics","active":true,"publicationSubtype":{"id":10}},"title":"La Niña diversity and Northwest Indian Ocean Rim teleconnections","docAbstract":"<p><span>The differences in tropical Pacific sea surface temperature (SST) expressions of El Ni&ntilde;o-Southern Oscillation (ENSO) events of the same phase have been linked with different global atmospheric circulation patterns. This study examines the dynamical forcing of precipitation during October&ndash;December (OND) and March&ndash;May (MAM) over East Africa and during December&ndash;March (DJFM) over Central-Southwest Asia for 1950&ndash;2010 associated with four tropical Pacific SST patterns characteristic of La Ni&ntilde;a events, the cold phase of ENSO. The self-organizing map method along with a statistical distinguishability test was used to isolate La Ni&ntilde;a events, and seasonal precipitation forcing was investigated in terms of the tropical overturning circulation and thermodynamic and moisture budgets. Recent La Ni&ntilde;a events with strong opposing SST anomalies between the central and western Pacific Ocean (phases 3 and 4), force the strongest global circulation modifications and drought over the Northwest Indian Ocean Rim. Over East Africa during MAM and OND, subsidence is forced by an enhanced tropical overturning circulation and precipitation reductions are exacerbated by increases in moisture flux divergence. Over Central-Southwest Asia during DJFM, the thermodynamic forcing of subsidence is primarily responsible for precipitation reductions, with moisture flux divergence acting as a secondary mechanism to reduce precipitation. Eastern Pacific La Ni&ntilde;a events in the absence of west Pacific SST anomalies (phases 1 and 2), are associated with weaker global teleconnections, particularly over the Indian Ocean Rim. The weak regional teleconnections result in statistically insignificant precipitation modifications over East Africa and Central-Southwest Asia.</span></p>","language":"English","publisher":"EBSCO Publishing","publisherLocation":"Heidelberg","doi":"10.1007/s00382-014-2083-y","usgsCitation":"Hoell, A., Funk, C.C., and Barlow, M., 2014, La Niña diversity and Northwest Indian Ocean Rim teleconnections: Climate Dynamics, v. 43, no. 9-10, p. 2707-2724, https://doi.org/10.1007/s00382-014-2083-y.","productDescription":"18 p.","startPage":"2707","endPage":"2724","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052606","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":306484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"9-10","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationDate":"2014-03-02","publicationStatus":"PW","scienceBaseUri":"57f7f032e4b0bc0bec09f602","contributors":{"authors":[{"text":"Hoell, Andrew","contributorId":145803,"corporation":false,"usgs":false,"family":"Hoell","given":"Andrew","affiliations":[{"id":16236,"text":"UCSB Climate Hazards Group","active":true,"usgs":false}],"preferred":false,"id":565427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Funk, Christopher C. 0000-0002-9254-6718 cfunk@usgs.gov","orcid":"https://orcid.org/0000-0002-9254-6718","contributorId":721,"corporation":false,"usgs":true,"family":"Funk","given":"Christopher","email":"cfunk@usgs.gov","middleInitial":"C.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":565426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barlow, Mathew","contributorId":145834,"corporation":false,"usgs":false,"family":"Barlow","given":"Mathew","affiliations":[{"id":16250,"text":"University of Massechusetts, Lowell","active":true,"usgs":false}],"preferred":false,"id":565428,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70134902,"text":"70134902 - 2014 - Geological controls on the occurrence of gas hydrate from core, downhole log, and seismic data in the Shenhu area, South China Sea","interactions":[],"lastModifiedDate":"2021-10-13T16:41:55.117592","indexId":"70134902","displayToPublicDate":"2014-11-01T11:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geological controls on the occurrence of gas hydrate from core, downhole log, and seismic data in the Shenhu area, South China Sea","docAbstract":"<p>Multi-channel seismic reflection data, well logs, and recovered sediment cores have been used in this study to characterize the geologic controls on the occurrence of gas hydrate in the Shenhu area of the South China Sea. The concept of the \"gas hydrate petroleum system\" has allowed for the systematic analysis of the impact of gas source, geologic controls on gas migration, and the role of the host sediment in the formation and stability of gas hydrates as encountered during the 2007 Guangzhou Marine Geological Survey Gas Hydrate Expedition (GMGS-1) in the Shenhu area. Analysis of seismic and bathymetric data identified seventeen