{"pageNumber":"1309","pageRowStart":"32700","pageSize":"25","recordCount":184769,"records":[{"id":70115891,"text":"70115891 - 2014 - Response to L. Land comment on Bricker, Rice, Bricker (2014) From Headwaters to Coast: Influence of human activities on water quality of the Potomac River Estuary. Aquatic Geochemistry 20: 291-324","interactions":[],"lastModifiedDate":"2021-03-16T20:53:46.205726","indexId":"70115891","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":866,"text":"Aquatic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Response to L. Land comment on Bricker, Rice, Bricker (2014) From Headwaters to Coast: Influence of human activities on water quality of the Potomac River Estuary. Aquatic Geochemistry 20: 291-324","docAbstract":"<p>Overabundance of nutrients is considered one of the top challenges to most populated coastal water bodies, including Chesapeake Bay (Executive Order 13508). As scientists, one of our responsibilities is to contribute to the discussion and evaluation of management actions that have the potential to decrease pollution with concomitant improvement of water quality. Results of our science should inform the legislative process for public policy. Bricker et al. (2014) consider the use of shellfish (i.e., oysters) to remediate nutrient pollution in the Potomac River Estuary (PRE), a tributary to Chesapeake Bay. This concept, termed bioextraction, has generated interest around the globe and has shown promise as a nutrient-removal method in other estuaries and with other shellfish species (Lindahl et al. 2005; Ferreira et al. 2009; Shumway 2011; Silva et al. 2011; Carmichael et al. 2012; Pollack et al. 2013; Rose et al. 2014).</p>","language":"English","publisher":"Springer","doi":"10.1007/s10498-014-9233-z","usgsCitation":"Bricker, S.B., Rice, K.C., and Bricker, I.O., 2014, Response to L. Land comment on Bricker, Rice, Bricker (2014) From Headwaters to Coast: Influence of human activities on water quality of the Potomac River Estuary. Aquatic Geochemistry 20: 291-324: Aquatic Geochemistry, v. 20, no. 5, p. 459-463, https://doi.org/10.1007/s10498-014-9233-z.","productDescription":"5 p.","startPage":"459","endPage":"463","ipdsId":"IP-057597","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":333060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333174,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70101080","text":"From Headwaters to Coast: Influence of human activities on water quality of the Potomac River Estuary"}],"volume":"20","issue":"5","noUsgsAuthors":false,"publicationDate":"2014-07-03","publicationStatus":"PW","scienceBaseUri":"5877230be4b0315b4c11fe6d","contributors":{"authors":[{"text":"Bricker, Suzanne B.","contributorId":64555,"corporation":false,"usgs":false,"family":"Bricker","given":"Suzanne","email":"","middleInitial":"B.","affiliations":[{"id":12448,"text":"U.S. National Oceanic and Atmospheric Administration","active":true,"usgs":false}],"preferred":false,"id":519031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":519030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bricker, III Owen Owen, P.","contributorId":119804,"corporation":false,"usgs":true,"family":"Bricker","given":"III","suffix":"Owen, P.","email":"","middleInitial":"Owen","affiliations":[],"preferred":false,"id":519032,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176232,"text":"70176232 - 2014 - Fate of nutrients in shallow groundwater receiving treated septage, Malibu, CA","interactions":[],"lastModifiedDate":"2016-09-06T20:06:38","indexId":"70176232","displayToPublicDate":"2016-09-05T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Fate of nutrients in shallow groundwater receiving treated septage, Malibu, CA","docAbstract":"<p><span>Treated wastewater discharged from more than 400 onsite wastewater treatment systems (OWTS) near the Civic Center area of Malibu, California, 40 km west of downtown Los Angeles, composes 28% of the recharge to a 3.4 km</span><sup><span>2</span></sup><span>&nbsp;alluvial aquifer. On the basis of &delta;</span><sup><span>18</span></sup><span>O and &delta;D data, the fraction of wastewater in some samples was &gt;70%. Ammonium and nitrate concentrations in water from 15 water-table wells sampled in July 2009 and April 2010 ranged from &lt;0.01 to 12 milligrams per liter as nitrogen (mg/L as N), and from &lt;0.01 to 11 mg/L as N, respectively. Chemical and isotopic data (&delta;</span><sup><span>15</span></sup><span>N of ammonium and nitrate, and &delta;</span><sup><span>18</span></sup><span>O of nitrate) show two processes remove nitrogen discharged from OWTS. Where groundwater was reducing, sorption of ammonium resulted in 30 to 50% nitrogen removal. Where groundwater was initially oxic, nitrification with subsequent denitrification as reducing conditions developed, resulted in up to 60% nitrogen removal. Nitrogen removal through sorption dominated during the cooler April sample period, and denitrification dominated during the warmer July sample period. The combination of mixing and nitrogen removal due to denitrification, sorption, and volatilization produces a &delta;</span><sup><span>15</span></sup><span>N apparent fractionation factor (&epsilon;</span><sub><span>app</span></sub><span>= -5), that can be explained using laboratory-derived fractionation factors (&epsilon;) for the individual processes. Phosphate concentrations ranged from &lt;0.04 to 2 mg/L as phosphorous. Sorption to iron oxides on the surfaces of mineral grains at near-neutral pH's removed some phosphate; however, little removal occurred at more alkaline pH's (&gt;7.3).</span></p>","language":"English","publisher":"National Groundwater Association","doi":"10.1111/gwat.12194","usgsCitation":"Izbicki, J.A., 2014, Fate of nutrients in shallow groundwater receiving treated septage, Malibu, CA: Groundwater, v. 52, no. Supplement S1, p. 218-233, https://doi.org/10.1111/gwat.12194.","productDescription":"16 p.","startPage":"218","endPage":"233","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-043823","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":472497,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/gwat.12194","text":"Publisher Index Page"},{"id":328238,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Malibu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.675,\n              34.02\n            ],\n            [\n              -118.675,\n              34.05\n            ],\n            [\n              -118.7,\n              34.05\n            ],\n            [\n              -118.7,\n              34.02\n            ],\n            [\n              -118.675,\n              34.02\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"52","issue":"Supplement S1","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2014-06-05","publicationStatus":"PW","scienceBaseUri":"57cd379ae4b0f2f0cec49185","contributors":{"authors":[{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":152474,"corporation":false,"usgs":true,"family":"Izbicki","given":"John","email":"jaizbick@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":647976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174176,"text":"70174176 - 2014 - Fine scale habitat use by age-1 stocked muskellunge and wild northern pike in an upper St. Lawrence River bay","interactions":[],"lastModifiedDate":"2016-07-12T18:19:58","indexId":"70174176","displayToPublicDate":"2016-06-27T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Fine scale habitat use by age-1 stocked muskellunge and wild northern pike in an upper St. Lawrence River bay","docAbstract":"<p><span>Radio telemetry of stocked muskellunge (</span><i>n</i><span>&nbsp;=&nbsp;6) and wild northern pike (</span><i>n</i><span>&nbsp;=&nbsp;6) was used to track late summer and fall movements from a common release point in a known shared nursery bay to test the hypothesis that age-1 northern pike and stocked muskellunge segregate and have different habitat affinities. Water depth, temperature, substrate and aquatic vegetation variables were estimated for each muskellunge (</span><i>n</i><span>&nbsp;=&nbsp;103) and northern pike (</span><i>n</i><span>&nbsp;=&nbsp;131) position and nested ANOVA comparisons by species indicated differences in habitat use. Muskellunge exhibited a greater displacement from the release point and used habitat in shallower water depths (mean&nbsp;=&nbsp;0.85&nbsp;m, SE&nbsp;=&nbsp;0.10) than northern pike (mean&nbsp;=&nbsp;1.45&nbsp;m, SE&nbsp;=&nbsp;0.08). Both principal components analysis (PCA) and principal components ordination (PCO) were used to interpret underlying gradients relative to fish positions in two-dimensional space. Our analysis indicated that a separation of age-1 northern pike and muskellunge occurred 7&nbsp;d post-release. This first principal component explained 48% of the variation in habitat use. Northern pike locations were associated with deeper habitats that generally had softer silt substrates and dense submersed vegetation. Muskellunge locations post-acclimation showed greater association with shallower habitats containing firmer sandy and clay substrates and emergent vegetation. The observed differences in habitat use suggest that fine-scale ecological separation occurred between these stocked muskellunge and wild northern pike, but small sample sizes and potential for individual variation limit extension of these conclusions. Further research is needed to determine if these patterns exist between larger samples of fishes over a greater range of habitats.</span></p>","language":"English","publisher":"International Association for Great Lakes Research","doi":"10.1016/j.jglr.2014.01.014","usgsCitation":"Farrell, J.M., Kapuscinski, K.L., and Underwood, H.B., 2014, Fine scale habitat use by age-1 stocked muskellunge and wild northern pike in an upper St. Lawrence River bay: Journal of Great Lakes Research, v. 40, Supplement 2, p. 148-153, https://doi.org/10.1016/j.jglr.2014.01.014.","productDescription":"6 p.","startPage":"148","endPage":"153","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-061058","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":324517,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","geographicExtents":"{\n  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of New York, College of Environmental Science and Forestry, Department of Environmental and Forest Biology, 250 Illick Hall, 1 Forestry Drive, Syracuse, NY 13210, USA","active":true,"usgs":false}],"preferred":false,"id":641039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapuscinski, Kevin L.","contributorId":172506,"corporation":false,"usgs":false,"family":"Kapuscinski","given":"Kevin","email":"","middleInitial":"L.","affiliations":[{"id":27059,"text":"State University of New York, College of Environmental Science and Forestry, Department of Environmental and Forest Biology, 304 Illick Hall, 1 Forestry Drive, Syracuse, NY 13210, USA","active":true,"usgs":false}],"preferred":false,"id":641040,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Underwood, H. Brian 0000-0002-2064-9128 hbunderw@usgs.gov","orcid":"https://orcid.org/0000-0002-2064-9128","contributorId":140185,"corporation":false,"usgs":true,"family":"Underwood","given":"H.","email":"hbunderw@usgs.gov","middleInitial":"Brian","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":641041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175170,"text":"70175170 - 2014 - Influences of glacial melt and permafrost thaw on the age of dissolved organic carbon in the Yukon River basin","interactions":[],"lastModifiedDate":"2017-06-29T11:59:33","indexId":"70175170","displayToPublicDate":"2016-05-25T06:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1836,"text":"Global Biogeochemical Cycles","active":true,"publicationSubtype":{"id":10}},"title":"Influences of glacial melt and permafrost thaw on the age of dissolved organic carbon in the Yukon River basin","docAbstract":"<div class=\"article-section__content mainAbstract\"><p><span>Responses of near-surface permafrost and glacial ice to climate change are of particular significance for understanding long-term effects on global carbon cycling and carbon export by high-latitude northern rivers. Here we report Δ</span><sup>14</sup><span>C-dissolved organic carbon (DOC) values and dissolved organic matter optical data for the Yukon River, 15 tributaries of the Yukon River, glacial meltwater, and groundwater and soil water end-member sources draining to the Yukon River, with the goal of assessing mobilization of aged DOC within the watershed. Ancient DOC was associated with glacial meltwater and groundwater sources. In contrast, DOC from watersheds dominated by peat soils and underlain by permafrost was typically enriched in Δ</span><sup>14</sup><span>C indicating that degradation of ancient carbon stores is currently not occurring at large enough scales to quantitatively influence bulk DOC exports from those landscapes. On an annual basis, DOC exported was predominantly modern during the spring period throughout the Yukon River basin and became older through summer-fall and winter periods, suggesting that contributions of older DOC from soils, glacial meltwaters, and groundwater are significant during these months. Our data indicate that rapidly receding glaciers and increasing groundwater inputs will likely result in greater contributions of older DOC in the Yukon River and its tributaries in coming decades.