Nine stream sites in the Blackfoot River, Salt River, and Bear River watersheds in southeast Idaho, USA were sampled in May 2001 for water, surficial sediment, aquatic plants, aquatic invertebrates, and fish. Selenium was measured in these aquatic ecosystem components, and a hazard assessment was performed on the data. Water quality characteristics such as pH, hardness, and specific conductance were relatively uniform among the nine sites. Of the aquatic components assessed, water was the least contaminated with selenium because measured concentrations were below the national water quality criterion of 5 μ g/L at eight of the nine sites. In contrast, selenium was elevated in sediment, aquatic plants, aquatic invertebrates, and fish from several sites, suggesting deposition in sediments and food web cycling through plants and invertebrates. Selenium was elevated to concentrations of concern in fish at eight sites (> 4 μ g/g in whole body). A hazard assessment of selenium in the aquatic environment suggested a moderate hazard at upper Angus Creek (UAC) and Smoky Creek (SC), and high hazard at Little Blackfoot River (LiB), Blackfoot River gaging station (BGS), State Land Creek (SLC), upper (UGC) and lower Georgetown Creek (LGC), Deer Creek (DC), and Crow Creek (CC). The results of this study indicate that selenium concentrations from the phosphate mining area of southeast Idaho were sufficiently elevated in several ecosystem components to cause adverse effects to aquatic resources in southeastern Idaho.
","language":"English","publisher":"Springer","doi":"10.1007/s10661-005-1618-4","issn":"01676369","usgsCitation":"Hamilton, S.J., and Buhl, K., 2005, Selenium in the Blackfoot, Salt, and Bear River Watersheds: Environmental Monitoring and Assessment, v. 104, no. 1-3, p. 309-339, https://doi.org/10.1007/s10661-005-1618-4.","productDescription":"31 p.","startPage":"309","endPage":"339","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":210680,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10661-005-1618-4"},{"id":237675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8cf6e4b08c986b3181e2","contributors":{"authors":[{"text":"Hamilton, S. J.","contributorId":27817,"corporation":false,"usgs":false,"family":"Hamilton","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buhl, K.J.","contributorId":19728,"corporation":false,"usgs":true,"family":"Buhl","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":422972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029496,"text":"70029496 - 2005 - Progress in NTHMP Hazard Assessment","interactions":[],"lastModifiedDate":"2012-03-12T17:20:52","indexId":"70029496","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2822,"text":"Natural Hazards","active":true,"publicationSubtype":{"id":10}},"title":"Progress in NTHMP Hazard Assessment","docAbstract":"The Hazard Assessment component of the U.S. National Tsunami Hazard Mitigation Program has completed 22 modeling efforts covering 113 coastal communities with an estimated population of 1.2 million residents that are at risk. Twenty-three evacuation maps have also been completed. Important improvements in organizational structure have been made with the addition of two State geotechnical agency representatives to Steering Group membership, and progress has been made on other improvements suggested by program reviewers. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Hazards","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11069-004-2406-0","issn":"0921030X","usgsCitation":"Gonzalez, F., Titov, V., Mofjeld, H., Venturato, A., Simmons, R., Hansen, R., Combellick, R., Eisner, R., Hoirup, D., Yanagi, B., Yong, S., Darienzo, M., Priest, G.R., Crawford, G., and Walsh, T.J., 2005, Progress in NTHMP Hazard Assessment: Natural Hazards, v. 35, no. 1, p. 89-110, https://doi.org/10.1007/s11069-004-2406-0.","startPage":"89","endPage":"110","numberOfPages":"22","costCenters":[],"links":[{"id":237710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210704,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11069-004-2406-0"}],"volume":"35","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8e64e4b0c8380cd7f17b","contributors":{"authors":[{"text":"Gonzalez, F.I.","contributorId":68100,"corporation":false,"usgs":true,"family":"Gonzalez","given":"F.I.","email":"","affiliations":[],"preferred":false,"id":422982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titov, V.V.","contributorId":48752,"corporation":false,"usgs":true,"family":"Titov","given":"V.V.","email":"","affiliations":[],"preferred":false,"id":422980,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mofjeld, H.O.","contributorId":27103,"corporation":false,"usgs":true,"family":"Mofjeld","given":"H.O.","email":"","affiliations":[],"preferred":false,"id":422975,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Venturato, A.J.","contributorId":102265,"corporation":false,"usgs":true,"family":"Venturato","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":422985,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Simmons, R.S.","contributorId":97695,"corporation":false,"usgs":true,"family":"Simmons","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":422984,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hansen, R.","contributorId":56370,"corporation":false,"usgs":true,"family":"Hansen","given":"R.","affiliations":[],"preferred":false,"id":422981,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Combellick, Rodney","contributorId":106305,"corporation":false,"usgs":false,"family":"Combellick","given":"Rodney","email":"","affiliations":[],"preferred":false,"id":422987,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Eisner, R.K.","contributorId":103859,"corporation":false,"usgs":true,"family":"Eisner","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":422986,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hoirup, D.F.","contributorId":30811,"corporation":false,"usgs":true,"family":"Hoirup","given":"D.F.","affiliations":[],"preferred":false,"id":422976,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Yanagi, B.S.","contributorId":108312,"corporation":false,"usgs":true,"family":"Yanagi","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":422988,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Yong, S.","contributorId":34317,"corporation":false,"usgs":true,"family":"Yong","given":"S.","email":"","affiliations":[],"preferred":false,"id":422978,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Darienzo, M.","contributorId":41525,"corporation":false,"usgs":true,"family":"Darienzo","given":"M.","email":"","affiliations":[],"preferred":false,"id":422979,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Priest, G. R.","contributorId":19572,"corporation":false,"usgs":true,"family":"Priest","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":422974,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Crawford, G.L.","contributorId":75325,"corporation":false,"usgs":true,"family":"Crawford","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":422983,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Walsh, T. J.","contributorId":33725,"corporation":false,"usgs":true,"family":"Walsh","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422977,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}} ,{"id":70029502,"text":"70029502 - 2005 - Wildlife as valuable natural resources vs. intolerable pests: A suburban wildlife management model","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029502","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3669,"text":"Urban Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Wildlife as valuable natural resources vs. intolerable pests: A suburban wildlife management model","docAbstract":"Management of wildlife in suburban environments involves a complex set of interactions between both human and wildlife populations. Managers need additional tools, such as models, that can help them assess the status of wildlife populations, devise and apply management programs, and convey this information to other professionals and the public. We present a model that conceptualizes how some wildlife populations can fluctuate between extremely low (rare, threatened, or endangered status) and extremely high (overabundant) numbers over time. Changes in wildlife abundance can induce changes in human perceptions, which continually redefine species as a valuable resource to be protected versus a pest to be controlled. Management programs thatincorporate a number of approaches and promote more stable populations of wildlife avoid the problems of the resource versus pest transformation, are less costly to society, and encourage more positive and less negative interactions between humans and wildlife. We presenta case example of the beaver Castor canadensis in Massachusetts to illustrate how this model functions and can be applied. ?? 