sub-linear, near-parallel submarine canyons in this area. These canyons, formed in the Miocene, migrated in a northeasterly direction, and resulted in the burial and abandonment of canyons partially filled by coarse-grained sediments. Downhole wireline log (DWL) data were acquired from eight drill sites and sediment coring was conducted at five of these sites, which revealed the presence of suitable reservoirs for the occurrence of concentrated gas hydrate accumulations. Gas hydrate-bearing sediment layers were identified from well log and core data at three sites mainly within silt and silt clay sediments. Gas hydrate was also discovered in a sand reservoir at one site as inferred from the analysis of the DWL data. Seismic anomalies attributed to the presence of gas below the base of gas hydrate stability zone, provided direct evidence for the migration of gas into the overlying gas hydrate-bearing sedimentary sections. Geochemical analyses of gas samples collected from cores confirmed that the occurrence of gas hydrate in the Shenhu area is controlled by the presence thermogenic methane gas that has migrated into the gas hydrate stability zone from a more deeply buried source.</p>","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam","doi":"10.1016/j.margeo.2014.09.040","usgsCitation":"Wang, X., Lee, M.W., Collett, T.S., Yang, S., Guo, Y., and Wu, S., 2014, Geological controls on the occurrence of gas hydrate from core, downhole log, and seismic data in the Shenhu area, South China Sea: Marine Geology, v. 357, p. 272-292, https://doi.org/10.1016/j.margeo.2014.09.040.","productDescription":"21 p.","startPage":"272","endPage":"292","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-055596","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":296523,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","otherGeospatial":"Shenhu area, South China Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              115.1,\n              19.8333\n            ],\n            [\n              115.2833,\n              19.8333\n            ],\n            [\n              115.2833,\n              19.9333\n            ],\n            [\n              115.1,\n              19.9333\n            ],\n            [\n              115.1,\n              19.8333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"357","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54882b51e4b02acb4f0c8c35","contributors":{"authors":[{"text":"Lee, Myung W. mlee@usgs.gov","contributorId":779,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","email":"mlee@usgs.gov","middleInitial":"W.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":526662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wang, Xiujuan","contributorId":127764,"corporation":false,"usgs":false,"family":"Wang","given":"Xiujuan","email":"","affiliations":[{"id":7142,"text":"Institute of Oceanology, Chinese Academy of Sciences","active":true,"usgs":false}],"preferred":false,"id":526660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collett, Timothy S. 0000-0002-7598-4708 tcollett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":1698,"corporation":false,"usgs":true,"family":"Collett","given":"Timothy","email":"tcollett@usgs.gov","middleInitial":"S.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":526659,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yang, Shengxiong","contributorId":74306,"corporation":false,"usgs":true,"family":"Yang","given":"Shengxiong","affiliations":[],"preferred":false,"id":526663,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guo, Yiqun","contributorId":68659,"corporation":false,"usgs":false,"family":"Guo","given":"Yiqun","affiliations":[{"id":34423,"text":"Guangzhou Marine Geological Survey, Guangzhou, China","active":true,"usgs":false}],"preferred":false,"id":526664,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wu, Shiguo","contributorId":11126,"corporation":false,"usgs":true,"family":"Wu","given":"Shiguo","affiliations":[],"preferred":false,"id":526665,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70132337,"text":"70132337 - 2014 - Guiding out-migrating juvenile sea lamprey (Petromyzon marinus) with pulsed direct current","interactions":[],"lastModifiedDate":"2020-12-31T20:54:59.443922","indexId":"70132337","displayToPublicDate":"2014-11-01T11:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3301,"text":"River Research and Applications","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Guiding out-migrating juvenile sea lamprey (<i>Petromyzon marinus</i>) with pulsed direct current","title":"Guiding out-migrating juvenile sea lamprey (Petromyzon marinus) with pulsed direct current","docAbstract":"<p><span>Non‐physical stimuli can deter or guide fish without affecting water flow or navigation and therefore