</span></p></div>","language":"English","publisher":"AGU","publisherLocation":"Hoboken, NJ","doi":"10.1002/2013GB004764","usgsCitation":"Aiken, G.R., Spencer, R., Striegl, R.G., Schuster, P.F., and Raymond, P.A., 2014, Influences of glacial melt and permafrost thaw on the age of dissolved organic carbon in the Yukon River basin: Global Biogeochemical Cycles, v. 28, no. 5, p. 525-537, https://doi.org/10.1002/2013GB004764.","productDescription":"13 p.","startPage":"525","endPage":"537","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052047","costCenters":[{"id":5044,"text":"National Research Program - Central 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,{"id":70169946,"text":"70169946 - 2014 - Collaborative modelling and integrated decision support system analysis of a developed terminal lake basin","interactions":[],"lastModifiedDate":"2016-03-31T13:37:07","indexId":"70169946","displayToPublicDate":"2016-03-31T09:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Collaborative modelling and integrated decision support system analysis of a developed terminal lake basin","docAbstract":"<p><span>A terminal lake basin in west-central Nevada, Walker Lake, has undergone drastic change over the past 90&nbsp;yrs due to upstream water use for agriculture. Decreased inflows to the lake have resulted in 100&nbsp;km</span><sup>2</sup><span>&nbsp;decrease in lake surface area and a total loss of fisheries due to salinization. The ecologic health of Walker Lake is of great concern as the lake is a stopover point on the Pacific route for migratory birds from within and outside the United States. Stakeholders, water institutions, and scientists have engaged in collaborative modeling and the development of a decision support system that is being used to develop and analyze management change options to restore the lake. Here we use an integrated management and hydrologic model that relies on state-of-the-art simulation capabilities to evaluate the benefits of using integrated hydrologic models as components of a decision support system. Nonlinear feedbacks among climate, surface-water and groundwater exchanges, and water use present challenges for simulating realistic outcomes associated with management change. Integrated management and hydrologic modeling provides a means of simulating benefits associated with management change in the Walker River basin where drastic changes in the hydrologic landscape have taken place over the last century. Through the collaborative modeling process, stakeholder support is increasing and possibly leading to management change options that result in reductions in Walker Lake salt concentrations, as simulated by the decision support system.</span></p>","language":"English","doi":"10.1016/j.jhydrol.2014.05.043","collaboration":"Bureau of Reclamation","usgsCitation":"Niswonger, R.G., Allander, K.K., and Jeton, A.E., 2014, Collaborative modelling and integrated decision support system analysis of a developed terminal lake basin: Journal of Hydrology, v. 517, p. 521-537, https://doi.org/10.1016/j.jhydrol.2014.05.043.","productDescription":"17 p.","startPage":"521","endPage":"537","numberOfPages":"17","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052113","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":319667,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Walker Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.2403564453125,\n              38.30071455572194\n            ],\n            [\n              -118.2403564453125,\n              38.30071455572194\n            ],\n            [\n              -118.2403564453125,\n              38.30071455572194\n            ],\n            [\n              -118.2403564453125,\n              38.30071455572194\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.5806884765625,\n              38.27053224010455\n            ],\n            [\n              -119.5806884765625,\n              39.13432124527173\n            ],\n            [\n              -118.28979492187499,\n              39.13432124527173\n            ],\n            [\n              -118.28979492187499,\n              38.27053224010455\n            ],\n            [\n              -119.5806884765625,\n              38.27053224010455\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"517","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56fe3c22e4b075ab2b2aa095","contributors":{"authors":[{"text":"Niswonger, Richard G. 0000-0001-6397-2403 rniswon@usgs.gov","orcid":"https://orcid.org/0000-0001-6397-2403","contributorId":152462,"corporation":false,"usgs":true,"family":"Niswonger","given":"Richard","email":"rniswon@usgs.gov","middleInitial":"G.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":625691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allander, Kip K. 0000-0002-3317-298X kalland@usgs.gov","orcid":"https://orcid.org/0000-0002-3317-298X","contributorId":2290,"corporation":false,"usgs":true,"family":"Allander","given":"Kip","email":"kalland@usgs.gov","middleInitial":"K.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":625692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jeton, Anne E.","contributorId":45351,"corporation":false,"usgs":true,"family":"Jeton","given":"Anne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":625693,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70173497,"text":"70173497 - 2014 - Reduced disease in black abalone following mass mortality: Phage therapy and natural selection","interactions":[],"lastModifiedDate":"2016-06-17T11:08:47","indexId":"70173497","displayToPublicDate":"2016-03-18T14:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1702,"text":"Frontiers in Microbiology","onlineIssn":"1664-302X","active":true,"publicationSubtype":{"id":10}},"title":"Reduced disease in black abalone following mass mortality: Phage therapy and natural selection","docAbstract":"<p><span>Black abalone,&nbsp;</span><i>Haliotis cracherodii</i><span>, populations along the NE Pacific ocean have declined due to the rickettsial disease withering syndrome (WS). Natural recovery on San Nicolas Island (SNI) of Southern California suggested the development of resistance in island populations. Experimental challenges in one treatment demonstrated that progeny of disease-selected black abalone from SNI survived better than did those from na&iuml;ve black abalone from Carmel Point in mainland coastal central California. Unexpectedly, the presence of a newly observed bacteriophage infecting the WS rickettsia (WS-RLO) had strong effects on the survival of infected abalone. Specifically, presence of phage-infected RLO (RLOv) reduced the host response to infection, RLO infection loads, and associated mortality. These data suggest that the black abalone: WS-RLO relationship is evolving through dual host mechanisms of resistance to RLO infection in the digestive gland via tolerance to infection in the primary target tissue (the post-esophagus) coupled with reduced pathogenicity of the WS-RLO by phage infection, which effectively reduces the infection load in the primary target tissue by half. Sea surface temperature patterns off southern California, associated with a recent hiatus in global-scale ocean warming, do not appear to be a sufficient explanation for survival patterns in SNI black abalone. These data highlight the potential for natural recovery of abalone populations over time and that further understanding of mechanisms governing host&ndash;parasite relationships will better enable us to manage declining populations.</span></p>","language":"English","publisher":"Frontiers","doi":"10.3389/fmicb.2014.00078","usgsCitation":"VanBlaricom, G.R., 2014, Reduced disease in black abalone following mass mortality: Phage therapy and natural selection: Frontiers in Microbiology, v. 5, no. 78, https://doi.org/10.3389/fmicb.2014.00078.","productDescription":"10 p.","startPage":"10","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054924","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":472498,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/fmicb.2014.00078","text":"Publisher Index 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,{"id":70168981,"text":"70168981 - 2014 - Eruptive and tectonic history of the Endeavour Segment, Juan de Fuca Ridge, based on AUV mapping data and lava flow ages","interactions":[],"lastModifiedDate":"2016-10-04T09:24:19","indexId":"70168981","displayToPublicDate":"2016-03-10T10:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1757,"text":"Geochemistry, Geophysics, Geosystems","active":true,"publicationSubtype":{"id":10}},"title":"Eruptive and tectonic history of the Endeavour Segment, Juan de Fuca Ridge, based on AUV mapping data and lava flow ages","docAbstract":"<p>High-resolution bathymetric surveys from autonomous underwater vehicles ABE and D. Allan B. were merged to create a coregistered map of 71.7 km2 of the Endeavour Segment of the Juan de Fuca Ridge. Radiocarbon dating of foraminifera in cores from three dives of remotely operated vehicle Doc Ricketts provide minimum eruption ages for 40 lava flows that are combined with the bathymetric data to outline the eruptive and tectonic history. The ages range from Modern to 10,700 marine-calibrated years before present (yr BP). During a robust magmatic phase from &gt;10,700 yr BP to ~4300 yr BP, flows erupted from an axial high and many flowed &gt;5 km down the flanks; some partly buried adjacent valleys. Axial magma chambers (AMCs) may have been wider than today to supply dike intrusions over a 2 km wide axial zone. Summit Seamount formed by ~4770 yr BP and was subsequently dismembered during a period of extension with little volcanism starting ~4300 yr BP. This tectonic phase with only rare volcanic eruptions lasted until ~2300 yr BP and may have resulted in near-solidification of the AMCs. The axial graben formed by crustal extension during this period of low magmatic activity. Infrequent eruptions occurred on the flanks between 2620&ndash;1760 yr BP and within the axial graben since ~1750 yr BP. This most recent phase of limited volcanic and intense hydrothermal activity that began ~2300 yr BP defines a hydrothermal phase of ridge development that coincides with the present-day 1 km wide AMCs and overlying hydrothermal vent fields.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1002/2014GC005415","usgsCitation":"Clague, D.A., Dreyer, B.M., Paduan, J.B., Martin, J.F., Caress, D., Gillespie, J.B., Kelley, D.S., Thomas, H., Portner, R.A., Delaney, J., Guilderson, T.P., and McGann, M., 2014, Eruptive and tectonic history of the Endeavour Segment, Juan de Fuca Ridge, based on AUV mapping data and lava flow ages: Geochemistry, Geophysics, Geosystems, v. 15, no. 8, p. 3364-3391, https://doi.org/10.1002/2014GC005415.","productDescription":"28 p.","startPage":"3364","endPage":"3391","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-062673","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":472499,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014gc005415","text":"Publisher Index Page"},{"id":318767,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Endeavor Segment, Juan de Fuca Ridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -129.0234375,\n              46.86019101567027\n            ],\n            [\n              -129.0234375,\n              48.21003212234042\n            ],\n            [\n              -127.7490234375,\n              48.21003212234042\n            ],\n            [\n              -127.7490234375,\n              46.86019101567027\n            ],\n      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B.","contributorId":167472,"corporation":false,"usgs":false,"family":"Paduan","given":"Jennifer","email":"","middleInitial":"B.","affiliations":[{"id":24714,"text":"Monterey Bay Aquarium Research Institite","active":true,"usgs":false}],"preferred":false,"id":622444,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Martin, Julie F","contributorId":167473,"corporation":false,"usgs":false,"family":"Martin","given":"Julie","email":"","middleInitial":"F","affiliations":[{"id":24714,"text":"Monterey Bay Aquarium Research Institite","active":true,"usgs":false}],"preferred":false,"id":622445,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Caress, David W","contributorId":147194,"corporation":false,"usgs":false,"family":"Caress","given":"David W","affiliations":[{"id":13620,"text":"Monterey Bay Aquarium Research Institute, Moss Landing, California","active":true,"usgs":false}],"preferred":false,"id":622446,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gillespie, James B.","contributorId":72809,"corporation":false,"usgs":true,"family":"Gillespie","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":622447,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kelley, Deborah