2005 Springer Science + Business Media, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Urban Ecosystems","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s11252-005-4379-5","issn":"10838155","usgsCitation":"DeStefano, S., and Deblinger, R., 2005, Wildlife as valuable natural resources vs. intolerable pests: A suburban wildlife management model: Urban Ecosystems, v. 8, no. 2 SPEC. ISS., p. 179-190, https://doi.org/10.1007/s11252-005-4379-5.","startPage":"179","endPage":"190","numberOfPages":"12","costCenters":[],"links":[{"id":237780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210760,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11252-005-4379-5"}],"volume":"8","issue":"2 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd0e4e4b08c986b32f10d","contributors":{"authors":[{"text":"DeStefano, S.","contributorId":84309,"corporation":false,"usgs":true,"family":"DeStefano","given":"S.","email":"","affiliations":[],"preferred":false,"id":423017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deblinger, R.D.","contributorId":8946,"corporation":false,"usgs":true,"family":"Deblinger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":423016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70027902,"text":"70027902 - 2005 - Multifractal magnetic susceptibility distribution models of hydrothermally altered rocks in the Needle Creek Igneous Center of the Absaroka Mountains, Wyoming","interactions":[],"lastModifiedDate":"2022-05-27T15:59:28.805108","indexId":"70027902","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2878,"text":"Nonlinear Processes in Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Multifractal magnetic susceptibility distribution models of hydrothermally altered rocks in the Needle Creek Igneous Center of the Absaroka Mountains, Wyoming","docAbstract":"Magnetic susceptibility was measured for 700 samples of drill core from thirteen drill holes in the porphyry copper-molybdenum deposit of the Stinkingwater mining district in the Absaroka Mountains, Wyoming. The magnetic susceptibility measurements, chemical analyses, and alteration class provided a database for study of magnetic susceptibility in these altered rocks. The distribution of the magnetic susceptibilities for all samples is multi-modal, with overlapping peaked distributions for samples in the propylitic and phyllic alteration class, a tail of higher susceptibilities for potassic alteration, and an approximately uniform distribution over a narrow range at the highest susceptibilities for unaltered rocks. Samples from all alteration and mineralization classes show susceptibilities across a wide range of values. Samples with secondary (supergene) alteration due to oxidation or enrichment show lower susceptibilities than primary (hypogene) alteration rock. Observed magnetic susceptibility variations and the monolithological character of the host rock suggest that the variations are due to varying degrees of alteration of blocks of rock between fractures that conducted hydrothermal fluids. Alteration of rock from the fractures inward progressively reduces the bulk magnetic susceptibility of the rock. The model introduced in this paper consists of a simulation of the fracture pattern and a simulation of the alteration of the rock between fractures. A multifractal model generated from multiplicative cascades with unequal ratios produces distributions statistically similar to the observed distributions. The reduction in susceptibility in the altered rocks was modelled as a diffusion process operating on the fracture distribution support. The average magnetic susceptibility was then computed for each block. For the purpose of comparing the model results with observation, the simulated magnetic susceptibilities were then averaged over the same interval as the measured data. Comparisons of the model and data from drillholes show good but not perfect agreement.
","language":"English","publisher":"Copernicus Publications","doi":"10.5194/npg-12-587-2005","usgsCitation":"Gettings, M.E., 2005, Multifractal magnetic susceptibility distribution models of hydrothermally altered rocks in the Needle Creek Igneous Center of the Absaroka Mountains, Wyoming: Nonlinear Processes in Geophysics, v. 12, no. 5, p. 587-601, https://doi.org/10.5194/npg-12-587-2005.","productDescription":"15 p.","startPage":"587","endPage":"601","numberOfPages":"15","costCenters":[],"links":[{"id":477934,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/npg-12-587-2005","text":"Publisher Index Page"},{"id":238150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Absaroka Mountains, Needle Creek Igneous Center","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.654541015625,\n 44.045154472558046\n ],\n [\n -109.42520141601561,\n 44.045154472558046\n ],\n [\n -109.42520141601561,\n 43.9\n ],\n [\n -109.654541015625,\n 43.9\n ],\n [\n -109.654541015625,\n 44.045154472558046\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"12","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-06-10","publicationStatus":"PW","scienceBaseUri":"505a6026e4b0c8380cd71311","contributors":{"authors":[{"text":"Gettings, Mark E. 0000-0002-2910-2321 mgetting@usgs.gov","orcid":"https://orcid.org/0000-0002-2910-2321","contributorId":602,"corporation":false,"usgs":true,"family":"Gettings","given":"Mark","email":"mgetting@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":415729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70029508,"text":"70029508 - 2005 - Loss estimates for a Puente Hills blind-thrust earthquake in Los Angeles, California","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70029508","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Loss estimates for a Puente Hills blind-thrust earthquake in Los Angeles, California","docAbstract":"Based on OpenSHA and HAZUS-MH, we present loss estimates for an earthquake rupture on the recently identified Puente Hills blind-thrust fault beneath Los Angeles. Given a range of possible magnitudes and ground motion models, and presuming a full fault rupture, we estimate the total economic loss to be between $82 and $252 billion. This range is not only considerably higher than a previous estimate of $69 billion, but also implies the event would be the costliest disaster in U.S. history. The analysis has also provided the following predictions: 3,000-18,000 fatalities, 142,000-735,000 displaced households, 42,000-211,000 in need of short-term public shelter, and 30,000-99,000 tons of debris generated. Finally, we show that the choice of ground motion model can be more influential than the earthquake magnitude, and that reducing this epistemic uncertainty (e.g., via model improvement and/or rejection) could reduce the uncertainty of the loss estimates by up to a factor of two. We note that a full Puente Hills fault rupture is a rare event (once every ???3,000 years), and that other seismic sources pose significant risk as well. ?? 2005, Earthquake Engineering Research Institute.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Spectra","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1193/1.1898332","issn":"87552930","usgsCitation":"Field, E.H., Seligson, H., Gupta, N., Gupta, V., Jordan, T., and Campbell, K., 2005, Loss estimates for a Puente Hills blind-thrust earthquake in Los Angeles, California: Earthquake Spectra, v. 21, no. 2, p. 329-338, https://doi.org/10.1193/1.1898332.","startPage":"329","endPage":"338","numberOfPages":"10","costCenters":[],"links":[{"id":210846,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1193/1.1898332"},{"id":237890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-01","publicationStatus":"PW","scienceBaseUri":"505a49d4e4b0c8380cd68901","contributors":{"authors":[{"text":"Field, E. H.","contributorId":86915,"corporation":false,"usgs":true,"family":"Field","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":423042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seligson, H.A.","contributorId":103860,"corporation":false,"usgs":true,"family":"Seligson","given":"H.A.","affiliations":[],"preferred":false,"id":423043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gupta, N.","contributorId":12252,"corporation":false,"usgs":false,"family":"Gupta","given":"N.","email":"","affiliations":[],"preferred":false,"id":423039,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gupta, V.","contributorId":10959,"corporation":false,"usgs":false,"family":"Gupta","given":"V.","email":"","affiliations":[],"preferred":false,"id":423038,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jordan, T.H.","contributorId":83320,"corporation":false,"usgs":true,"family":"Jordan","given":"T.H.","affiliations":[],"preferred":false,"id":423041,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Campbell, K.W.","contributorId":26309,"corporation":false,"usgs":true,"family":"Campbell","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":423040,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70029509,"text":"70029509 - 2005 - A modified beam-to-earth transformation to measure short-wavelength internal waves with an acoustic Doppler current profiler","interactions":[],"lastModifiedDate":"2017-08-15T17:37:50","indexId":"70029509","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2186,"text":"Journal of Atmospheric and Oceanic Technology","active":true,"publicationSubtype":{"id":10}},"title":"A modified beam-to-earth transformation to measure short-wavelength internal waves with an acoustic Doppler current profiler","docAbstract":"The algorithm used to transform velocity signals from beam coordinates to earth coordinates in an acoustic Doppler current profiler (ADCP) relies on the assumption that the currents are uniform over the horizontal distance separating the beams. This condition may be violated by (nonlinear) internal waves, which can have wavelengths as small as 100-200 m. In this case, the standard algorithm combines velocities measured at different phases of a wave and produces horizontal velocities that increasingly differ from true velocities with distance from the ADCP. Observations made in Massachusetts Bay show that currents measured with a bottom-mounted upward-looking ADCP during periods when short-wavelength internal waves are present differ significantly from currents measured by point current meters, except very close to the instrument. These periods are flagged with high error velocities by the standard ADCP algorithm. In this paper measurements from the four spatially diverging beams and the backscatter intensity signal are used to calculate the propagation direction and celerity of the internal waves. Once this information is known, a modified beam-to-earth transformation that combines appropriately lagged beam measurements can be used to obtain current estimates in earth coordinates that compare well with pointwise measurements. ?? 