have been investigated to improve fish passage at anthropogenic barriers and to control movement of invasive fish. Upstream fish migration can be blocked or guided without physical structure by electrifying the water, but directional downstream fish guidance with electricity has received little attention. We tested two non‐uniform pulsed direct current electric systems, each having different electrode orientations (vertical versus horizontal), to determine their ability to guide out‐migrating juvenile sea lamprey (</span><i>Petromyzon marinus</i><span>) and rainbow trout (</span><i>Oncorhynchus mykiss</i><span>). Both systems guided significantly more juvenile sea lamprey to a specific location in our experimental raceway when activated than when deactivated, but guidance efficiency decreased at the highest water velocities tested. At the electric field setting that effectively guided sea lamprey, rainbow trout were guided by the vertical electrode system, but most were blocked by the horizontal electrode system. Additional research should characterize the response of other species to non‐uniform fields of pulsed DC and develop electrode configurations that guide fish over a range of water velocity. Published 2013. This article is a U.S. Government work and is in the public domain in the USA.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/rra.2703","usgsCitation":"Johnson, N.S., and Miehls, S.M., 2014, Guiding out-migrating juvenile sea lamprey (Petromyzon marinus) with pulsed direct current: River Research and Applications, v. 30, no. 9, p. 1146-1156, https://doi.org/10.1002/rra.2703.","productDescription":"11 p.","startPage":"1146","endPage":"1156","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-049198","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":296064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"9","noUsgsAuthors":false,"publicationDate":"2013-09-02","publicationStatus":"PW","scienceBaseUri":"5465d632e4b04d4b7dbd65e4","contributors":{"authors":[{"text":"Johnson, Nicholas S. 0000-0002-7419-6013 njohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7419-6013","contributorId":597,"corporation":false,"usgs":true,"family":"Johnson","given":"Nicholas","email":"njohnson@usgs.gov","middleInitial":"S.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":522809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miehls, Scott M. 0000-0002-5546-1854 smiehls@usgs.gov","orcid":"https://orcid.org/0000-0002-5546-1854","contributorId":5007,"corporation":false,"usgs":true,"family":"Miehls","given":"Scott","email":"smiehls@usgs.gov","middleInitial":"M.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":522810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70199595,"text":"70199595 - 2014 - Reply to: Turner, R.E., 2014. Discussion of: Olea, R.A. and Coleman, J.L., Jr., 2014. A synoptic examination of causes of land loss in southern Louisiana as related to the exploitation of subsurface geologic resources, Journal of Coastal Research, 30(5), 1025–1044; Journal of Coastal Research, 30(6), 1330–1334.","interactions":[],"lastModifiedDate":"2018-09-24T11:05:07","indexId":"70199595","displayToPublicDate":"2014-11-01T11:04:57","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Reply to: Turner, R.E., 2014. Discussion of: Olea, R.A. and Coleman, J.L., Jr., 2014. A synoptic examination of causes of land loss in southern Louisiana as related to the exploitation of subsurface geologic resources, Journal of Coastal Research, 30(5), 1025–1044; Journal of Coastal Research, 30(6), 1330–1334.","docAbstract":"<p>To a large extent, geology is a science of solving inverse problems based on some data and scientific principles. Solutions to these types of problems are not unique, especially when using different data, invoking different principles, or both. It is not surprising that the discussant and we have reached different conclusions on the same specific issue of land loss along the coast of Louisiana because we use different observations and view those observations in a different context. The objective of this reply is to orient the reader, who then can decide which approach is more likely to be the correct analysis.