S","contributorId":167474,"corporation":false,"usgs":false,"family":"Kelley","given":"Deborah","email":"","middleInitial":"S","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":622448,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Thomas, Hans","contributorId":167475,"corporation":false,"usgs":false,"family":"Thomas","given":"Hans","email":"","affiliations":[{"id":24714,"text":"Monterey Bay Aquarium Research Institite","active":true,"usgs":false}],"preferred":false,"id":622449,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Portner, Ryan A","contributorId":167476,"corporation":false,"usgs":false,"family":"Portner","given":"Ryan","email":"","middleInitial":"A","affiliations":[{"id":24714,"text":"Monterey Bay Aquarium Research Institite","active":true,"usgs":false}],"preferred":false,"id":622450,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Delaney, John R.","contributorId":167477,"corporation":false,"usgs":false,"family":"Delaney","given":"John R.","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":622451,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Guilderson, Thomas P.","contributorId":59121,"corporation":false,"usgs":true,"family":"Guilderson","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":622452,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"McGann, Mary L. 0000-0002-3057-2945 mmcgann@usgs.gov","orcid":"https://orcid.org/0000-0002-3057-2945","contributorId":147188,"corporation":false,"usgs":true,"family":"McGann","given":"Mary L.","email":"mmcgann@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":622441,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70173945,"text":"70173945 - 2014 - The rock abrasion record at Gale Crater: Mars Science Laboratory results from Bradbury Landing to Rocknest","interactions":[],"lastModifiedDate":"2018-11-14T08:31:32","indexId":"70173945","displayToPublicDate":"2016-02-24T13:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"The rock abrasion record at Gale Crater: Mars Science Laboratory results from Bradbury Landing to Rocknest","docAbstract":"<p>Ventifacts, rocks abraded by wind-borne particles, are found in Gale Crater, Mars. In the eastward drive from &ldquo;Bradbury Landing&rdquo; to &ldquo;Rocknest,&rdquo; they account for about half of the float and outcrop seen by Curiosity's cameras. Many are faceted and exhibit abrasion textures found at a range of scales, from submillimeter lineations to centimeter-scale facets, scallops, flutes, and grooves. The drive path geometry in the first 100 sols of the mission emphasized the identification of abrasion facets and textures formed by westerly flow. This upwind direction is inconsistent with predictions based on models and the orientation of regional dunes, suggesting that these ventifact features formed from very rare high-speed winds. The absence of active sand and evidence for deflation in the area indicates that most of the ventifacts are fossil features experiencing little abrasion today.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1002/2013JE004579","usgsCitation":"Bridges, N., Calef, F., Hallett, B., Herkenhoff, K.E., Lanza, N., Le Mouélic, S., Newman, C., Blaney, D., Pablo, D., Kocurek, G., Langevin, Y., Lewis, K., Mangold, N., Maurice, S., Meslin, P., Pinet, P., Renno, N., Rice, C., Richardson, M., Sautter, V., Sletten, R., Wiens, R.C., and Yingst, R., 2014, The rock abrasion record at Gale Crater: Mars Science Laboratory results from Bradbury Landing to Rocknest: Journal of Geophysical Research E: Planets, v. 119, p. 1374-1389, https://doi.org/10.1002/2013JE004579.","productDescription":"15 p.","startPage":"1374","endPage":"1389","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052431","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":472500,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2013je004579","text":"Publisher Index Page"},{"id":323957,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bradbury Landing, Gale Crater, Mars, Rocknest","volume":"119","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-06-18","publicationStatus":"PW","scienceBaseUri":"576913ece4b07657d19ff2a4","contributors":{"authors":[{"text":"Bridges, N.T.","contributorId":23673,"corporation":false,"usgs":true,"family":"Bridges","given":"N.T.","email":"","affiliations":[],"preferred":false,"id":639686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Calef, F.J. III","contributorId":91068,"corporation":false,"usgs":true,"family":"Calef","given":"F.J.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":639687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hallett, B.W.","contributorId":98392,"corporation":false,"usgs":true,"family":"Hallett","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":639688,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":639685,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lanza, N.L.","contributorId":33530,"corporation":false,"usgs":true,"family":"Lanza","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":639689,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Le Mouélic, S.","contributorId":77819,"corporation":false,"usgs":true,"family":"Le Mouélic","given":"S.","affiliations":[],"preferred":false,"id":639690,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Newman, C.E.","contributorId":172131,"corporation":false,"usgs":false,"family":"Newman","given":"C.E.","email":"","affiliations":[{"id":26988,"text":"Ashima Research, Pasadena","active":true,"usgs":false}],"preferred":false,"id":639691,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Blaney, D.L.","contributorId":43477,"corporation":false,"usgs":true,"family":"Blaney","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":639692,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Pablo, 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K.W.","contributorId":101784,"corporation":false,"usgs":true,"family":"Lewis","given":"K.W.","affiliations":[],"preferred":false,"id":639696,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Mangold, N.","contributorId":101164,"corporation":false,"usgs":true,"family":"Mangold","given":"N.","email":"","affiliations":[],"preferred":false,"id":639697,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Maurice, S.","contributorId":18144,"corporation":false,"usgs":true,"family":"Maurice","given":"S.","email":"","affiliations":[],"preferred":false,"id":639698,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Meslin, P.-Y.","contributorId":95351,"corporation":false,"usgs":true,"family":"Meslin","given":"P.-Y.","email":"","affiliations":[],"preferred":false,"id":639699,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Pinet, 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M.E.","contributorId":172136,"corporation":false,"usgs":false,"family":"Richardson","given":"M.E.","email":"","affiliations":[{"id":26988,"text":"Ashima Research, Pasadena","active":true,"usgs":false}],"preferred":false,"id":639703,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Sautter, V.","contributorId":31278,"corporation":false,"usgs":true,"family":"Sautter","given":"V.","email":"","affiliations":[],"preferred":false,"id":639704,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Sletten, R.S.","contributorId":172137,"corporation":false,"usgs":false,"family":"Sletten","given":"R.S.","email":"","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":639705,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Wiens, R. C.","contributorId":101893,"corporation":false,"usgs":false,"family":"Wiens","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":639706,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Yingst, R.A.","contributorId":101370,"corporation":false,"usgs":false,"family":"Yingst","given":"R.A.","email":"","affiliations":[{"id":24732,"text":"Planetary Science Institute, Tucson","active":true,"usgs":false}],"preferred":false,"id":639707,"contributorType":{"id":1,"text":"Authors"},"rank":23}]}}
,{"id":70173990,"text":"70173990 - 2014 - Stress-based aftershock forecasts made within 24h post mainshock: Expected north San Francisco Bay area seismicity changes after the 2014 M=6.0 West Napa earthquake","interactions":[],"lastModifiedDate":"2021-03-24T11:58:28.810308","indexId":"70173990","displayToPublicDate":"2016-02-17T06:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Stress-based aftershock forecasts made within 24h post mainshock: Expected north San Francisco Bay area seismicity changes after the 2014 <i>M</i>=6.0 West Napa earthquake","title":"Stress-based aftershock forecasts made within 24h post mainshock: Expected north San Francisco Bay area seismicity changes after the 2014 M=6.0 West Napa earthquake","docAbstract":"<p><span>We calculate stress changes resulting from the&nbsp;</span><i>M</i><span> = 6.0 West Napa earthquake on north San Francisco Bay area faults. The earthquake ruptured within a series of long faults that pose significant hazard to the Bay area, and we are thus concerned with potential increases in the probability of a large earthquake through stress transfer. We conduct this exercise as a prospective test because the skill of stress‐based aftershock forecasting methodology is inconclusive. We apply three methods: (1) generalized mapping of regional Coulomb stress change, (2) stress changes resolved on Uniform California Earthquake Rupture Forecast faults, and (3) a mapped rate/state aftershock forecast. All calculations were completed within 24 h after the main shock and were made without benefit of known aftershocks, which will be used to evaluative the prospective forecast. All methods suggest that we should expect heightened seismicity on parts of the southern Rodgers Creek, northern Hayward, and Green Valley faults.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1002/2014GL062379","usgsCitation":"Parsons, T.E., Segou, M., Sevilgen, V., Milner, K., Field, E., Toda, S., and Stein, R.S., 2014, Stress-based aftershock forecasts made within 24h post mainshock: Expected north San Francisco Bay area seismicity changes after the 2014 M=6.0 West Napa earthquake: Geophysical Research Letters, v. 41, p. 8792-8799, https://doi.org/10.1002/2014GL062379.","productDescription":"8 p.","startPage":"8792","endPage":"8799","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-061472","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":472501,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014gl062379","text":"Publisher Index Page"},{"id":324157,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Marin County, Napa County, Solanoa County, Sonoma County","city":"San Francisco","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.167724609375,\n              37.73162487017297\n            ],\n            [\n              -123.167724609375,\n              38.487994609214795\n            ],\n            [\n              -122.09243774414062,\n              38.487994609214795\n            ],\n            [\n              -122.09243774414062,\n              37.73162487017297\n            ],\n            [\n              -123.167724609375,\n              37.73162487017297\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"41","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-12-18","publicationStatus":"PW","scienceBaseUri":"576a654be4b07657d1a11e82","contributors":{"authors":[{"text":"Parsons, Thomas E. 0000-0002-0582-4338 tparsons@usgs.gov","orcid":"https://orcid.org/0000-0002-0582-4338","contributorId":2314,"corporation":false,"usgs":true,"family":"Parsons","given":"Thomas","email":"tparsons@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":640073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Segou, Margaret","contributorId":140800,"corporation":false,"usgs":false,"family":"Segou","given":"Margaret","email":"","affiliations":[{"id":13572,"text":"Geoscience Azur","active":true,"usgs":false}],"preferred":false,"id":640074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sevilgen, Volkan vsevilgen@usgs.gov","contributorId":3254,"corporation":false,"usgs":true,"family":"Sevilgen","given":"Volkan","email":"vsevilgen@usgs.gov","affiliations":[],"preferred":true,"id":640075,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Milner, Kevin","contributorId":28886,"corporation":false,"usgs":true,"family":"Milner","given":"Kevin","affiliations":[],"preferred":false,"id":640076,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Field, Edward H. 0000-0001-8172-7882 field@usgs.gov","orcid":"https://orcid.org/0000-0001-8172-7882","contributorId":1165,"corporation":false,"usgs":true,"family":"Field","given":"Edward H.","email":"field@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":640077,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Toda, Shinji","contributorId":43062,"corporation":false,"usgs":true,"family":"Toda","given":"Shinji","email":"","affiliations":[],"preferred":false,"id":640078,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stein, Ross S. 0000-0001-7586-3933 rstein@usgs.gov","orcid":"https://orcid.org/0000-0001-7586-3933","contributorId":2604,"corporation":false,"usgs":true,"family":"Stein","given":"Ross","email":"rstein@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":640079,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70173902,"text":"70173902 - 2014 - Survival