2005 American Meteorological Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Atmospheric and Oceanic Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1175/JTECH1731.1","issn":"07390572","usgsCitation":"Scotti, A., Butman, B., Beardsley, R., Alexander, P.S., and Anderson, S., 2005, A modified beam-to-earth transformation to measure short-wavelength internal waves with an acoustic Doppler current profiler: Journal of Atmospheric and Oceanic Technology, v. 22, no. 5, p. 583-591, https://doi.org/10.1175/JTECH1731.1.","startPage":"583","endPage":"591","numberOfPages":"9","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":477876,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/jtech1731.1","text":"Publisher Index Page"},{"id":237891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210847,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1175/JTECH1731.1"}],"volume":"22","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-01","publicationStatus":"PW","scienceBaseUri":"5059e485e4b0c8380cd466ae","contributors":{"authors":[{"text":"Scotti, A.","contributorId":67270,"corporation":false,"usgs":true,"family":"Scotti","given":"A.","email":"","affiliations":[],"preferred":false,"id":423045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butman, B.","contributorId":85580,"corporation":false,"usgs":true,"family":"Butman","given":"B.","email":"","affiliations":[],"preferred":false,"id":423046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beardsley, R.C.","contributorId":106508,"corporation":false,"usgs":true,"family":"Beardsley","given":"R.C.","affiliations":[],"preferred":false,"id":423048,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Alexander, P. S.","contributorId":88012,"corporation":false,"usgs":true,"family":"Alexander","given":"P.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":423047,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Anderson, S.","contributorId":45779,"corporation":false,"usgs":true,"family":"Anderson","given":"S.","affiliations":[],"preferred":false,"id":423044,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70027816,"text":"70027816 - 2005 - Digital elevation model of King Edward VII Peninsula, West Antarctica, from SAR interferometry and ICESat laser altimetry","interactions":[],"lastModifiedDate":"2017-01-18T13:58:26","indexId":"70027816","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1940,"text":"IEEE Geoscience and Remote Sensing Letters","active":true,"publicationSubtype":{"id":10}},"title":"Digital elevation model of King Edward VII Peninsula, West Antarctica, from SAR interferometry and ICESat laser altimetry","docAbstract":"We present a digital elevation model (DEM) of King Edward VII Peninsula, Sulzberger Bay, West Antarctica, developed using 12 European Remote Sensing (ERS) synthetic aperture radar (SAR) scenes and 24 Ice, Cloud, and land Elevation Satellite (ICESat) laser altimetry profiles. We employ differential interferograms from the ERS tandem mission SAR scenes acquired in the austral fall of 1996, and four selected ICESat laser altimetry profiles acquired in the austral fall of 2004, as ground control points (GCPs) to construct an improved geocentric 60-m resolution DEM over the grounded ice region. We then extend the DEM to include two ice shelves using ICESat profiles via Kriging. Twenty additional ICESat profiles acquired in 2003-2004 are used to assess the accuracy of the DEM. After accounting for radar penetration depth and predicted surface changes, including effects due to ice mass balance, solid Earth tides, and glacial isostatic adjustment, in part to account for the eight-year data acquisition discrepancy, the resulting difference between the DEM and ICESat profiles is -0.57 ?? 5.88 m. After removing the discrepancy between the DEM and ICESat profiles for a final combined DEM using a bicubic spline, the overall difference is 0.05 ?? 1.35 m. ?? 2005 IEEE.
","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"IEEE Geoscience and Remote Sensing Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1109/LGRS.2005.853623","issn":"1545598X","usgsCitation":"Baek, S., Kwoun, O., Braun, A., Lu, Z., and Shum, C., 2005, Digital elevation model of King Edward VII Peninsula, West Antarctica, from SAR interferometry and ICESat laser altimetry: IEEE Geoscience and Remote Sensing Letters, v. 2, no. 4, p. 413-417, https://doi.org/10.1109/LGRS.2005.853623.","startPage":"413","endPage":"417","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":238358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211149,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1109/LGRS.2005.853623"}],"otherGeospatial":"King Edward VII Peninsula, Antarctica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -209.53125,\n -79.23718500609334\n ],\n [\n -209.53125,\n -66.65297740055277\n ],\n [\n -98.61328125,\n -66.65297740055277\n ],\n [\n -98.61328125,\n -79.23718500609334\n ],\n [\n -209.53125,\n -79.23718500609334\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a014ee4b0c8380cd4fb76","contributors":{"authors":[{"text":"Baek, S.","contributorId":39557,"corporation":false,"usgs":true,"family":"Baek","given":"S.","email":"","affiliations":[],"preferred":false,"id":415344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kwoun, Oh-Ig","contributorId":41945,"corporation":false,"usgs":true,"family":"Kwoun","given":"Oh-Ig","email":"","affiliations":[],"preferred":false,"id":415345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Braun, Andreas","contributorId":80877,"corporation":false,"usgs":true,"family":"Braun","given":"Andreas","email":"","affiliations":[],"preferred":false,"id":415346,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lu, Z.","contributorId":106241,"corporation":false,"usgs":true,"family":"Lu","given":"Z.","affiliations":[],"preferred":false,"id":415348,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shum, C. K.","contributorId":85373,"corporation":false,"usgs":true,"family":"Shum","given":"C. K.","affiliations":[],"preferred":false,"id":415347,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70027411,"text":"70027411 - 2005 - Numerical simulation of saltwater intrusion in response to sea-level rise","interactions":[],"lastModifiedDate":"2012-03-12T17:21:15","indexId":"70027411","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Numerical simulation of saltwater intrusion in response to sea-level rise","docAbstract":"A two dimensional numerical model of variable-density groundwater flow and dispersive solute transport was used to predict the extent, rate, and lag time of saltwater intrusion in response to various sea-level rise scenarios. Three simulations were performed with varying rates of sea-level rise. For the first simulation, sea-level rise was specified at a rate of 0.9 mm/yr, which is the slowest rate of sea-level rise estimated by the Intergovernmental Panel on Climate Change (IPCC). After 100 years, the 250 mg/L chloride isochlor moved inland by about 40 m, and required an additional 8 years for the system to reach equilibrium. For the next simulation, sea-level rise was specified at 4.8 mm/yr, which is the central value of the IPCC estimate. For this moderate rate of sea-level rise, the 250 mg/L isochlor moved inland by about 740 m after 100 years, and required an additional 10 years for the system to reach equilibrium. For the fastest rate of sea level rise estimated by IPCC (8.8 mm/yr), the 250 mg/L isochlor moved inland by about 1800 m after 100 years, and required more than 50 years to reach equilibrium. Copyright ASCE 2005.","largerWorkTitle":"World Water Congress 2005: Impacts of Global Climate Change - Proceedings of the 2005 World Water and Environmental Resources Congress","conferenceTitle":"2005 World Water and Environmental Resources Congress","conferenceDate":"15 May 2005 through 19 May 