{"pageNumber":"2586","pageRowStart":"64625","pageSize":"25","recordCount":184617,"records":[{"id":73783,"text":"fs20053102 - 2005 - Roads and traffic: Effects on ecology and wildlife habitat use; applications for cooperative adaptive management","interactions":[],"lastModifiedDate":"2016-05-26T14:45:16","indexId":"fs20053102","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3102","title":"Roads and traffic: Effects on ecology and wildlife habitat use; applications for cooperative adaptive management","docAbstract":"<p>The land of the United States in dissected by more than 4 million miles of roads that fragment wildlife habitat on both public and private lands. Traffic on these roads causes additional effects. On secondary roads, which provide access to the most natural habitat, the levels, timing, and types of traffic are seldom known. In order to understand the effects of traffic on wildlife, USGS is conducting research cooperatively with the Bureau of Land Management, the U.S. Forest Service, the National Park Service, and the Colorado Division of Wildlife.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053102","usgsCitation":"Ouren, D.S., and Watts, R.D., 2005, Roads and traffic: Effects on ecology and wildlife habitat use; applications for cooperative adaptive management: U.S. Geological Survey Fact Sheet 2005-3102, 2 p., https://doi.org/10.3133/fs20053102.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":126702,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3102.jpg"},{"id":320260,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Gunnison Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.0010986328125,\n              38.35458032659834\n            ],\n            [\n              -108.0010986328125,\n              38.94232097947902\n            ],\n            [\n              -106.86126708984375,\n              38.94232097947902\n            ],\n            [\n              -106.86126708984375,\n              38.35458032659834\n            ],\n            [\n              -108.0010986328125,\n              38.35458032659834\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0fe4b07f02db5feaca","contributors":{"authors":[{"text":"Ouren, Douglas S. ourend@usgs.gov","contributorId":1931,"corporation":false,"usgs":true,"family":"Ouren","given":"Douglas","email":"ourend@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":286474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watts, Raymond D.","contributorId":105713,"corporation":false,"usgs":true,"family":"Watts","given":"Raymond","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":286475,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70035629,"text":"70035629 - 2005 - Paleomagnetic quantification of upper-plate deformation during Miocene detachment faulting in the Mohave Mountains, Arizona","interactions":[],"lastModifiedDate":"2012-03-12T17:21:52","indexId":"70035629","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Paleomagnetic quantification of upper-plate deformation during Miocene detachment faulting in the Mohave Mountains, Arizona","docAbstract":"Paleomagnetic data from Miocene (???20 Ma) volcanic rocks and dikes of west central Arizona reveal the tilt history of Proterozoic crystalline rocks in the hanging wall of the Chemehuevi-Whipple Mountains detachment fault. We obtained magnetization data from dikes and flows in two structural blocks encompassing Crossman Peak and Standard Wash in the Mohave Mountains. In the Crossman block the dike swarm records two components of primary magnetization: (1) CNH, a normal polarity, high-unblocking-temperature or high-coercivity component (inclination, I = 48.5??, declination, D = 6.4??), and (2) CRHm, a reversed polarity, high-temperature or high-coercivity component (I = -33.6??, D = 197.5??). Argon age spectra imply that the dikes have not been reheated above 300??C since their emplacement, and a baked-contact test suggests that the magnetization is likely to be Miocene in age. CRHm deviates from the expected direction of the Miocene axial dipole field and is best explained as a result of progressive tilting about the strike of the overlying andesite flows. These data suggest that the Crossman block was tilted 60?? to the southwest prior to intrusion of the vertical dike swarm, and the block continued to tilt during a magnetic field reversal to normal polarity (CNH). Miocene dikes in the Crossman block are roughly coplanar, so the younger dikes with normal polarity magnetization intruded along planes of weakness parallel to the earlier reversed polarity swarm. An alternative explanation involves CNH magnetization being acquired later during hydrothermal alteration associated with the final stages of dike emplacement. In the Standard Wash block, the primary component of magnetization is a dual-polarity, high-temperature or high-coercivity component (SWHl, I = 7.2??,D= 0.7??). To produce agreement between the expected Miocene magnetic direction and the SWH component requires (1) correcting for a 56?? tilt about the strike of flow bedding and (2) removing a counterclockwise vertical-axis rotation of 20??. The two rotations restore the Standard Wash dikes to vertical, make parallel the dike layering in the Crossman and Standard Wash blocks, and align the strikes of bedding in both blocks. Geologic mapping, geochemical evidence, and paleomagnetic data are consistent with the upper plate of the Mohave Mountains having tilted in response to formation of the underlying detachment fault.