and reproduction of myxobolus cerebralis-resistant Rainbow Trout introduced to the colorado river and increased resistance of age-0 progeny","interactions":[],"lastModifiedDate":"2016-06-15T12:25:46","indexId":"70173902","displayToPublicDate":"2016-02-08T14:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Survival and reproduction of myxobolus cerebralis-resistant Rainbow Trout introduced to the colorado river and increased resistance of age-0 progeny","docAbstract":"<p><i>Myxobolus cerebralis</i><span>&nbsp;caused severe declines in rainbow trout populations across Colorado following its introduction in the 1980s. One promising approach for the recovery of Colorado&rsquo;s rainbow trout populations has been the production of rainbow trout that are genetically resistant to the parasite. We introduced one of these resistant crosses, known as the GR&times;CRR (cross between the German Rainbow [GR] and Colorado River Rainbow [CRR] trout strains), to the upper Colorado River. The abundance, survival, and growth of the stocked GR&times;CRR population was examined to determine if GR&times;CRRs had contributed offspring to the age-0 population, and determine whether these offspring displayed increased resistance and survival characteristics compared to their wild CRR counterparts. Apparent survival of the introduced GR&times;CRR over the entire study period was estimated to be 0.007 (&plusmn;0.001). Despite low survival of the GR&times;CRRs, age-0 progeny of the GR&times;CRR were encountered in years 2008 through 2011. Genetic assignments revealed a shift in the genetic composition of the rainbow trout fry population over time, with CRR fish comprising the entirety of the fry population in 2007, and GR-cross fish comprising nearly 80% of the fry population in 2011. A decrease in average infection severity (myxospores fish</span><sup><span>&minus;1</span></sup><span>) was observed concurrent with the shift in the genetic composition of the rainbow trout fry population, decreasing from an average of 47,708 (&plusmn;8,950) myxospores fish</span><sup><span>&minus;1</span></sup><span>&nbsp;in 2009 to 2,672 (&plusmn;4,379) myxospores fish</span><sup><span>&minus;1</span></sup><span>&nbsp;in 2011. Results from this experiment suggest that the GR&times;CRR can survive and reproduce in rivers with a high prevalence of&nbsp;</span><i>M. cerebralis</i><span>. In addition, reduced myxospore burdens in age-0 fish indicated that stocking this cross may ultimately lead to an overall reduction in infection prevalence and severity in the salmonid populations of the upper Colorado River.</span></p>","language":"English","publisher":"PLoS ONE","publisherLocation":"San Francisco","doi":"10.1371/journal.pone.0096954","usgsCitation":"Winkelman, D.L., Fetherman, E.R., Baerwald, M.R., and Schisler, G.J., 2014, Survival and reproduction of myxobolus cerebralis-resistant Rainbow Trout introduced to the colorado river and increased resistance of age-0 progeny: PLoS ONE, e96954; 11 p, https://doi.org/10.1371/journal.pone.0096954.","productDescription":"e96954; 11 p","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-053677","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":472503,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0096954","text":"Publisher Index Page"},{"id":323681,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States, Mexico","state":"Arizona, California, Colorado, New Mexico, Utah, Wyoming","otherGeospatial":"Southwestern United States, tip of northwestern Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.74072265625,\n              32.45415593941475\n            ],\n            [\n              -116.74072265625,\n              41.95131994679697\n            ],\n            [\n              -105.22705078125,\n              41.95131994679697\n            ],\n            [\n              -105.22705078125,\n              32.45415593941475\n            ],\n            [\n              -116.74072265625,\n              32.45415593941475\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2014-05-08","publicationStatus":"PW","scienceBaseUri":"57627c38e4b07657d19a6a15","contributors":{"authors":[{"text":"Winkelman, Dana L. 0000-0002-5247-0114 danaw@usgs.gov","orcid":"https://orcid.org/0000-0002-5247-0114","contributorId":4141,"corporation":false,"usgs":true,"family":"Winkelman","given":"Dana","email":"danaw@usgs.gov","middleInitial":"L.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":639014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fetherman, Eric R.","contributorId":15096,"corporation":false,"usgs":true,"family":"Fetherman","given":"Eric","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":639015,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baerwald, Melinda R.","contributorId":171890,"corporation":false,"usgs":false,"family":"Baerwald","given":"Melinda","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":639016,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schisler, George J.","contributorId":32432,"corporation":false,"usgs":true,"family":"Schisler","given":"George","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":639017,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70173456,"text":"70173456 - 2014 - Evaluation of catch-and-release regulations on Brook Trout in Pennsylvania streams","interactions":[],"lastModifiedDate":"2016-06-17T14:47:53","indexId":"70173456","displayToPublicDate":"2016-01-26T18:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of catch-and-release regulations on Brook Trout in Pennsylvania streams","docAbstract":"<p><span>In 2004, the Pennsylvania Fish and Boat Commission implemented catch-and-release (CR) regulations on headwater stream systems to determine if eliminating angler harvest would result in an increase in the number of adult (&ge;100&nbsp;mm) or large (&ge;175&nbsp;mm) Brook Trout&nbsp;</span><i>Salvelinus fontinalis</i><span>. Under the CR regulations, angling was permitted on a year-round basis, no Brook Trout could be harvested at any time, and there were no tackle restrictions. A before-after&ndash;control-impact design was used to evaluate the experimental regulations. Brook Trout populations were monitored in 16 treatment (CR regulations) and 7 control streams (statewide regulations) using backpack electrofishing gear periodically for up to 15&nbsp;years (from 1990 to 2003 or 2004) before the implementation of the CR regulations and over a 7&ndash;8-year period (from 2004 or 2005 to 2011) after implementation. We used Poisson mixed models to evaluate whether electrofishing catch per effort (CPE; catch/100&nbsp;m</span><sup>2</sup><span>) of adult (&ge;100&nbsp;mm) or large (&ge;175&nbsp;mm) Brook Trout increased in treatment streams as a result of implementing CR regulations. Brook Trout CPE varied among sites and among years, and there was no significant effect (increase or decrease) of CR regulations on the CPE of adult or large Brook Trout. Results of our evaluation suggest that CR regulations were not effective at improving the CPE of adult or large Brook Trout in Pennsylvania streams. Low angler use, high voluntary catch and release, and slow growth rates in infertile headwater streams are likely the primary reasons for the lack of response.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02755947.2013.848251","usgsCitation":"Detar, J., Kristine, D., Wagner, T., and Greene, T., 2014, Evaluation of catch-and-release regulations on Brook Trout in Pennsylvania streams: North American Journal of Fisheries Management, v. 34, no. 1, p. 49-56, https://doi.org/10.1080/02755947.2013.848251.","productDescription":"7 p.","startPage":"49","endPage":"56","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-050734","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":498974,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02755947.2013.848251","text":"Publisher Index 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twagner@usgs.gov","orcid":"https://orcid.org/0000-0003-1726-016X","contributorId":1050,"corporation":false,"usgs":true,"family":"Wagner","given":"Tyler","email":"twagner@usgs.gov","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":637150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Greene, Tom","contributorId":172109,"corporation":false,"usgs":false,"family":"Greene","given":"Tom","email":"","affiliations":[],"preferred":false,"id":639621,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70173949,"text":"70173949 - 2014 - Prevalence of pure versus mixed snow cover pixels across spatial resolutions in alpine environments: implications for binary and fractional remote sensing approaches","interactions":[],"lastModifiedDate":"2016-06-20T10:22:54","indexId":"70173949","displayToPublicDate":"2016-01-19T07:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3250,"text":"Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Prevalence of pure versus mixed snow cover pixels across spatial resolutions in alpine environments: implications for binary and fractional remote sensing approaches","docAbstract":"<p>Remote sensing of snow-covered area (SCA) can be binary (indicating the presence/absence of snow cover at each pixel) or fractional (indicating the fraction of each pixel covered by snow). Fractional SCA mapping provides more information than binary SCA, but is more difficult to implement and may not be feasible with all types of remote sensing data. The utility of fractional SCA mapping relative to binary SCA mapping varies with the intended application as well as by spatial resolution, temporal resolution and period of interest, and climate. We quantified the frequency of occurrence of partially snow-covered (mixed) pixels at spatial resolutions between 1 m and 500 m over five dates at two study areas in the western U.S., using 0.5 m binary SCA maps derived from high spatial resolution imagery aggregated to fractional SCA at coarser spatial resolutions. In addition, we used in situ monitoring to estimate the frequency of partially snow-covered conditions for the period September 2013&ndash;August 2014 at 10 60-m grid cell footprints at two study areas with continental snow climates. Results from the image analysis indicate that at 40 m, slightly above the nominal spatial resolution of Landsat, mixed pixels accounted for 25%&ndash;93% of total pixels, while at 500 m, the nominal spatial resolution of MODIS bands used for snow cover mapping, mixed pixels accounted for 67%&ndash;100% of total pixels. Mixed pixels occurred more commonly at the continental snow climate site than at the maritime snow climate site. The in situ data indicate that some snow cover was present between 186 and 303 days, and partial snow cover conditions occurred on 10%&ndash;98% of days with snow cover. Four sites remained partially snow-free throughout most of the winter and spring, while six sites were entirely snow covered throughout most or all of the winter and spring. Within 60 m grid cells, the late spring/summer transition from snow-covered to snow-free conditions lasted 17&ndash;56 days and averaged 37 days. Our results suggest that mixed snow-covered snow-free pixels are common at the spatial resolutions imaged by both the Landsat and MODIS sensors. This highlights the additional information available from fractional SCA products and suggests fractional SCA can provide a major advantage for hydrological and climatological monitoring and modeling, particularly when accurate representation of the spatial distribution of snow cover is critical.</p>","language":"English","publisher":"MDPI","doi":"10.3390/rs61212478","usgsCitation":"Selkowitz, D.J., Forster, R., and Caldwell, M.K., 2014, Prevalence of pure versus mixed snow cover pixels across spatial resolutions in alpine environments: implications for binary and fractional remote sensing approaches: Remote Sensing, v. 6, no. 12, p. 12478-12508, https://doi.org/10.3390/rs61212478.","productDescription":"30 p.","startPage":"12478","endPage":"12508","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-060122","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":472504,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/rs61212478","text":"Publisher Index Page"},{"id":323952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"12","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2014-12-11","publicationStatus":"PW","scienceBaseUri":"576913e4e4b07657d19ff238","contributors":{"authors":[{"text":"Selkowitz, David J. 0000-0003-0824-7051 dselkowitz@usgs.gov","orcid":"https://orcid.org/0000-0003-0824-7051","contributorId":3259,"corporation":false,"usgs":true,"family":"Selkowitz","given":"David","email":"dselkowitz@usgs.gov","middleInitial":"J.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"preferred":true,"id":639740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Forster, Richard","contributorId":172149,"corporation":false,"usgs":false,"family":"Forster","given":"Richard","affiliations":[{"id":26993,"text":"University of Utah, Department of Geography","active":true,"usgs":false}],"preferred":false,"id":639741,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Caldwell, Megan K. mcaldwell@usgs.gov","contributorId":4243,"corporation":false,"usgs":true,"family":"Caldwell","given":"Megan","email":"mcaldwell@usgs.gov","middleInitial":"K.