2005","conferenceLocation":"Anchorage, AK","language":"English","doi":"10.1061/40792(173)376","isbn":"0784407924; 9780784407929","usgsCitation":"Langevin, C., and Dausman, A., 2005, Numerical simulation of saltwater intrusion in response to sea-level rise, in World Water Congress 2005: Impacts of Global Climate Change - Proceedings of the 2005 World Water and Environmental Resources Congress, Anchorage, AK, 15 May 2005 through 19 May 2005, https://doi.org/10.1061/40792(173)376.","startPage":"376","costCenters":[],"links":[{"id":211159,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/40792(173)376"},{"id":238369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2012-04-26","publicationStatus":"PW","scienceBaseUri":"505a6927e4b0c8380cd73bb8","contributors":{"authors":[{"text":"Langevin, C.D.","contributorId":25976,"corporation":false,"usgs":true,"family":"Langevin","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":413540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dausman, A.M.","contributorId":99373,"corporation":false,"usgs":true,"family":"Dausman","given":"A.M.","affiliations":[],"preferred":false,"id":413541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70027409,"text":"70027409 - 2005 - Calibration of numerical models for small debris flows in Yosemite Valley, California, USA","interactions":[],"lastModifiedDate":"2013-02-21T20:44:43","indexId":"70027409","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2824,"text":"Natural Hazards and Earth System Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Calibration of numerical models for small debris flows in Yosemite Valley, California, USA","docAbstract":"This study compares documented debris flow runout distances with numerical simulations in the Yosemite Valley of California, USA, where about 15% of historical events of slope instability can be classified as debris flows and debris slides (Wieczorek and Snyder, 2004). To model debris flows in the Yosemite Valley, we selected six streams with evidence of historical debris flows; three of the debris flow deposits have single channels, and the other three split their pattern in the fan area into two or more channels. From field observations all of the debris flows involved coarse material, with only very small clay content. We applied the one dimensional DAN (Dynamic ANalysis) model (Hungr, 1995) and the two-dimensional FLO2D model (O'Brien et al., 1993) to predict and compare the runout distance and the velocity of the debris flows observed in the study area. As a first step, we calibrated the parameters for the two softwares through the back analysis of three debris- flows channels using a trial-and-error procedure starting with values suggested in the literature. In the second step we applied the selected values to the other channels, in order to evaluate their predictive capabilities. After parameter calibration using three debris flows we obtained results similar to field observations We also obtained a good agreement between the two models for velocities. Both models are strongly influenced by topography: we used the 30 m cell size DTM available for the study area, that is probably not accurate enough for a highly detailed analysis, but it can be sufficient for a first screening. European Geosciences Union ?? 2005 Author(s). This work is licensed under a Creative Commons License.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Natural Hazards and Earth System Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"European Geosciences Union","doi":"10.5194/nhess-5-993-2005","issn":"15618633","usgsCitation":"Bertolo, P., and Wieczorek, G.F., 2005, Calibration of numerical models for small debris flows in Yosemite Valley, California, USA: Natural Hazards and Earth System Sciences, v. 5, no. 6, p. 993-1001, https://doi.org/10.5194/nhess-5-993-2005.","startPage":"993","endPage":"1001","numberOfPages":"9","costCenters":[],"links":[{"id":477793,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5194/nhess-5-993-2005","text":"Publisher Index Page"},{"id":238330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267919,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.5194/nhess-5-993-2005"}],"volume":"5","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-12-13","publicationStatus":"PW","scienceBaseUri":"5059f317e4b0c8380cd4b5c4","contributors":{"authors":[{"text":"Bertolo, P.","contributorId":20539,"corporation":false,"usgs":true,"family":"Bertolo","given":"P.","email":"","affiliations":[],"preferred":false,"id":413535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wieczorek, G. F.","contributorId":50143,"corporation":false,"usgs":true,"family":"Wieczorek","given":"G.","middleInitial":"F.","affiliations":[],"preferred":false,"id":413536,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70027660,"text":"70027660 - 2005 - Modeling and measuring the nocturnal drainage flow in a high-elevation, subalpine forest with complex terrain","interactions":[],"lastModifiedDate":"2018-10-31T08:26:22","indexId":"70027660","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2316,"text":"Journal of Geophysical Research D: Atmospheres","active":true,"publicationSubtype":{"id":10}},"title":"Modeling and measuring the nocturnal drainage flow in a high-elevation, subalpine forest with complex terrain","docAbstract":"The nocturnal drainage flow of air causes significant uncertainty in ecosystem CO2, H2O, and energy budgets determined with the eddy covariance measurement approach. In this study, we examined the magnitude, nature, and dynamics of the nocturnal drainage flow in a subalpine forest ecosystem with complex terrain. We used an experimental approach involving four towers, each with vertical profiling of wind speed to measure the magnitude of drainage flows and dynamics in their occurrence. We developed an analytical drainage flow model, constrained with measurements of canopy structure and SF6 diffusion, to help us interpret the tower profile results. Model predictions were in good agreement with observed profiles of wind speed, leaf area density, and wind drag coefficient. Using theory, we showed that this one‐dimensional model is reduced to the widely used exponential wind profile model under conditions where vertical leaf area density and drag coefficient are uniformly distributed. We used the model for stability analysis, which predicted the presence of a very stable layer near the height of maximum leaf area density. This stable layer acts as a flow impediment, minimizing vertical dispersion between the subcanopy air space and the atmosphere above the canopy. The prediction is consistent with the results of SF6 diffusion observations that showed minimal vertical dispersion of nighttime, subcanopy drainage flows. The stable within‐canopy air layer coincided with the height of maximum wake‐to‐shear production ratio. We concluded that nighttime drainage flows are restricted to a relatively shallow layer of air beneath the canopy, with little vertical mixing across a relatively long horizontal fetch. Insight into the horizontal and vertical structure of the drainage flow is crucial for understanding the magnitude and dynamics of the mean advective CO2 flux that becomes significant during stable nighttime conditions and are typically missed during measurement of the turbulent CO2 flux. The model and interpretation provided in this study should lead to research strategies for the measurement of these advective fluxes and their inclusion in the overall mass balance for CO2 at this site with complex terrain.
","language":"English","publisher":"AGU","doi":"10.1029/2005JD006282","issn":"01480227","usgsCitation":"Yi, C., Monson, R.K., Zhai, Z., Anderson, D., Lamb, B., Allwine, G., Turnipseed, A., and Burns, S.P., 2005, Modeling and measuring the nocturnal drainage flow in a high-elevation, subalpine forest with complex terrain: Journal of Geophysical Research D: Atmospheres, v. 110, no. 22, p. 1-13, https://doi.org/10.1029/2005JD006282.","productDescription":"13 p.","startPage":"1","endPage":"13","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477854,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jd006282","text":"Publisher Index Page"},{"id":238274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211091,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JD006282"}],"volume":"110","issue":"22","noUsgsAuthors":false,"publicationDate":"2005-11-16","publicationStatus":"PW","scienceBaseUri":"505a5bd7e4b0c8380cd6f842","contributors":{"authors":[{"text":"Yi, C.","contributorId":62039,"corporation":false,"usgs":true,"family":"Yi","given":"C.","email":"","affiliations":[],"preferred":false,"id":414613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Monson, Russell