</p>","language":"English","publisher":"Coastal Education and Research Foundation","doi":"10.2112/JCOASTRES-D-14A-00004.1","usgsCitation":"Olea, R., and Coleman, J., 2014, Reply to: Turner, R.E., 2014. Discussion of: Olea, R.A. and Coleman, J.L., Jr., 2014. A synoptic examination of causes of land loss in southern Louisiana as related to the exploitation of subsurface geologic resources, Journal of Coastal Research, 30(5), 1025–1044; Journal of Coastal Research, 30(6), 1330–1334.: Journal of Coastal Research, v. 30, no. 6, p. 1335-1337, https://doi.org/10.2112/JCOASTRES-D-14A-00004.1.","productDescription":"3 p.","startPage":"1335","endPage":"1337","ipdsId":"IP-057121","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":472660,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2112/jcoastres-d-14a-00004.1","text":"Publisher Index Page"},{"id":357662,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":357606,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/pdf/43290021.pdf"}],"volume":"30","issue":"6","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bc03732e4b0fc368eb53ad1","contributors":{"authors":[{"text":"Olea, Ricardo A. 0000-0003-4308-0808","orcid":"https://orcid.org/0000-0003-4308-0808","contributorId":47873,"corporation":false,"usgs":true,"family":"Olea","given":"Ricardo A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":745929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, James L.","contributorId":208106,"corporation":false,"usgs":false,"family":"Coleman","given":"James L.","affiliations":[{"id":37715,"text":"Ex-USGS, now retired","active":true,"usgs":false}],"preferred":false,"id":745930,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70136059,"text":"70136059 - 2014 - Reducing risk from lahar hazards: Concepts, case studies, and roles for scientists","interactions":[],"lastModifiedDate":"2019-03-13T15:28:39","indexId":"70136059","displayToPublicDate":"2014-11-01T10:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3841,"text":"Journal of Applied Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Reducing risk from lahar hazards: Concepts, case studies, and roles for scientists","docAbstract":"<p>Lahars are rapid flows of mud-rock slurries that can occur without warning and catastrophically impact areas more than 100 km downstream of source volcanoes. Strategies to mitigate the potential for damage or loss from lahars fall into four basic categories: (1) avoidance of lahar hazards through land-use planning; (2) modification of lahar hazards through engineered protection structures; (3) lahar warning systems to enable evacuations; and (4) effective response to and recovery from lahars when they do occur. Successful application of any of these strategies requires an accurate understanding and assessment of the hazard, an understanding of the applicability and limitations of the strategy, and thorough planning. The human and institutional components leading to successful application can be even more important: engagement of all stakeholders in hazard education and risk-reduction planning; good communication of hazard and risk information among scientists, emergency managers, elected officials, and the at-risk public during crisis and non-crisis periods; sustained response training; and adequate funding for risk-reduction efforts. This paper reviews a number of methods for lahar-hazard risk reduction, examines the limitations and tradeoffs, and provides real-world examples of their application in the U.S. Pacific Northwest and in other volcanic regions of the world. An overriding theme is that lahar-hazard risk reduction cannot be effectively accomplished without the active, impartial involvement of volcano scientists, who are willing to assume educational, interpretive, and advisory roles to work in partnership with elected officials, emergency managers, and vulnerable communities.</p>","language":"English","publisher":"Springer-Verlag","doi":"10.1186/s13617-014-0016-4","usgsCitation":"Pierson, T.C., Wood, N.J., and Driedger, C.L., 2014, Reducing risk from lahar hazards: Concepts, case studies, and roles for scientists: Journal of Applied Volcanology, v. 3, no. 16, p. 1-25, https://doi.org/10.1186/s13617-014-0016-4.","productDescription":"25 p.","startPage":"1","endPage":"25","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-056294","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":472661,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/s13617-014-0016-4","text":"Publisher Index Page"},{"id":297074,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"16","noUsgsAuthors":false,"publicationDate":"2014-11-06","publicationStatus":"PW","scienceBaseUri":"54dd2c40e4b08de9379b36e2","contributors":{"authors":[{"text":"Pierson, Thomas C. 0000-0001-9002-4273 tpierson@usgs.gov","orcid":"https://orcid.org/0000-0001-9002-4273","contributorId":2498,"corporation":false,"usgs":true,"family":"Pierson","given":"Thomas","email":"tpierson@usgs.gov","middleInitial":"C.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":537067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Nathan J. 0000-0002-6060-9729 nwood@usgs.gov","orcid":"https://orcid.org/0000-0002-6060-9729","contributorId":3347,"corporation":false,"usgs":true,"family":"Wood","given":"Nathan","email":"nwood@usgs.gov","middleInitial":"J.