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":639742,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70173946,"text":"70173946 - 2014 - Thermal measurements of dark and bright surface features on Vesta as derived from Dawn/VIR","interactions":[],"lastModifiedDate":"2016-06-20T10:25:51","indexId":"70173946","displayToPublicDate":"2016-01-13T13:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Thermal measurements of dark and bright surface features on Vesta as derived from Dawn/VIR","docAbstract":"<p>Remote sensing data acquired during Dawn&rsquo;s orbital mission at Vesta showed several local concentrations of high-albedo (bright) and low-albedo (dark) material units, in addition to spectrally distinct meteorite impact ejecta. The thermal behavior of such areas seen at local scale (1-10 km) is related to physical properties that can provide information about the origin of those materials. We use Dawn&rsquo;s Visible and InfraRed (VIR) mapping spectrometer hyperspectral data to retrieve surface temperatures and emissivities, with high accuracy as long as temperatures are greater than 220 K. Some of the dark and bright features were observed multiple times by VIR in the various mission phases at variable spatial resolution, illumination and observation angles, local solar time, and heliocentric distance. This work presents the first temperature maps and spectral emissivities of several kilometer-scale dark and bright material units on Vesta. Results retrieved from the infrared data acquired by VIR show that bright regions generally correspond to regions with lower temperature, while dark regions correspond to areas with higher temperature. During maximum daily insolation and in the range of heliocentric distances explored by Dawn, i.e. 2.23-2.54 AU, the warmest dark unit found on Vesta rises to a temperature of 273 K, while bright units observed under comparable conditions do not exceed 266 K. Similarly, dark units appear to have higher emissivity on average compared to bright units. Dark-material units show a weak anticorrelation between temperature and albedo, whereas the relation is stronger for bright material units observed under the same conditions. Individual features may show either evanescent or distinct margins in the thermal images, as a consequence of the cohesion of the surface material. Finally, for the two categories of dark and bright materials, we were able to highlight the influence of heliocentric distance on surface temperatures, and estimate an average temperature rate change of 1% following a variation of 0.04 AU in the solar distance.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.icarus.2014.03.017","usgsCitation":"Tosi, F., Capria, M.T., Sanctis, D., Combe, J., Zambon, F., Nathues, A., Schröder, S., Li, J., Palomba, E., Longobardo, A., Blewett, D., Denevi, B., Palmer, E., Capaccioni, F., Ammannito, E., Titus, T.N., Mittlefehldt, D., Sunshine, J., Russell, C., Raymond, C., and Team, D., 2014, Thermal measurements of dark and bright surface features on Vesta as derived from Dawn/VIR: Icarus, v. 240, p. 36-57, https://doi.org/10.1016/j.icarus.2014.03.017.","productDescription":"21 p.","startPage":"36","endPage":"57","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-049721","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":323955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"240","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913ede4b07657d19ff2ac","contributors":{"authors":[{"text":"Tosi, Federico","contributorId":172138,"corporation":false,"usgs":false,"family":"Tosi","given":"Federico","email":"","affiliations":[{"id":26990,"text":"INAF-IAPS Istituto di Astrofisica e Planetologia Spaziali, Rome","active":true,"usgs":false}],"preferred":false,"id":639709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capria, Maria Teresa","contributorId":167367,"corporation":false,"usgs":false,"family":"Capria","given":"Maria","email":"","middleInitial":"Teresa","affiliations":[{"id":16145,"text":"Italian Space Agency","active":true,"usgs":false}],"preferred":false,"id":639710,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sanctis, De","contributorId":172139,"corporation":false,"usgs":false,"family":"Sanctis","given":"De","email":"","affiliations":[{"id":26990,"text":"INAF-IAPS Istituto di Astrofisica e Planetologia Spaziali, Rome","active":true,"usgs":false}],"preferred":false,"id":639711,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Combe, J.-Ph.","contributorId":172140,"corporation":false,"usgs":false,"family":"Combe","given":"J.-Ph.","email":"","affiliations":[{"id":26991,"text":"Bear Fight Institute, Winthrop, Washington","active":true,"usgs":false}],"preferred":false,"id":639712,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zambon, F.","contributorId":172141,"corporation":false,"usgs":false,"family":"Zambon","given":"F.","email":"","affiliations":[{"id":26990,"text":"INAF-IAPS Istituto di Astrofisica e Planetologia Spaziali, Rome","active":true,"usgs":false}],"preferred":false,"id":639713,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nathues, A.","contributorId":24145,"corporation":false,"usgs":true,"family":"Nathues","given":"A.","affiliations":[],"preferred":false,"id":639714,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schröder, S.E.","contributorId":172142,"corporation":false,"usgs":false,"family":"Schröder","given":"S.E.","affiliations":[{"id":26992,"text":"Institute of Planetary Research, German Aerospace Center","active":true,"usgs":false}],"preferred":false,"id":639715,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Li, J.-Y.","contributorId":172143,"corporation":false,"usgs":false,"family":"Li","given":"J.-Y.","email":"","affiliations":[{"id":24732,"text":"Planetary Science Institute, Tucson","active":true,"usgs":false}],"preferred":false,"id":639716,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Palomba, E.","contributorId":145551,"corporation":false,"usgs":false,"family":"Palomba","given":"E.","email":"","affiliations":[{"id":16145,"text":"Italian Space Agency","active":true,"usgs":false}],"preferred":false,"id":639717,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Longobardo, A.","contributorId":172144,"corporation":false,"usgs":false,"family":"Longobardo","given":"A.","email":"","affiliations":[{"id":26990,"text":"INAF-IAPS Istituto di Astrofisica e Planetologia Spaziali, Rome","active":true,"usgs":false}],"preferred":false,"id":639718,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Blewett, D.T.","contributorId":79283,"corporation":false,"usgs":true,"family":"Blewett","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":639719,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Denevi, B.W.","contributorId":20559,"corporation":false,"usgs":true,"family":"Denevi","given":"B.W.","affiliations":[],"preferred":false,"id":639720,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Palmer, E.","contributorId":172145,"corporation":false,"usgs":false,"family":"Palmer","given":"E.","email":"","affiliations":[{"id":24732,"text":"Planetary Science Institute, Tucson","active":true,"usgs":false}],"preferred":false,"id":639721,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Capaccioni, F.","contributorId":90900,"corporation":false,"usgs":true,"family":"Capaccioni","given":"F.","email":"","affiliations":[],"preferred":false,"id":639722,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Ammannito, E.","contributorId":145550,"corporation":false,"usgs":false,"family":"Ammannito","given":"E.","email":"","affiliations":[{"id":16145,"text":"Italian Space Agency","active":true,"usgs":false}],"preferred":false,"id":639723,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Titus, Timothy N. 0000-0003-0700-4875 ttitus@usgs.gov","orcid":"https://orcid.org/0000-0003-0700-4875","contributorId":146,"corporation":false,"usgs":true,"family":"Titus","given":"Timothy","email":"ttitus@usgs.gov","middleInitial":"N.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":639708,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Mittlefehldt, D.W.","contributorId":172129,"corporation":false,"usgs":false,"family":"Mittlefehldt","given":"D.W.","email":"","affiliations":[{"id":26987,"text":"ARES, NASA Johnson Space Center","active":true,"usgs":false}],"preferred":false,"id":639724,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Sunshine, J.M.","contributorId":74591,"corporation":false,"usgs":true,"family":"Sunshine","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":639725,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Russell, C.T.","contributorId":32275,"corporation":false,"usgs":false,"family":"Russell","given":"C.T.","email":"","affiliations":[{"id":33607,"text":"University of California Los Angeles","active":true,"usgs":false}],"preferred":false,"id":639726,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Raymond, C.A.","contributorId":50301,"corporation":false,"usgs":false,"family":"Raymond","given":"C.A.","email":"","affiliations":[{"id":18954,"text":"Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA","active":true,"usgs":false}],"preferred":false,"id":639727,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Team, Dawn/VIR","contributorId":172146,"corporation":false,"usgs":false,"family":"Team","given":"Dawn/VIR","email":"","affiliations":[{"id":590,"text":"U.S. Army Corps of Engineers","active":false,"usgs":false}],"preferred":false,"id":639728,"contributorType":{"id":1,"text":"Authors"},"rank":21}]}}
,{"id":70173668,"text":"70173668 - 2014 - When to be discrete: The importance of time formulation in understanding animal movement","interactions":[],"lastModifiedDate":"2016-06-08T09:57:47","indexId":"70173668","displayToPublicDate":"2016-01-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2792,"text":"Movement Ecology","active":true,"publicationSubtype":{"id":10}},"title":"When to be discrete: The importance of time formulation in understanding animal movement","docAbstract":"<p><span>Animal movement is essential to our understanding of population dynamics, animal behavior, and the impacts of global change. Coupled with high-resolution biotelemetry data, exciting new inferences about animal movement have been facilitated by various specifications of contemporary models. These approaches differ, but most share common themes. One key distinction is whether the underlying movement process is conceptualized in discrete or continuous time. This is perhaps the greatest source of confusion among practitioners, both in terms of implementation and biological interpretation. In general, animal movement occurs in continuous time but we observe it at fixed discrete-time intervals. Thus, continuous time is conceptually and theoretically appealing, but in practice it is perhaps more intuitive to interpret movement in discrete intervals. With an emphasis on state-space models, we explore the differences and similarities between continuous and discrete versions of mechanistic movement models, establish some common terminology, and indicate under which circumstances one form might be preferred over another. Counter to the overly simplistic view that discrete- and continuous-time conceptualizations are merely different means to the same end, we present novel mathematical results revealing hitherto unappreciated consequences of model formulation on inferences about animal movement. Notably, the speed and direction of movement are intrinsically linked in current continuous-time random walk formulations, and this can have important implications when interpreting animal behavior. We illustrate these concepts in the context of state-space models with multiple movement behavior states using northern fur seal (</span><i class=\"EmphasisTypeItalic\">Callorhinus ursinus</i><span>) biotelemetry data.