K.","contributorId":48136,"corporation":false,"usgs":true,"family":"Monson","given":"Russell","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":414611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zhai, Z.","contributorId":24189,"corporation":false,"usgs":true,"family":"Zhai","given":"Z.","email":"","affiliations":[],"preferred":false,"id":414609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Anderson, D.E.","contributorId":47320,"corporation":false,"usgs":true,"family":"Anderson","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":414610,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lamb, B.","contributorId":17058,"corporation":false,"usgs":true,"family":"Lamb","given":"B.","affiliations":[],"preferred":false,"id":414607,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Allwine, G.","contributorId":52462,"corporation":false,"usgs":true,"family":"Allwine","given":"G.","email":"","affiliations":[],"preferred":false,"id":414612,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Turnipseed, A.A.","contributorId":23726,"corporation":false,"usgs":true,"family":"Turnipseed","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":414608,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Burns, Sean P.","contributorId":98921,"corporation":false,"usgs":true,"family":"Burns","given":"Sean","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":414614,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70027658,"text":"70027658 - 2005 - A legacy of change: The lower Colorado River, Arizona-California-Nevada, USA, and Sonora-Baja California Norte, Mexico","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70027658","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"A legacy of change: The lower Colorado River, Arizona-California-Nevada, USA, and Sonora-Baja California Norte, Mexico","docAbstract":"The lower Colorado is among the most regulated rivers in the world. It ranks as the fifth largest river in volume in the coterminous United States, but its flow is fully allocated and no longer reaches the sea. Lower basin reservoirs flood nearly one third of the river channel and store 2 years of annual flow. Diverted water irrigates 1.5 million ha of cropland and provides water for industry and domestic use by 22 million people in the southwestern United States and northern Mexico. The native fish community of the lower Colorado River was among the most unique in the world, and the main stem was home to nine freshwater species, all of which were endemic to the basin. Today, five are extirpated, seven are federally endangered, and three are being reintroduced through stocking. Decline of the native fauna is attributed to predation by nonnative fishes and physical habitat degradation. Nearly 80 alien species have been introduced, and more than 20 now are common. These nonnative species thrived in modified habitats, where they largely eliminated the native kinds. As a result, the lower Colorado River has the dubious distinction of being among the few major rivers of the world with an entirely introduced fish fauna. ?? 2005 by the American Fisheries Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08922284","usgsCitation":"Mueller, G., Marsh, P., and Minckley, W., 2005, A legacy of change: The lower Colorado River, Arizona-California-Nevada, USA, and Sonora-Baja California Norte, Mexico: American Fisheries Society Symposium, v. 2005, no. 45, p. 139-156.","startPage":"139","endPage":"156","numberOfPages":"18","costCenters":[],"links":[{"id":238238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2005","issue":"45","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e436e4b0c8380cd464e1","contributors":{"authors":[{"text":"Mueller, G.A.","contributorId":9205,"corporation":false,"usgs":true,"family":"Mueller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":414601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marsh, P.C.","contributorId":74710,"corporation":false,"usgs":true,"family":"Marsh","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":414603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Minckley, W.L.","contributorId":13925,"corporation":false,"usgs":true,"family":"Minckley","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":414602,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70027869,"text":"70027869 - 2005 - Ontogenetic behavior and dispersal of Sacramento River white sturgeon, Acipenser transmontanus, with a note on body color","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027869","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1528,"text":"Environmental Biology of Fishes","active":true,"publicationSubtype":{"id":10}},"title":"Ontogenetic behavior and dispersal of Sacramento River white sturgeon, Acipenser transmontanus, with a note on body color","docAbstract":"We studied Sacramento River white sturgeon, Acipenser transmontanus, in the laboratory to develop a conceptual model of ontogenetic behavior and provide insight into probable behavior of wild sturgeon. After hatching, free embryos initiated a low intensity, brief downstream dispersal during which fish swam near the bottom and were photonegative. The weak, short dispersal style and behavior of white sturgeon free embryos contrasts greatly with the intense, long dispersal style and behavior (photopositive and swimming far above the bottom) of dispersing free embryos of other sturgeon species. If spawned eggs are concentrated within a few kilometers downstream of a spawning site, the adaptive significance of the free embryo dispersal is likely to move fish away from the egg deposition site to avoid predation and reduce fish density prior to feeding. Larvae foraged on the open bottom, swam <1 m above the bottom, aggregated, but did not disperse. Early juveniles initiated a strong dispersal with fish strongly vigorously swimming downstream. Duration of the juvenile dispersal is unknown, but the strong swimming likely disperses fish many kilometers. Recruitment failure in white sturgeon populations may be a mis-match between the innate fish dispersal and post-dispersal rearing habitat, which is now highly altered by damming and reservoirs. Sacramento River white sturgeon has a two-step downstream dispersal by the free embryo and juvenile life intervals. Diel activity of all life intervals peaked at night, whether fish were dispersing or foraging. Nocturnal behavior is likely a response to predation, which occurs during both activities. An intense black-tail body color was present on foraging larvae, but was weak or absent on the two life intervals that disperse. Black-tail color may be an adaptation for avoiding predation, signaling among aggregated larvae, or both, but not for dispersal. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Biology of Fishes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10641-005-2198-4","issn":"03781909","usgsCitation":"Kynard, B., and Parker, E., 2005, Ontogenetic behavior and dispersal of Sacramento River white sturgeon, Acipenser transmontanus, with a note on body color: Environmental Biology of Fishes, v. 74, no. 1, p. 19-30, https://doi.org/10.1007/s10641-005-2198-4.","startPage":"19","endPage":"30","numberOfPages":"12","costCenters":[],"links":[{"id":211014,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10641-005-2198-4"},{"id":238149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6e4ee4b0c8380cd755a1","contributors":{"authors":[{"text":"Kynard, B.","contributorId":51232,"corporation":false,"usgs":true,"family":"Kynard","given":"B.","email":"","affiliations":[],"preferred":false,"id":415614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, E.","contributorId":101429,"corporation":false,"usgs":true,"family":"Parker","given":"E.","email":"","affiliations":[],"preferred":false,"id":415615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70027335,"text":"70027335 - 2005 - Application of acoustic doppler current profilers for measuring three-dimensional flow fields and as a surrogate measurement of bedload transport","interactions":[],"lastModifiedDate":"2018-04-21T13:45:40","indexId":"70027335","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Application of acoustic doppler current profilers for measuring three-dimensional flow fields and as a surrogate measurement of bedload transport","docAbstract":"Acoustic Doppler current profilers (ADCPs) have been in use in the riverine environment for nearly 20 years. Their application primarily has been focused on the measurement of streamflow discharge. ADCPs emit high-frequency sound pulses and receive reflected sound echoes from sediment particles in the water column. The Doppler shift between transmitted and return signals is resolved into a velocity component that is measured in three dimensions by simultaneously transmitting four independent acoustical pulses. To measure the absolute velocity magnitude and direction in the water column, the velocity magnitude and direction of the instrument must also be computed. Typically this is accomplished by ensonifying the streambed with an acoustical pulse that also provides a depth measurement for each of the four acoustic beams. Sediment transport on or near the streambed will bias these measurements and requires external positioning such as a differentially corrected Global Positioning Systems (GPS). Although the influence of hydraulic structures such as spur dikes and bridge piers is typically only measured and described in one or two dimensions, the use of differentially corrected GPS with ADCPs provides a fully three-dimensional measurement of the magnitude and direction of the water column at such structures. The measurement of these flow