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochemistry, Geophysics, Geosystems","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005GC000972","issn":"15252027","usgsCitation":"Pease, V., Hillhouse, J.W., and Wells, R., 2005, Paleomagnetic quantification of upper-plate deformation during Miocene detachment faulting in the Mohave Mountains, Arizona: Geochemistry, Geophysics, Geosystems, v. 6, no. 9, https://doi.org/10.1029/2005GC000972.","costCenters":[],"links":[{"id":216161,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005GC000972"},{"id":244010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"9","noUsgsAuthors":false,"publicationDate":"2005-09-07","publicationStatus":"PW","scienceBaseUri":"505a7414e4b0c8380cd77412","contributors":{"authors":[{"text":"Pease, V.","contributorId":38384,"corporation":false,"usgs":true,"family":"Pease","given":"V.","email":"","affiliations":[],"preferred":false,"id":451551,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hillhouse, John W.","contributorId":29475,"corporation":false,"usgs":true,"family":"Hillhouse","given":"John","middleInitial":"W.","affiliations":[],"preferred":false,"id":451550,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wells, R.E. 0000-0002-7796-0160","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":67537,"corporation":false,"usgs":true,"family":"Wells","given":"R.E.","affiliations":[],"preferred":false,"id":451552,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":73403,"text":"ofr20051399 - 2005 - Visitor survey results for the Souris River Loop National Wildlife Refuges: Completion report","interactions":[],"lastModifiedDate":"2016-05-04T15:52:54","indexId":"ofr20051399","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1399","title":"Visitor survey results for the Souris River Loop National Wildlife Refuges: Completion report","docAbstract":"<p>In support of the CCP planning effort for the Souris River Loop Refuges, the Policy Analysis and Science Assistance Branch/Fort Collins Science Center (PASA) of the U.S. Geological Survey conducted visitor surveys at three refuges in North Dakota: Des Lacs, J. Clark Salyer, and Upper Souris National Wildlife Refuges. This research was conducted in order to assess visitor experience, perceptions, and preferences and visitor spending related to recreation on these public lands. This baseline information and input is needed by the refuges to inform their CCP process. Specifically, this survey research assesses the characteristics of visitors and their trips, the activities in which visitors engage while on the refuge, details regarding their trip experience, as well as their preferences and attitudes about various management features, including existing and future conditions.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051399","usgsCitation":"Sexton, N.R., Koontz, L., and Stewart, S., 2005, Visitor survey results for the Souris River Loop National Wildlife Refuges: Completion report: U.S. Geological Survey Open-File Report 2005-1399, 170 p., https://doi.org/10.3133/ofr20051399.","productDescription":"170 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":192554,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20051399.PNG"},{"id":320275,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1399/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Souris River Loop National Wildlife Refuges","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb8e","contributors":{"authors":[{"text":"Sexton, Natalie R.","contributorId":82750,"corporation":false,"usgs":true,"family":"Sexton","given":"Natalie","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":286401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koontz, Lynne koontzl@usgs.gov","contributorId":2174,"corporation":false,"usgs":false,"family":"Koontz","given":"Lynne","email":"koontzl@usgs.gov","affiliations":[{"id":7016,"text":"Environmental Quality Division, National Park Service, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":286399,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, Susan C.","contributorId":48257,"corporation":false,"usgs":true,"family":"Stewart","given":"Susan C.","affiliations":[],"preferred":false,"id":286400,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028854,"text":"70028854 - 2005 - Alkali elemental and potassium isotopic compositions of Semarkona chondrules","interactions":[],"lastModifiedDate":"2022-05-27T15:41:54.657217","indexId":"70028854","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2715,"text":"Meteoritics and Planetary Science","active":true,"publicationSubtype":{"id":10}},"title":"Alkali elemental and potassium isotopic compositions of Semarkona chondrules","docAbstract":"<p><span>We report measurements of K isotope