</span></p>","language":"English","publisher":"BioMed Central","doi":"10.1186/s40462-014-0021-6","usgsCitation":"McClintock, B.T., Johnson, D., Hooten, M., Ver Hoef, J.M., and Morales, J.M., 2014, When to be discrete: The importance of time formulation in understanding animal movement: Movement Ecology, v. 2, no. 21, 14 p., https://doi.org/10.1186/s40462-014-0021-6.","productDescription":"14 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054164","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":472507,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/s40462-014-0021-6","text":"Publisher Index Page"},{"id":323248,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"21","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2014-10-15","publicationStatus":"PW","scienceBaseUri":"5759423ae4b04f417c256a1b","contributors":{"authors":[{"text":"McClintock, Brett T. 0000-0001-6154-4376","orcid":"https://orcid.org/0000-0001-6154-4376","contributorId":83785,"corporation":false,"usgs":true,"family":"McClintock","given":"Brett","email":"","middleInitial":"T.","affiliations":[{"id":12448,"text":"U.S. National Oceanic and Atmospheric Administration","active":true,"usgs":false},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":637821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Devin S.","contributorId":47524,"corporation":false,"usgs":true,"family":"Johnson","given":"Devin S.","affiliations":[],"preferred":false,"id":637822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hooten, Mevin 0000-0002-1614-723X mhooten@usgs.gov","orcid":"https://orcid.org/0000-0002-1614-723X","contributorId":2958,"corporation":false,"usgs":true,"family":"Hooten","given":"Mevin","email":"mhooten@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":12963,"text":"Colorado Cooperative Fish and Wildlife Research Unit, Fort Collins, CO","active":true,"usgs":false}],"preferred":true,"id":637476,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ver Hoef, Jay M.","contributorId":42504,"corporation":false,"usgs":true,"family":"Ver Hoef","given":"Jay","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":637823,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morales, Juan M.","contributorId":171521,"corporation":false,"usgs":false,"family":"Morales","given":"Juan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":637824,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70162210,"text":"70162210 - 2014 - Invasive Brown Treesnake movements at road edges indicate road-crossing avoidance","interactions":[],"lastModifiedDate":"2016-01-19T08:41:15","indexId":"70162210","displayToPublicDate":"2016-01-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Invasive Brown Treesnake movements at road edges indicate road-crossing avoidance","docAbstract":"<p>Roads have significant impacts on the dispersal of wildlife. Although this poses a threat to the abundance and diversity of desirable flora and fauna, it also affords some opportunity for enhancing control of invasive species. Roads are the most common terrain features that may affect the rate of landscape-scale movements of invasive Brown Treesnakes (Boiga irregularis) throughout Guam. We radio tracked 45 free-ranging Brown Treesnakes in close proximity to two roads in Guam and recorded instances where daily relocations of snakes spanned roads. Then we reconstructed observed movement histories with randomized turning angles, which served as a useful null hypothesis for assessing the effect of roads or road edge habitat on Brown Treesnake movement patterns. Random walk simulations demonstrated that Brown Treesnakes crossed these roads at a rate far lower than would be expected if snake movement was random with respect to roads and road edge habitat. We discuss two alternative hypotheses for these results: 1) habitat gaps posed by roads physically or behaviorally restrict snake movement; or 2) road edges provide preferred foraging habitat from which snakes are reluctant to depart. Because roads often form the boundaries of jurisdictional and management units, the effects of roads on the movement of invasive Brown Treesnakes will influence the prospects for success of future landscape-level suppression efforts.</p>","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","doi":"10.1670/13-037","usgsCitation":"Siers, S.R., Savidge, J.S., and Reed, R., 2014, Invasive Brown Treesnake movements at road edges indicate road-crossing avoidance: Journal of Herpetology, v. 48, no. 4, p. 500-505, https://doi.org/10.1670/13-037.","productDescription":"6 p.","startPage":"500","endPage":"505","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-051182","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":314457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Guam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              144.60411071777344,\n              13.233261466546951\n            ],\n            [\n              144.60411071777344,\n              13.655328309840225\n            ],\n            [\n              144.97283935546872,\n              13.655328309840225\n            ],\n            [\n              144.97283935546872,\n              13.233261466546951\n            ],\n            [\n              144.60411071777344,\n              13.233261466546951\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"48","issue":"4","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c45e4b0961cf27fd1ab","contributors":{"authors":[{"text":"Siers, Shane R.","contributorId":152305,"corporation":false,"usgs":false,"family":"Siers","given":"Shane","email":"","middleInitial":"R.","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":588864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savidge, Julie S","contributorId":152306,"corporation":false,"usgs":false,"family":"Savidge","given":"Julie","email":"","middleInitial":"S","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":588865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, Robert N. reedr@usgs.gov","contributorId":1686,"corporation":false,"usgs":true,"family":"Reed","given":"Robert N.","email":"reedr@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":588863,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170586,"text":"70170586 - 2014 - Experimental manipulation of TN:TP ratiossuppress cyanobacterial biovolume and microcystinconcentration in large-scale <i>in situ</i> mesocosms","interactions":[],"lastModifiedDate":"2016-04-27T10:25:05","indexId":"70170586","displayToPublicDate":"2016-01-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2592,"text":"Lake and Reservoir Management","active":true,"publicationSubtype":{"id":10}},"title":"Experimental manipulation of TN:TP ratiossuppress cyanobacterial biovolume and microcystinconcentration in large-scale <i>in situ</i> mesocosms","docAbstract":"<p><span>A global dataset was compiled to examine relations between the total nitrogen to total phosphorus ratio (TN:TP) and microcystin concentration in lakes and reservoirs. Microcystin concentration decreased as TN:TP ratios increased, suggesting that manipulation of the TN:TP ratio may reduce microcystin concentrations. This relationship was experimentally tested by adding ammonium nitrate to increase the TN:TP ratio in large-scale (70&nbsp;m</span><sup>3</sup><span>),&nbsp;</span><i>in situ</i><span>&nbsp;mesocosms located in a eutrophic reservoir that routinely experiences toxic blooms of cyanobacteria. At a TN:TP ratio &gt;75:1, chlorophytes dominated the phytoplankton community in the mesocosms, while cyanobacterial biovolume was significantly reduced and microcystin was not detected. In contrast, the unmanipulated reservoir was dominated by cyanobacteria, and microcystin was detected. Secchi depths were 1.1 to 1.8&nbsp;times greater in the mesocosms relative to the reservoir. Cladoceran zooplankton had a larger body size (0.14&nbsp;mm on average) in the mesocosms compared to conspecifics in the reservoir, which was likely related to the higher quality food. Combined, these empirical and experimental data indicate that although nutrient addition is counterintuitive to current cyanobacteria management practices, increasing the TN:TP ratio by adding nitrogen may be a potential short-term management strategy to reduce cyanobacteria and cyanotoxins when other alternatives (e.g., phosphorus reduction) are not possible. Additional experimental studies with careful controls are needed to define best management practices and identify any potential unintended consequences before nitrogen addition is implemented as a lake and reservoir management practice.</span></p>","language":"English","publisher":"Taylor and Francis","doi":"10.1080/10402381.2013.876131","usgsCitation":"Harris, T.D., Wilhelm, F.M., Graham, J., and Loftin, K.A., 2014, Experimental manipulation of TN:TP ratiossuppress cyanobacterial biovolume and microcystinconcentration in large-scale <i>in situ</i> mesocosms: Lake and Reservoir Management, v. 30, no. 1, p. 72-83, https://doi.org/10.1080/10402381.2013.876131.","productDescription":"12 p.","startPage":"72","endPage":"83","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052249","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":472505,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/10402381.2013.876131","text":"Publisher Index Page"},{"id":320594,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"1","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationDate":"2014-01-30","publicationStatus":"PW","scienceBaseUri":"5721e2b3e4b0b13d3913032b","contributors":{"authors":[{"text":"Harris, Theodore D. 0000-0003-0944-8007 tdharris@usgs.gov","orcid":"https://orcid.org/0000-0003-0944-8007","contributorId":4040,"corporation":false,"usgs":true,"family":"Harris","given":"Theodore","email":"tdharris@usgs.gov","middleInitial":"D.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":627768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilhelm, Frank M.","contributorId":149759,"corporation":false,"usgs":false,"family":"Wilhelm","given":"Frank","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":627769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graham, Jennifer L. 0000-0002-6420-9335 jlgraham@usgs.gov","orcid":"https://orcid.org/0000-0002-6420-9335","contributorId":150737,"corporation":false,"usgs":true,"family":"Graham","given":"Jennifer L.","email":"jlgraham@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":627770,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Loftin, Keith A. 0000-0001-5291-876X kloftin@usgs.gov","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":868,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","email":"kloftin@usgs.gov","middleInitial":"A.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":627771,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70135054,"text":"70135054 - 2014 - Final Project Memorandum: Ecological implications of mangrove forest migration in the southeastern U.S.","interactions":[],"lastModifiedDate":"2017-06-13T16:35:43","indexId":"70135054","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Final Project Memorandum: Ecological implications of mangrove forest migration in the southeastern U.S.","docAbstract":"Winter climate change has the potential to have a large impact on coastal wetlands in the southeastern United States. Warmer winter temperatures and reductions in the intensity of freeze events would likely lead to mangrove forest range expansion and salt marsh displacement in parts of the U.S. Gulf of Mexico and Atlantic coast. The objective of this research was to better evaluate the ecological implications of mangrove forest migration and salt marsh displacement. The potential ecological impacts of mangrove migration are diverse ranging from important biotic impacts (e.g., coastal fisheries, land bird migration; colonial-nesting wading birds) to ecosystem stability (e.g., response to sea level rise and drought; habitat loss; coastal protection) to biogeochemical processes (e.g., carbon storage; water quality). This research specifically investigated the impact of mangrove forest migration on coastal wetland soil processes and the consequent implications for coastal wetland responses to sea level rise and carbon storage.","language":"English","publisher":"Department of Interior Southeast Climate Science Center","publisherLocation":"Raleigh, NC ","usgsCitation":"Osland, M.J., Day, R.H., Krauss, K.W., From, A.S., Larriviere, J.C., Hester, M.W., Yando, E.S., and Willis, J., 2014, Final Project Memorandum: Ecological implications of mangrove forest migration in the southeastern U.S., 14 p.","productDescription":"14 p.","ipdsId":"IP-061252","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":342446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342445,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://globalchange.ncsu.edu/secsc/projects/ecological-implications-of-mangrove-forest-migration-in-the-southeastern-united-states/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5940f9b5e4b0764e6c63ead5","contributors":{"authors":[{"text":"Osland, Michael J. 0000-0001-9902-8692 mosland@usgs.gov","orcid":"https://orcid.org/0000-0001-9902-8692","contributorId":3080,"corporation":false,"usgs":true,"family":"Osland","given":"Michael","email":"mosland@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":526756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, Richard H. 0000-0002-5959-7054 dayr@usgs.gov","orcid":"https://orcid.org/0000-0002-5959-7054","contributorId":2427,"corporation":false,"usgs":true,"family":"Day","given":"Richard","email":"dayr@usgs.gov","middleInitial":"H.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":526757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krauss, Ken W. 0000-0003-2195-0729 kraussk@usgs.gov","orcid":"https://orcid.org/0000-0003-2195-0729","contributorId":2017,"corporation":false,"usgs":true,"family":"Krauss","given":"Ken","email":"kraussk@usgs.gov","middleInitial":"W.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":526760,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"From, Andrew S. 0000-0002-6543-2627 froma@usgs.gov","orcid":"https://orcid.org/0000-0002-6543-2627","contributorId":5038,"corporation":false,"usgs":true,"family":"From","given":"Andrew","email":"froma@usgs.gov","middleInitial":"S.