disturbances in a field setting also captures the natural pulsations of river flow that cannot be easily quantified or modeled by numerical simulations or flumes. Several examples of measured three-dimensional flow conditions at bridge sites throughout Alaska are presented. The bias introduced to the bottom-track measurement is being investigated as a surrogate measurement of bedload transport. By fixing the position of the ADCP for a known period of time the apparent velocity of the streambed at that position can be determined. Initial results and comparison to traditionally measured bedload values are presented. These initial results and those by other researchers are helping to determine a direction for further research of noncontact measurements of sediment transport. Copyright ASCE 2005.","largerWorkTitle":"World Water Congress 2005: Impacts of Global Climate Change - Proceedings of the 2005 World Water and Environmental Resources Congress","conferenceTitle":"2005 World Water and Environmental Resources Congress","conferenceDate":"15 May 2005 through 19 May 2005","conferenceLocation":"Anchorage, AK","language":"English","doi":"10.1061/40792(173)391","isbn":"0784407924; 9780784407929","usgsCitation":"Conaway, J.S., 2005, Application of acoustic doppler current profilers for measuring three-dimensional flow fields and as a surrogate measurement of bedload transport, in World Water Congress 2005: Impacts of Global Climate Change - Proceedings of the 2005 World Water and Environmental Resources Congress, Anchorage, AK, 15 May 2005 through 19 May 2005, https://doi.org/10.1061/40792(173)391.","startPage":"391","costCenters":[],"links":[{"id":235529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209253,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/40792(173)391"}],"noUsgsAuthors":false,"publicationDate":"2012-04-26","publicationStatus":"PW","scienceBaseUri":"5059ec94e4b0c8380cd49362","contributors":{"authors":[{"text":"Conaway, Jeffrey S. 0000-0002-3036-592X jconaway@usgs.gov","orcid":"https://orcid.org/0000-0002-3036-592X","contributorId":2026,"corporation":false,"usgs":true,"family":"Conaway","given":"Jeffrey","email":"jconaway@usgs.gov","middleInitial":"S.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true}],"preferred":true,"id":413218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70027657,"text":"70027657 - 2005 - Coastal foredune displacement and recovery, Barrett Beach-Talisman, Fire Island, New York, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027657","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3804,"text":"Zeitschrift fur Geomorphologie, Supplementband","active":true,"publicationSubtype":{"id":10}},"title":"Coastal foredune displacement and recovery, Barrett Beach-Talisman, Fire Island, New York, USA","docAbstract":"Coastal foredune mobility has been tracked at Fire Island National Seashore since 1976 with annual field surveys and analysis of frequent aerial photography. Sequential mapping of the foredune crestline depicts nearly islandwide displacement during major storm events, such as in 1992, and localized displacement during alongshore passage of inshore circulation cells during other years. An instance of localized landward erosion and curvilinear displacement along approximately 400 m of foredune occurred in 1994, followed by recovery over the next nine years. Data from annual surveys and partially supported by four LIDAR flights establish that volume recovery rates in the foredune ranged from about 1.0 m3/m/yr to nearly 12.0 m 3/m/yr. Analysis of the foredune morphology and location shows nearly complete recovery of foredune shape and dimension during this interval and it also demonstrates that there has been inland displacement of the foredune crestline of up to 40 m. Total volume recovery within the localized foredune erosion site was greatest, between 34 m3/m to 47 m3/m, in areas of greatest displacement and eventually contributed to creation of a foredune of similar dimension along the entire eroded zone. This process of erosion and recovery describes a mechanism for foredune dimension retention during episodic erosion and displacement and may be a model for foredune persistence accompanying barrier island migration. ?? 2005 Gebru??der Borntraeger.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Zeitschrift fur Geomorphologie, Supplementband","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00442798","usgsCitation":"Psuty, N., Pace, J., and Allen, J., 2005, Coastal foredune displacement and recovery, Barrett Beach-Talisman, Fire Island, New York, USA: Zeitschrift fur Geomorphologie, Supplementband, v. 141, p. 153-168.","startPage":"153","endPage":"168","numberOfPages":"16","costCenters":[],"links":[{"id":238204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f782e4b0c8380cd4cb5d","contributors":{"authors":[{"text":"Psuty, N.P.","contributorId":58742,"corporation":false,"usgs":true,"family":"Psuty","given":"N.P.","affiliations":[],"preferred":false,"id":414600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pace, J.P.","contributorId":18883,"corporation":false,"usgs":true,"family":"Pace","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":414599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, J.R.","contributorId":16955,"corporation":false,"usgs":true,"family":"Allen","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":414598,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":72472,"text":"sir20055123 - 2005 - Evaluation of models and data for assessing whooping crane habitat in the central Platte River, Nebraska","interactions":[],"lastModifiedDate":"2016-05-27T13:41:53","indexId":"sir20055123","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5123","title":"Evaluation of models and data for assessing whooping crane habitat in the central Platte River, Nebraska","docAbstract":"The primary objectives of this evaluation were to improve the performance of the Whooping Crane Habitat Suitability model (C4R) used by the U.S. Fish and Wildlife Service (Service) for defining the relationship between river discharge and habitat availability, and to assist the Service in implementing improved model(s) with existing hydraulic files. The C4R habitat model is applied at the scale of individual river cross-sections, but the model outputs are scaledup to larger reaches of the river using a decision support “model” comprised of other data and procedures. Hence, the validity of the habitat model depends at least partially on how its outputs are incorporated into this larger context. For that reason, we also evaluated other procedures including the PHABSIM data files, the FORTRAN computer programs used to implement the model, and other parameters used to simulate the relationship between river flows and the availability of Whooping Crane roosting habitat along more than 100 miles of heterogeneous river channels. An equally important objective of this report was to fully document these related procedures as well as the model and evaluation results so that interested parties could readily understand the technical basis for the Service’s recommendations.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055123","usgsCitation":"Farmer, A.H., Cade, B.S., Terrell, J.W., Henriksen, J.H., and Runge, J.T., 2005, Evaluation of models and data for assessing whooping crane habitat in the central Platte River, Nebraska: U.S. Geological Survey Scientific Investigations Report 2005-5123, ix, 64 p., https://doi.org/10.3133/sir20055123.","productDescription":"ix, 64 p.","numberOfPages":"77","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":191083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055123.PNG"},{"id":320250,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Platte River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624bfc","contributors":{"authors":[{"text":"Farmer, Adrian H.","contributorId":107759,"corporation":false,"usgs":true,"family":"Farmer","given":"Adrian","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cade, Brian S. 0000-0001-9623-9849 cadeb@usgs.gov","orcid":"https://orcid.org/0000-0001-9623-9849","contributorId":1278,"corporation":false,"usgs":true,"family":"Cade","given":"Brian","email":"cadeb@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":285711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Terrell, James W. 0000-0001-5394-5663","orcid":"https://orcid.org/0000-0001-5394-5663","contributorId":92726,"corporation":false,"usgs":true,"family":"Terrell","given":"James","email":"","middleInitial":"W.