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":537068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Driedger, Carolyn L. 0000-0002-4011-4112 driedger@usgs.gov","orcid":"https://orcid.org/0000-0002-4011-4112","contributorId":537,"corporation":false,"usgs":true,"family":"Driedger","given":"Carolyn","email":"driedger@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":537069,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70135072,"text":"70135072 - 2014 - Wave-driven sediment mobilization on a storm-controlled continental shelf (Northwest Iberia)","interactions":[],"lastModifiedDate":"2021-01-07T18:46:09.71468","indexId":"70135072","displayToPublicDate":"2014-11-01T10:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2381,"text":"Journal of Marine Systems","active":true,"publicationSubtype":{"id":10}},"title":"Wave-driven sediment mobilization on a storm-controlled continental shelf (Northwest Iberia)","docAbstract":"<p>Seafloor sediment mobilization on the inner Northwest Iberian continental shelf is caused largely by ocean surface waves. The temporal and spatial variability in the wave height, wave period, and wave direction has a profound effect on local sediment mobilization, leading to distinct sediment mobilization scenarios. Six grain-size specific sediment mobilization scenarios, representing seasonal average and storm conditions, were simulated with a physics-based numerical model. Model inputs included meteorological and oceanographic data in conjunction with seafloor grain-size and the shelf bathymetric data. The results show distinct seasonal variations, most importantly in wave height, leading to sediment mobilization, specifically on the inner shelf shallower than 30 m water depth where up to 49% of the shelf area is mobilized. Medium to severe storm events are modeled to mobilize up to 89% of the shelf area above 150 m water depth. The frequency of each of these seasonal and storm-related sediment mobilization scenarios is addressed using a decade of meteorological and oceanographic data. The temporal and spatial patterns of the modeled sediment mobilization scenarios are discussed in the context of existing geological and environmental processes and conditions to assist scientific, industrial and environmental efforts that are directly affected by sediment mobilization. Examples, where sediment mobilization plays a vital role, include seafloor nutrient advection, recurrent arrival of oil from oil-spill-laden seafloor sediment, and bottom trawling impacts.</p>","language":"English","publisher":"Elsevier","publisherLocation":"New York, NY","doi":"10.1016/j.jmarsys.2014.07.018","usgsCitation":"Oberle, F., Storlazzi, C., and Hanebuth, T., 2014, Wave-driven sediment mobilization on a storm-controlled continental shelf (Northwest Iberia): Journal of Marine Systems, v. 139, p. 362-372, https://doi.org/10.1016/j.jmarsys.2014.07.018.","productDescription":"11 p.","startPage":"362","endPage":"372","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-061568","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":296503,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Portugal, Spain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -10.78857421875,\n              40.58058466412761\n            ],\n            [\n              -7.75634765625,\n              40.58058466412761\n            ],\n            [\n              -7.75634765625,\n              43.35713822211053\n            ],\n            [\n              -10.78857421875,\n              43.35713822211053\n            ],\n            [\n              -10.78857421875,\n              40.58058466412761\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"139","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54882b66e4b02acb4f0c8c5a","contributors":{"authors":[{"text":"Oberle, Ferdinand 0000-0001-8871-3619","orcid":"https://orcid.org/0000-0001-8871-3619","contributorId":127792,"corporation":false,"usgs":false,"family":"Oberle","given":"Ferdinand","affiliations":[{"id":7156,"text":"MARUM – Center for Marine Environmental Sciences, University of Bremen","active":true,"usgs":false}],"preferred":false,"id":526779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490 cstorlazzi@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":2333,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt D.","email":"cstorlazzi@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":526778,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hanebuth, Till","contributorId":127793,"corporation":false,"usgs":false,"family":"Hanebuth","given":"Till","affiliations":[{"id":7156,"text":"MARUM – Center for Marine Environmental Sciences, University of Bremen","active":true,"usgs":false}],"preferred":false,"id":526780,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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