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":526761,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Larriviere, Jack C. jlarriviere@usgs.gov","contributorId":5839,"corporation":false,"usgs":true,"family":"Larriviere","given":"Jack","email":"jlarriviere@usgs.gov","middleInitial":"C.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":526763,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hester, Mark W.","contributorId":9566,"corporation":false,"usgs":true,"family":"Hester","given":"Mark","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":526759,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Yando, Erik S.","contributorId":127788,"corporation":false,"usgs":false,"family":"Yando","given":"Erik","email":"","middleInitial":"S.","affiliations":[{"id":7155,"text":"University of Louisiana at Lafayette","active":true,"usgs":false}],"preferred":false,"id":526758,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Willis, Jonathan A","contributorId":127789,"corporation":false,"usgs":false,"family":"Willis","given":"Jonathan A","affiliations":[{"id":7155,"text":"University of Louisiana at Lafayette","active":true,"usgs":false}],"preferred":false,"id":526762,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70135997,"text":"70135997 - 2014 - Physically based method for measuring suspended-sediment concentration and grain size using multi-frequency arrays of acoustic-doppler profilers","interactions":[],"lastModifiedDate":"2017-06-14T15:15:39","indexId":"70135997","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Physically based method for measuring suspended-sediment concentration and grain size using multi-frequency arrays of acoustic-doppler profilers","docAbstract":"<p>As the result of a 12-year program of sediment-transport research and field testing on the Colorado River (6 stations in UT and AZ), Yampa River (2 stations in CO), Little Snake River (1 station in CO), Green River (1 station in CO and 2 stations in UT), and Rio Grande (2 stations in TX), we have developed a physically based method for measuring suspended-sediment concentration and grain size at 15-minute intervals using multifrequency arrays of acoustic-Doppler profilers. This multi-frequency method is able to achieve much higher accuracies than single-frequency acoustic methods because it allows removal of the influence of changes in grain size on acoustic backscatter. The method proceeds as follows. (1) Acoustic attenuation at each frequency is related to the concentration of silt and clay with a known grain-size distribution in a river cross section using physical samples and theory. (2) The combination of acoustic backscatter and attenuation at each frequency is uniquely related to the concentration of sand (with a known reference grain-size distribution) and the concentration of silt and clay (with a known reference grain-size distribution) in a river cross section using physical samples and theory. (3) Comparison of the suspended-sand concentrations measured at each frequency using this approach then allows theory-based calculation of the median grain size of the suspended sand and final correction of the suspended-sand concentration to compensate for the influence of changing grain size on backscatter. Although this method of measuring suspended-sediment concentration is somewhat less accurate than using conventional samplers in either the EDI or EWI methods, it is much more accurate than estimating suspended-sediment concentrations using calibrated pump measurements or single-frequency acoustics. Though the EDI and EWI methods provide the most accurate measurements of suspended-sediment concentration, these measurements are labor-intensive, expensive, and may be impossible to collect at time intervals less than discharge-independent changes in suspended-sediment concentration can occur (&lt; hours). Therefore, our physically based multi-frequency acoustic method shows promise as a cost-effective, valid approach for calculating suspended-sediment loads in river at a level of accuracy sufficient for many scientific and management purposes.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 2015 Joint Federal Interagency Conference on Sedimentation and Hydrologic Modeling ","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"SEDHYD 2015 Conference","conferenceDate":"April 19-23, 2015","conferenceLocation":"Reno, NV","language":"English","usgsCitation":"Topping, D.J., Wright, S., Griffiths, R.E., and Dean, D.J., 2014, Physically based method for measuring suspended-sediment concentration and grain size using multi-frequency arrays of acoustic-doppler profilers, <i>in</i> Proceedings of the 2015 Joint Federal Interagency Conference on Sedimentation and Hydrologic Modeling , Reno, NV, April 19-23, 2015, 14 p.","productDescription":"14 p.","ipdsId":"IP-061039","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":342444,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342443,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.sedhyd.org/2015/openconf/modules/request.php?module=oc_program&action=summary.php&id=250"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5940f9b5e4b0764e6c63ead1","contributors":{"authors":[{"text":"Topping, David J. 0000-0002-2104-4577 dtopping@usgs.gov","orcid":"https://orcid.org/0000-0002-2104-4577","contributorId":715,"corporation":false,"usgs":true,"family":"Topping","given":"David","email":"dtopping@usgs.gov","middleInitial":"J.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":false,"id":537048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, Scott 0000-0002-0387-5713 sawright@usgs.gov","orcid":"https://orcid.org/0000-0002-0387-5713","contributorId":1536,"corporation":false,"usgs":true,"family":"Wright","given":"Scott","email":"sawright@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":537049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Griffiths, Ronald E. 0000-0003-3620-2926 rgriffiths@usgs.gov","orcid":"https://orcid.org/0000-0003-3620-2926","contributorId":162,"corporation":false,"usgs":true,"family":"Griffiths","given":"Ronald","email":"rgriffiths@usgs.gov","middleInitial":"E.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":537050,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dean, David J. 0000-0003-0203-088X djdean@usgs.gov","orcid":"https://orcid.org/0000-0003-0203-088X","contributorId":131047,"corporation":false,"usgs":true,"family":"Dean","given":"David","email":"djdean@usgs.gov","middleInitial":"J.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":537051,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70189612,"text":"70189612 - 2014 - Elders recall an earlier tsunami on Indian Ocean shores","interactions":[],"lastModifiedDate":"2018-02-21T13:53:48","indexId":"70189612","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"Elders recall an earlier tsunami on Indian Ocean shores","docAbstract":"Ten years on, the Indian Ocean tsunami of 26 December 2004 still looms large in efforts to reduce coastal risk. The disaster has spurred worldwide advances in tsunami detection and warning, tsunami-risk assessment, and tsunami awareness [Satake, 2014].\n\tNearly a lifetime has passed since the northwestern Indian Ocean last produced a devastating tsunami. Documentation of this tsunami, in November 1945, was hindered by international instability in the wake of the Second World War and, in British India, by the approach of independence and partition. The parent earthquake, of magnitude 8.1, was widely recorded, and the tsunami registered on tide gauges, but intelligence reports and newspaper articles say little about inundation limits while permitting a broad range of catalogued death tolls. What has been established about the 1945 tsunami falls short of what's needed today for ground-truthing inundation models, estimating risk to enlarged populations, and anchoring awareness campaigns in local facts.\n\tRecent efforts to reduce coastal risk around the Arabian Sea include a project in which eyewitnesses to the 1945 tsunami were found and interviewed (Fig. 1), and related archives were gathered. Results are being made available through UNESCO's Indian Ocean Tsunami Information Center in hopes of increasing scientific understanding and public awareness of the region's tsunami hazards.","language":"English","publisher":"American Geophysical Union","doi":"10.1002/2014EO510002","usgsCitation":"Kakar, D.M., Naeem, G., Usman, A., Hasan, H., Lohdi, H., Srinivasalu, S., Andrade, V., Rajendran, C., Naderi Beni, A., Hamzeh, M.A., Hoffmann, G., Al Balushi, N., Gale, N., Kodijat, A., Fritz, H.M., and Atwater, B.F., 2014, Elders recall an earlier tsunami on Indian Ocean shores: Eos, Earth and Space Science News, v. 95, no. 51, p. 485-486, https://doi.org/10.1002/2014EO510002.","productDescription":"2 p.","startPage":"485","endPage":"486","ipdsId":"IP-060909","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":472508,"rank":0,"type":{"id":41,"text":"Open Access External Repository 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,{"id":70129357,"text":"70129357 - 2014 - Estimating the magnitude and frequency of floods for urban and small, rural streams in Georgia, South Carolina, and North Carolina","interactions":[],"lastModifiedDate":"2017-06-13T17:50:57","indexId":"70129357","displayToPublicDate":"2015-12-31T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Estimating the magnitude and frequency of floods for urban and small, rural streams in Georgia, South Carolina, and North Carolina","docAbstract":"Reliable estimates of the magnitude and frequency of floods are essential for such things as the design of transportation and water-conveyance structures, Flood Insurance Studies, and flood-plain management. The flood-frequency estimates are particularly important in densely populated urban areas. A multistate approach was used to update methods for determining the magnitude and frequency of floods in urban and small, rural streams that are not substantially affected by regulation or tidal fluctuations in Georgia, South Carolina, and North Carolina. The multistate approach has the advantage over a single state approach of increasing the number of stations available for analysis, expanding the geographical coverage that would allow for application of regional regression equations across state boundaries, and building on a previous flood-frequency investigation of rural streamflow-gaging stations (streamgages) in the Southeastern United States. In addition, streamgages from the inner Coastal Plain of New Jersey were included in the analysis.\r\nGeneralized least-squares regression techniques were used to generate predictive  equations for estimating the 50-, 20-, 10-, 4-, 2-, 1-, 0.5-, and 0.2-percent annual exceedance probability flows for urban and small, rural ungaged basins for three hydrologic regions; the Piedmont-Ridge and Valley, Sand Hills, and Coastal Plain. Incorporation of urban streamgages from New Jersey also allowed for the expansion of the applicability of the predictive equations in the Coastal Plain from 2.1 to 53.5 square miles. Explanatory variables in the regression equations included drainage area (DA) and percent of impervious area (IA) for the Piedmont-Ridge and Valley region; DA and percent of developed land for the Sand Hills; and DA, IA, and 24-hour, 50-year maximum precipitation for the Coastal Plain. An application spreadsheet also was developed that can be used to compute the flood-frequency estimates along with the 95-percent prediction intervals for an ungaged location. \r\n","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 3rd Joint Federal Interagency Conference on Sedimentation and Hydrologic Modeling","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"SEDHYD 2015","conferenceDate":"April 19-23, 2015","conferenceLocation":"Reno, NV","language":"English","publisher":"Department of Interior","usgsCitation":"Feaster, T., Gotvald, A.J., and Weaver, J.C., 2014, Estimating the magnitude and frequency of floods for urban and small, rural streams in Georgia, South Carolina, and North Carolina, 9 p.","productDescription":"9 p.","startPage":"512","endPage":"520","ipdsId":"IP-059335","costCenters":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"links":[{"id":342454,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342453,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://acwi.gov/sos/pubs/3rdJFIC/"}],"country":"United States","state":"Georgia, North Carolina, South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.85791015625,\n              29.38217507514529\n            ],\n            [\n              -75.05859375,\n              29.38217507514529\n            ],\n            [\n              -75.05859375,\n              37.3002752813443\n            ],\n            [\n              -86.85791015625,\n              37.3002752813443\n            ],\n            [\n              -86.85791015625,\n              29.38217507514529\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5940f9b5e4b0764e6c63ead8","contributors":{"authors":[{"text":"Feaster, Toby D. 0000-0002-5626-5011 tfeaster@usgs.gov","orcid":"https://orcid.org/0000-0002-5626-5011","contributorId":1109,"corporation":false,"usgs":true,"family":"Feaster","given":"Toby