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":285714,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henriksen, Jim H.","contributorId":54684,"corporation":false,"usgs":true,"family":"Henriksen","given":"Jim","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285712,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Runge, Jeffery T.","contributorId":66356,"corporation":false,"usgs":true,"family":"Runge","given":"Jeffery","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":285713,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70027576,"text":"70027576 - 2005 - A multivariate study of mangrove morphology (Rhizophora mangle) using both above and below-water plant architecture","interactions":[],"lastModifiedDate":"2012-03-12T17:20:48","indexId":"70027576","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1587,"text":"Estuarine, Coastal and Shelf Science","active":true,"publicationSubtype":{"id":10}},"title":"A multivariate study of mangrove morphology (Rhizophora mangle) using both above and below-water plant architecture","docAbstract":"A descriptive study of the architecture of the red mangrove, Rhizophora mangle L., habitat of Tampa Bay, FL, was conducted to assess if plant architecture could be used to discriminate overwash from fringing forest type. Seven above-water (e.g., tree height, diameter at breast height, and leaf area) and 10 below-water (e.g., root density, root complexity, and maximum root order) architectural features were measured in eight mangrove stands. A multivariate technique (discriminant analysis) was used to test the ability of different models comprising above-water, below-water, or whole tree architecture to classify forest type. Root architectural features appear to be better than classical forestry measurements at discriminating between fringing and overwash forests but, regardless of the features loaded into the model, misclassification rates were high as forest type was only correctly classified in 66% of the cases. Based upon habitat architecture, the results of this study do not support a sharp distinction between overwash and fringing red mangrove forests in Tampa Bay but rather indicate that the two are architecturally undistinguishable. Therefore, within this northern portion of the geographic range of red mangroves, a more appropriate classification system based upon architecture may be one in which overwash and fringing forest types are combined into a single, \"tide dominated\" category. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Estuarine, Coastal and Shelf Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.ecss.2005.06.019","issn":"02727714","usgsCitation":"Brooks, R.A., and Bell, S., 2005, A multivariate study of mangrove morphology (Rhizophora mangle) using both above and below-water plant architecture: Estuarine, Coastal and Shelf Science, v. 65, no. 3, p. 440-448, https://doi.org/10.1016/j.ecss.2005.06.019.","startPage":"440","endPage":"448","numberOfPages":"9","costCenters":[],"links":[{"id":210933,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ecss.2005.06.019"},{"id":238021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e491e4b0c8380cd4672a","contributors":{"authors":[{"text":"Brooks, R. A.","contributorId":53803,"corporation":false,"usgs":true,"family":"Brooks","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":414211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, S.S.","contributorId":48754,"corporation":false,"usgs":true,"family":"Bell","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":414210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70027654,"text":"70027654 - 2005 - Conceptualization and simulation of the Edwards aquifer, San Antonio region, Texas","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027654","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Conceptualization and simulation of the Edwards aquifer, San Antonio region, Texas","docAbstract":"Numerical ground-water flow models for the Edwards aquifer in the San Antonio region of Texas generally have been based on a diffuse-flow conceptualization. That is, although conduits likely are present, the assumption is that flow in the aquifer predominantly is through a network of small fractures and openings sufficiently numerous that the aquifer can be considered a porous-media continuum at the regional scale. Whether flow through large fractures and conduits or diffuse flow predominates in the Edwards aquifer at the regional scale is an open question. A new numerical ground-water-flow model (Edwards aquifer model) that incorporates important components of the latest information and an alternate conceptualization of the Edwards aquifer was developed. The conceptualization upon which the Edwards aquifer model is based emphasizes conduit development and conduit flow, and the model can be considered a test of one of two reasonable conceptualizations. The model incorporates conduits simulated as generally continuously connected, one-cell-wide (1,320 feet) zones with very large hydraulic-conductivity values (as much as 300,000 feet per day). The locations of the conduits are based on a number of factors, including major potentiometric-surface troughs in the aquifer, the presence of sinking streams, geochemical information, and geologic structures (for example, faults and grabens). The model includes both the San Antonio and Barton Springs segments of the Edwards aquifer in the San Antonio region, Texas, and was calibrated for steady-state (1939-46) and transient (1947-2000) conditions. Transient simulations were conducted using monthly recharge and pumpage (withdrawals) data. The predominantly conduit-flow conceptualization incorporated in the Edwards aquifer model yielded a reasonably good match between measured and simulated hydraulic heads in the confined part of the aquifer and between measured and simulated springflows. The simulated directions of flow in the Edwards aquifer model are most strongly influenced by the presence of simulated conduits and barrier faults. The simulated flow in the Edwards aquifer is appreciably influenced by the locations of the simulated conduits, which tend to facilitate flow. The simulated subregional flow directions generally are toward the nearest conduit and subsequently along the conduits from the recharge zone into the confined zone and toward the major springs. Structures simulated in the Edwards aquifer model that tend to restrict ground-water flow are barrier faults. The influence of simulated barrier faults on flow directions is most evident in northern Medina County.","largerWorkTitle":"Geotechnical Special Publication","conferenceTitle":"10th Multidisciplinary Conference - Sinkholes and the Engineering and Environmental Impacts of Karst","conferenceDate":"24 September 2005 through 28 September 2005","conferenceLocation":"San Antonio, TX","language":"English","issn":"08950563","usgsCitation":"Lindgren, K., Dutton, A., Hovorka, S., Worthington, S., and Painter, S., 2005, Conceptualization and simulation of the Edwards aquifer, San Antonio region, Texas, in Geotechnical Special Publication, no. 144, San Antonio, TX, 24 September 2005 through 28 September 2005, p. 122-130.","startPage":"122","endPage":"130","numberOfPages":"9","costCenters":[],"links":[{"id":238171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"144","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f9ade4b0c8380cd4d70e","contributors":{"editors":[{"text":"Beck B.F.","contributorId":128361,"corporation":true,"usgs":false,"organization":"Beck B.F.","id":536626,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Lindgren, K.J.","contributorId":68958,"corporation":false,"usgs":true,"family":"Lindgren","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":414587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutton, A.R.","contributorId":93976,"corporation":false,"usgs":true,"family":"Dutton","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":414589,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hovorka, S.D.","contributorId":71259,"corporation":false,"usgs":true,"family":"Hovorka","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":414588,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Worthington, S.R.H.","contributorId":55522,"corporation":false,"usgs":true,"family":"Worthington","given":"S.R.H.","email":"","affiliations":[],"preferred":false,"id":414586,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Painter, S.","contributorId":28799,"corporation":false,"usgs":true,"family":"Painter","given":"S.","affiliations":[],"preferred":false,"id":414585,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70027636,"text":"70027636 - 2005 - Phosphorus component in AnnAGNPS","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70027636","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3626,"text":"Transactions of the American Society of Agricultural Engineers","active":true,"publicationSubtype":{"id":10}},"title":"Phosphorus component in AnnAGNPS","docAbstract":"The USDA Annualized Agricultural Non-Point Source Pollution model (AnnAGNPS) has been developed to aid in evaluation of watershed response to agricultural management practices. Previous studies have demonstrated the capability of the model to simulate runoff and sediment, but not phosphorus (P). The main purpose of this article is to evaluate the performance of AnnAGNPS on P simulation using comparisons with measurements from the Deep Hollow watershed of the Mississippi Delta Management Systems Evaluation Area (MDMSEA) project. A sensitivity analysis was performed to identify input parameters whose impact is the greatest on P yields. Sensitivity analysis results indicate that the most sensitive variables of those selected are initial soil P contents, P application rate, and plant P uptake. AnnAGNPS simulations of dissolved P yield do not agree well with observed dissolved P yield (Nash-Sutcliffe coefficient of efficiency of 0.34, R2 of 0.51, and slope of 0.24); however, AnnAGNPS simulations of total P yield agree well with observed total P yield (Nash-Sutcliffe coefficient of efficiency of 0.85, R2 of 0.88, and slope of 0.83). The difference in dissolved P yield may be attributed to limitations in model simulation of P processes. Uncertainties in input parameter selections also affect the model's performance.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Society of Agricultural Engineers","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00012351","usgsCitation":"Yuan, Y., Bingner, R., Theurer, F., Rebich, R., and Moore, P., 2005, Phosphorus component in AnnAGNPS: Transactions of the American Society of Agricultural Engineers, v. 48, no. 6, p. 2145-2154.","startPage":"2145","endPage":"2154","numberOfPages":"10","costCenters":[],"links":[{"id":238458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a78b5e4b0c8380cd7876d","contributors":{"authors":[{"text":"Yuan, Y.","contributorId":90893,"corporation":false,"usgs":true,"family":"Yuan","given":"Y.","email":"","affiliations":[],"preferred":false,"id":414507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingner, R.L.","contributorId":21346,"corporation":false,"usgs":true,"family":"Bingner","given":"R.L.","affiliations":[],"preferred":false,"id":414504,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Theurer, F.D.","contributorId":86166,"corporation":false,"usgs":true,"family":"Theurer","given":"F.D.","affiliations":[],"preferred":false,"id":414506,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rebich, R.A.","contributorId":20788,"corporation":false,"usgs":true,"family":"Rebich","given":"R.A.","affiliations":[],"preferred":false,"id":414503,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moore, P.A.","contributorId":58835,"corporation":false,"usgs":true,"family":"Moore","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":414505,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70027854,"text":"70027854 - 2005 - Microsatellite DNA markers for delineating population structure and kinship among the endangered Kirtland's warbler (Dendroica kirtlandii)","interactions":[],"lastModifiedDate":"2012-03-12T17:21:18","indexId":"70027854","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2775,"text":"Molecular Ecology Notes","onlineIssn":"1471-8286","printIssn":"1471-8278","active":true,"publicationSubtype":{"id":10}},"title":"Microsatellite DNA markers for delineating population structure and kinship among the endangered Kirtland's warbler (Dendroica kirtlandii)","docAbstract":"We document the isolation and characterization of 23 microsatellite DNA markers for the endangered Kirtland's warbler (Dendroica kirtlandii), a Nearctic/Neotropical migrant passerine. This suite of markers revealed moderate to high levels of allelic diversity (averaging 7.7 alleles per locus) and heterozygosity (averaging 72%). Genotypic frequencies at 22 of 23 (95%) markers conformed to Hardy-Weinberg equilibrium expectations, and no linkage disequilibrium was observed in blood samples taken from 14 warblers found on the wintering grounds in the Bahamas archipelago. Multilocus genotypes resulting from this suite of markers should reduce the amount of resources required for initiating new genetic studies assessing breeding structure, parentage, demographics, and individual-level ecological interactions for D. kirtlandii. ?? 2005 Blackwell Publishing Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Molecular Ecology Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1471-8286.2005.00998.x","issn":"14718278","usgsCitation":"King, T., Eackles, M., Henderson, A., Bocetti, C.I., Currie, D., and Wunderle, J., 2005, Microsatellite DNA markers for delineating population structure and kinship among the endangered Kirtland's warbler (Dendroica kirtlandii): Molecular Ecology Notes, v. 5, no. 3, p. 569-571, https://doi.org/10.1111/j.1471-8286.2005.00998.x.","startPage":"569","endPage":"571","numberOfPages":"3","costCenters":[],"links":[{"id":211254,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1471-8286.2005.00998.x"},{"id":238510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-05-09","publicationStatus":"PW","scienceBaseUri":"505a569de4b0c8380cd6d6dc","contributors":{"authors":[{"text":"King, T.L.","contributorId":93416,"corporation":false,"usgs":true,"family":"King","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":415559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eackles, M.S.","contributorId":79059,"corporation":false,"usgs":true,"family":"Eackles","given":"M.S.","affiliations":[],"preferred":false,"id":415557,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henderson, A.P.","contributorId":24163,"corporation":false,"usgs":true,"family":"Henderson","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":415554,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bocetti, Carol I.","contributorId":60343,"corporation":false,"usgs":true,"family":"Bocetti","given":"Carol","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":415556,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Currie, D.","contributorId":38853,"corporation":false,"usgs":true,"family":"Currie","given":"D.","email":"","affiliations":[],"preferred":false,"id":415555,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wunderle, J.M. Jr.","contributorId":90837,"corporation":false,"usgs":true,"family":"Wunderle","given":"J.M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":415558,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":1015301,"text":"1015301 - 2005 - Delayed effects of flood control on a flood-dependent riparian forest","interactions":[],"lastModifiedDate":"2017-12-30T10:26:51","indexId":"1015301","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Delayed effects of flood control on a flood-dependent riparian forest","docAbstract":"The downstream effects of dams on riparian forests are strongly mediated by the character and magnitude of adjustment of the fluvial–geomorphic system. To examine the effects of flow regulation on sand-bed streams in eastern Colorado, we studied the riparian forest on three river segments, the dam-regulated South Fork Republican River downstream of Bonny Dam, the unregulated South Fork Republican River upstream of Bonny Dam, and the unregulated Arikaree River. Although Bonny Dam significantly reduced peak and mean discharge downstream since 1951, there was little difference in forest structure between the regulated and unregulated segments. On all river segments, the riparian forest was dominated by the native pioneer tree, Populus deltoides, which became established during a period of channel narrowing beginning after the 1935 flood of record and ending by 1965. The nonnative Elaeagnus angustifolia was present on all river segments, with recruitment ongoing. The lack of contrast in forest structure between regulated and unregulated reaches resulted primarily from the fact that no large floods occurred on any of the study segments since dam construction. Most of the riparian forest in the study area was located on the broad narrowing terrace, which was rarely inundated on the unregulated segments, resulting in little contrast with the regulated segment. A minor dam effect occurred on the small modern floodplain, which was actively disturbed on the unregulated segments, but not on the regulated segments. Although Bonny Dam had the potential to significantly influence downstream riparian ecosystems, this influence had not been expressed, and may never be if a large flood does not occur within the lifetime of the dam. Minor dam effects to riparian systems can be expected downstream of large dams in some settings, including the present example in which there was insufficient time for the dam effects to by fully expressed.
","language":"English","publisher":"Wiley","doi":"10.1890/04-0076","usgsCitation":"Katz, G.L., Friedman, J.M., and Beatty, S.W., 2005, Delayed effects of flood control on a flood-dependent riparian forest: Ecological Applications, v. 15, no. 3, p. 1019-1035, https://doi.org/10.1890/04-0076.","productDescription":"17 p.","startPage":"1019","endPage":"1035","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":132876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f751c","contributors":{"authors":[{"text":"Katz, Gabrielle L.","contributorId":194352,"corporation":false,"usgs":false,"family":"Katz","given":"Gabrielle","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":322806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Jonathan M. 0000-0002-1329-0663 friedmanj@usgs.gov","orcid":"https://orcid.org/0000-0002-1329-0663","contributorId":2473,"corporation":false,"usgs":true,"family":"Friedman","given":"Jonathan","email":"friedmanj@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":322808,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beatty, Susan W.","contributorId":70530,"corporation":false,"usgs":true,"family":"Beatty","given":"Susan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":322807,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}