D.","email":"tfeaster@usgs.gov","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":519848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gotvald, Anthony J. 0000-0002-9019-750X agotvald@usgs.gov","orcid":"https://orcid.org/0000-0002-9019-750X","contributorId":1970,"corporation":false,"usgs":true,"family":"Gotvald","given":"Anthony","email":"agotvald@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":519849,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, J. Curtis 0000-0001-7068-5445 jcweaver@usgs.gov","orcid":"https://orcid.org/0000-0001-7068-5445","contributorId":2229,"corporation":false,"usgs":true,"family":"Weaver","given":"J.","email":"jcweaver@usgs.gov","middleInitial":"Curtis","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":519850,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70173455,"text":"70173455 - 2014 - Regional variability among nonlinear chlorophyll-phosphorus relationships in lakes","interactions":[],"lastModifiedDate":"2016-06-17T14:53:37","indexId":"70173455","displayToPublicDate":"2015-12-22T13:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Regional variability among nonlinear chlorophyll-phosphorus relationships in lakes","docAbstract":"<p><span>The relationship between chlorophyll&nbsp;</span><i>a</i><span>&nbsp;(Chl&nbsp;</span><i>a</i><span>) and total phosphorus (TP) is a fundamental relationship in lakes that reflects multiple aspects of ecosystem function and is also used in the regulation and management of inland waters. The exact form of this relationship has substantial implications on its meaning and its use. We assembled a spatially extensive data set to examine whether nonlinear models are a better fit for Chl&nbsp;</span><i>a</i><span>&mdash;TP relationships than traditional log-linear models, whether there were regional differences in the form of the relationships, and, if so, which regional factors were related to these differences. We analyzed a data set from 2105 temperate lakes across 35 ecoregions by fitting and comparing two different nonlinear models and one log-linear model. The two nonlinear models fit the data better than the log-linear model. In addition, the parameters for the best-fitting model varied among regions: the maximum and lower Chl&nbsp;</span><i>a</i><span>asymptotes were positively and negatively related to percent regional pasture land use, respectively, and the rate at which chlorophyll increased with TP was negatively related to percent regional wetland cover. Lakes in regions with more pasture fields had higher maximum chlorophyll concentrations at high TP concentrations but lower minimum chlorophyll concentrations at low TP concentrations. Lakes in regions with less wetland cover showed a steeper Chl&nbsp;</span><i>a</i><span>&mdash;TP relationship than wetland-rich regions. Interpretation of Chl&nbsp;</span><i>a</i><span>&mdash;TP relationships depends on regional differences, and theory and management based on a monolithic relationship may be inaccurate.</span></p>","language":"English","publisher":"ASLO","doi":"10.4319/lo.2014.59.5.1691","usgsCitation":"Filstrup, C.T., Wagner, T., Soranno, P.A., Stanley, E.H., Stow, C., Webster, K.E., and Downing, J., 2014, Regional variability among nonlinear chlorophyll-phosphorus relationships in lakes: Limnology and Oceanography, v. 59, no. 5, p. 1691-1703, https://doi.org/10.4319/lo.2014.59.5.1691.","productDescription":"12 p.","startPage":"1691","endPage":"1703","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-051853","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":323926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa, Maine, Michigan, New Hampshire, Ohio, 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,{"id":70171553,"text":"70171553 - 2014 - USGS geologic Mapping and karst research in the Ozark National Scenic Riverways, Missouri, USA","interactions":[],"lastModifiedDate":"2016-06-03T13:10:43","indexId":"70171553","displayToPublicDate":"2015-12-22T13:15:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1809,"text":"George Wright Society Forum","active":true,"publicationSubtype":{"id":10}},"title":"USGS geologic Mapping and karst research in the Ozark National Scenic Riverways, Missouri, USA","docAbstract":"<p>The Ozark National Scenic Riverways (ONSR) was created in 1964 to protect 134 miles of the Current River and its major tributary, the Jacks Fork, that are located in south-central Missouri (fig. 1). The park includes numerous large karst springs including Big Spring, by flow volume this is the largest spring in the National Park system. The National Park Service (NPS) administers a narrow, nearly continuous corridor of land adjacent to the two rivers. Base flow for the rivers is chiefly supplied by groundwater that has traveled through the karst landscape from as far as 38 miles away from the spring (Imes and Frederick, 2002). The watershed is vulnerable to pollution, but the area remains largely rural with few industries. The springs and rivers provide habitat for numerous aquatic species as well as recreational resources for floaters, fishermen, and campers. The ONSR is a major cave park with hundreds of known caves and diverse in-cave resources.</p>","language":"English","publisher":"George Wright Society","collaboration":"National Park Service","usgsCitation":"Weary, D.J., and Grant, V.M., 2014, USGS geologic Mapping and karst research in the Ozark National Scenic Riverways, Missouri, USA: George Wright Society Forum, v. 31, no. 2, p. 157-167.","productDescription":"10 p.","startPage":"157","endPage":"167","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-051107","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":322140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":322137,"type":{"id":15,"text":"Index Page"},"url":"https://www.georgewright.org/node/10198"}],"country":"United States","state":"Missouri","otherGeospatial":"Ozark National Scenic Rivers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.61361694335938,\n              36.893899678382716\n            ],\n            [\n              -91.61361694335938,\n              37.276238364942955\n            ],\n            [\n              -90.93795776367188,\n              37.276238364942955\n            ],\n            [\n              -90.93795776367188,\n              36.893899678382716\n            ],\n            [\n              -91.61361694335938,\n              36.893899678382716\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"2","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5752aa3ae4b053f0edd13ebf","contributors":{"authors":[{"text":"Weary, David J. 0000-0002-6115-6397 dweary@usgs.gov","orcid":"https://orcid.org/0000-0002-6115-6397","contributorId":545,"corporation":false,"usgs":true,"family":"Weary","given":"David","email":"dweary@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":631760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, Victoria M","contributorId":170004,"corporation":false,"usgs":false,"family":"Grant","given":"Victoria","email":"","middleInitial":"M","affiliations":[{"id":5106,"text":"National Park Service, Yellowstone National Park, Mammoth, Wyoming 82190","active":true,"usgs":false}],"preferred":false,"id":631761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173468,"text":"70173468 - 2014 - Predictive Management of Asian Carps in the Upper Mississippi River System","interactions":[],"lastModifiedDate":"2016-06-17T13:57:45","indexId":"70173468","displayToPublicDate":"2015-12-16T14:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5040,"text":"Reviews in Fisheries Science & Aquaculture","onlineIssn":"2330-8257","printIssn":"2330-8249","active":true,"publicationSubtype":{"id":10}},"title":"Predictive Management of Asian Carps in the Upper Mississippi River System","docAbstract":"<p><span>Prolific non-native organisms pose serious threats to ecosystems and economies worldwide. Nonnative bighead carp (</span><i>Hypophthalmichthys nobilis</i><span>) and silver carp (</span><i>H. molitrix</i><span>), collectively referred to as Asian carps, continue to colonize aquatic ecosystems throughout the central United States. These species are r-selected, exhibiting iteroparous spawning, rapid growth, broad environmental tolerance, high density, and long-distance movement. Hydrological, thermal, and physicochemical conditions are favorable for establishment beyond the current range, rendering containment and control imperative. Ecological approaches to confine Asian carp populations and prevent colonization characterize contemporary management in the United States. Foraging and reproduction of Asian carps govern habitat selection and movement, providing valuable insight for predictive control. Current management approaches are progressive and often anticipatory but deficient in human dimensions. We define predictive management of Asian carps as synthesis of ecology and human dimensions at regional and local scales to develop strategies for containment and control. We illustrate predictive management in the Upper Mississippi River System and suggest resource managers integrate predictive models, containment paradigms, and human dimensions to design effective, socially acceptable management strategies. Through continued research, university-agency collaboration, and public engagement, predictive management of Asian carps is an auspicious paradigm for preventing and alleviating consequences of colonization in the United States.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/23308249.2014.967747","usgsCitation":"Vondracek, B.C., and Carlson, A.K., 2014, Predictive Management of Asian Carps in the Upper Mississippi River System: Reviews in Fisheries Science & Aquaculture, v. 22, no. 4, p. 284-300, https://doi.org/10.1080/23308249.2014.967747.","productDescription":"16 p.","startPage":"284","endPage":"300","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054341","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":323904,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70173457,"text":"70173457 - 2014 - A regional neural network model for predicting mean daily river water temperature","interactions":[],"lastModifiedDate":"2016-06-17T14:44:17","indexId":"70173457","displayToPublicDate":"2015-12-15T14:30:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"A regional neural network model for predicting mean daily river water temperature","docAbstract":"<p><span>Water temperature is a fundamental property of river habitat and often a key aspect of river resource management, but measurements to characterize thermal regimes are not available for most streams and rivers. As such, we developed an artificial neural network (ANN) ensemble model to predict mean daily water temperature in 197,402 individual stream reaches during the warm season (May&ndash;October) throughout the native range of brook trout&nbsp;</span><i>Salvelinus fontinalis</i><span>&nbsp;in the eastern U.S. We compared four models with different groups of predictors to determine how well water temperature could be predicted by climatic, landform, and land cover attributes, and used the median prediction from an ensemble of 100 ANNs as our final prediction for each model. The final model included air temperature, landform attributes and forested land cover and predicted mean daily water temperatures with moderate accuracy as determined by root mean squared error (RMSE) at 886 training sites with data from 1980 to 2009 (RMSE&nbsp;=&nbsp;1.91&nbsp;&deg;C). Based on validation at 96 sites (RMSE&nbsp;=&nbsp;1.82) and separately for data from 2010 (RMSE&nbsp;=&nbsp;1.93), a year with relatively warmer conditions, the model was able to generalize to new stream reaches and years. The most important predictors were mean daily air temperature, prior 7&nbsp;day mean air temperature, and network catchment area according to sensitivity analyses. Forest land cover at both riparian and catchment extents had relatively weak but clear negative effects. Predicted daily water temperature averaged for the month of July matched expected spatial trends with cooler temperatures in headwaters and at higher elevations and latitudes. Our ANN ensemble is unique in predicting daily temperatures throughout a large region, while other regional efforts have predicted at relatively coarse time steps. The model may prove a useful tool for predicting water temperatures in sampled and unsampled rivers under current conditions and future projections of climate and land use changes, thereby providing information that is valuable to management of river ecosystems and biota such as brook trout.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2014.05.035","usgsCitation":"Wagner, T., and DeWeber, J.T., 2014, A regional neural network model for predicting mean daily river water temperature: Journal of Hydrology, v. 517, p. 187-200, https://doi.org/10.1016/j.jhydrol.2014.05.035.","productDescription":"13 p.","startPage":"187","endPage":"200","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-046229","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":323923,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  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