ratios in 28 Semarkona chondrules with a wide range of petrologic types and bulk compositions as well as the compositions of CPX-mesostasis pairs in 17 type I Semarkona chondrules, including two chondrules with radial alkali zonation and 19 type II chondrules. Despite the wide range in K/Al ratios, no systematic variations in K isotopic compositions were found. Semarkona chondrules do not record a simple history of Rayleigh-type loss of K. Experimentally determined evaporation rates suggest that considerable alkali evaporation would have occurred during chondrule formation. Nevertheless, based on Na CPX-mesostasis distribution coefficients, the alkali contents of the cores of most chondrules in Semarkona were probably established at the time of final crystallization. However, Na CPX-mesostasis distribution coefficients also show that alkali zonation in type I Semarkona chondrules was produced by entry of alkalis after solidification, probably during parent body alteration. This alkali metasomatism may have gone to completion in some chondrules. Our preferred explanation for the lack of systematic isotopic enrichments, even in alkali depleted type I chondrule cores, is that they exchanged with the ambient gas as they cooled.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1945-5100.2005.tb00962.x","usgsCitation":"Alexander, C.M., and Grossman, J.N., 2005, Alkali elemental and potassium isotopic compositions of Semarkona chondrules: Meteoritics and Planetary Science, v. 40, no. 4, p. 541-556, https://doi.org/10.1111/j.1945-5100.2005.tb00962.x.","productDescription":"16 p.","startPage":"541","endPage":"556","numberOfPages":"16","costCenters":[],"links":[{"id":477724,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1945-5100.2005.tb00962.x","text":"Publisher Index Page"},{"id":236446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e966e4b0c8380cd48254","contributors":{"authors":[{"text":"Alexander, C. M. O’D.","contributorId":105418,"corporation":false,"usgs":false,"family":"Alexander","given":"C.","email":"","middleInitial":"M. O’D.","affiliations":[],"preferred":false,"id":420033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grossman, Jeffrey N. 0000-0001-9099-9628","orcid":"https://orcid.org/0000-0001-9099-9628","contributorId":37317,"corporation":false,"usgs":true,"family":"Grossman","given":"Jeffrey","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":420032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028836,"text":"70028836 - 2005 - Thermal maturity of type II kerogen from the New Albany Shale assessed by13C CP/MAS NMR","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028836","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3426,"text":"Solid State Nuclear Magnetic Resonance","active":true,"publicationSubtype":{"id":10}},"title":"Thermal maturity of type II kerogen from the New Albany Shale assessed by13C CP/MAS NMR","docAbstract":"Thermal maturity of oil and gas source rocks is typically quantified in terms of vitrinite reflectance, which is based on optical properties of terrestrial woody remains. This study evaluates 13C CP/MAS NMR parameters in kerogen (i.e., the insoluble fraction of organic matter in sediments and sedimentary rocks) as proxies for thermal maturity in marine-derived source rocks where terrestrially derived vitrinite is often absent or sparse. In a suite of samples from the New Albany Shale (Middle Devonian to the Early Mississippian, Illinois Basin) the abundance of aromatic carbon in kerogen determined by 13C CP/MAS NMR correlates linearly well with vitrinite reflectance. ?? 2004 Elsevier Inc. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Solid State Nuclear Magnetic Resonance","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.ssnmr.2004.08.001","issn":"09262040","usgsCitation":"Werner-Zwanziger, U., Lis, G., Mastalerz, M., and Schimmelmann, A., 2005, Thermal maturity of type II kerogen from the New Albany Shale assessed by13C CP/MAS NMR: Solid State Nuclear Magnetic Resonance, v. 27, no. 1-2, p. 140-148, https://doi.org/10.1016/j.ssnmr.2004.08.001.","startPage":"140","endPage":"148","numberOfPages":"9","costCenters":[],"links":[{"id":209958,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ssnmr.2004.08.001"},{"id":236727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb245e4b08c986b3256b2","contributors":{"authors":[{"text":"Werner-Zwanziger, U.","contributorId":37941,"corporation":false,"usgs":true,"family":"Werner-Zwanziger","given":"U.","email":"","affiliations":[],"preferred":false,"id":419932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lis, G.","contributorId":62806,"corporation":false,"usgs":true,"family":"Lis","given":"G.","email":"","affiliations":[],"preferred":false,"id":419933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mastalerz, Maria","contributorId":78065,"corporation":false,"usgs":true,"family":"Mastalerz","given":"Maria","affiliations":[],"preferred":false,"id":419934,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schimmelmann, A.","contributorId":28348,"corporation":false,"usgs":false,"family":"Schimmelmann","given":"A.","affiliations":[],"preferred":false,"id":419931,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70028873,"text":"70028873 - 2005 - Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028873","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia","docAbstract":"Increased tree growth in temperate and boreal forests has been proposed as a direct consequence of a warming climate. Acid deposition effects on nutrient availability may influence the climate dependency of tree growth, however. This study presents an analysis of archived soil samples that has enabled changes in soil chemistry to be tracked with patterns of tree growth through the 20th century. Soil samples collected in 1926, 1964, and 2001, near St. Petersburg, Russia, showed that acid deposition was likely to have decreased root-available concentrations of Ca (an essential element) and increased root-available concentrations of Al (an inhibitor of Ca uptake). These soil changes coincided with decreased diameter growth and a suppression of climate-tree growth relationships in Norway spruce. Expected increases in tree growth from climate warming may be limited by decreased soil fertility in regions of northern and eastern Europe, and eastern North America, where Ca availability has been reduced by acidic deposition. ?? 2005 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es048759o","issn":"0013936X","usgsCitation":"Lawrence, G., Lapenis, A., Berggren, D., Aparin, B., Smith, K., Shortle, W., Bailey, S., Varlyguin, D., and Babikov, B., 2005, Climate dependency of tree growth suppressed by acid deposition effects on soils in Northwest Russia: Environmental Science & Technology, v. 39, no. 7, p. 2004-2010, https://doi.org/10.1021/es048759o.","startPage":"2004","endPage":"2010","numberOfPages":"7","costCenters":[],"links":[{"id":209981,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es048759o"},{"id":236761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"7","noUsgsAuthors":false,"publicationDate":"2005-02-16","publicationStatus":"PW","scienceBaseUri":"5059f651e4b0c8380cd4c6b1","contributors":{"authors":[{"text":"Lawrence, G.B. 0000-0002-8035-2350","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":76347,"corporation":false,"usgs":true,"family":"Lawrence","given":"G.B.","affiliations":[],"preferred":false,"id":420130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapenis, A.G.","contributorId":85701,"corporation":false,"usgs":true,"family":"Lapenis","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":420132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berggren, D.","contributorId":35531,"corporation":false,"usgs":true,"family":"Berggren","given":"D.","email":"","affiliations":[],"preferred":false,"id":420128,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aparin, B.F.","contributorId":24899,"corporation":false,"usgs":true,"family":"Aparin","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":420126,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, K.T.","contributorId":94807,"corporation":false,"usgs":true,"family":"Smith","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":420133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shortle, W.C.","contributorId":20919,"corporation":false,"usgs":true,"family":"Shortle","given":"W.C.","affiliations":[],"preferred":false,"id":420125,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bailey, S.W.","contributorId":29113,"corporation":false,"usgs":true,"family":"Bailey","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":420127,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Varlyguin, D.L.","contributorId":84967,"corporation":false,"usgs":true,"family":"Varlyguin","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":420131,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Babikov, B.","contributorId":71752,"corporation":false,"usgs":true,"family":"Babikov","given":"B.","email":"","affiliations":[],"preferred":false,"id":420129,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70028859,"text":"70028859 - 2005 - Water dispersal of vegetative bulbils of the invasive exotic Dioscorea oppositifolia L. in southern Illinois","interactions":[],"lastModifiedDate":"2019-11-19T18:31:54","indexId":"70028859","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2571,"text":"Journal of the Torrey Botanical Society","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Water dispersal of vegetative bulbils of the invasive exotic <i>Dioscorea oppositifolia</i> L. in southern Illinois","title":"Water dispersal of vegetative bulbils of the invasive exotic Dioscorea oppositifolia L. in southern Illinois","docAbstract":"<p>Riparian corridors promote dispersal of several species of exotic invasives worldwide. Dispersal plays a role in the colonization of exotic invasive species into new areas and this study was conducted to determine if the invasiveness of <i>Dioscorea oppositifolia</i> L. (Chinese yam) is facilitated by secondary dispersal of vegetative diaspores (bulbils) by water. Since seed production of this plant has not been observed in the United States, bulbils represent the only means of dispersal to new habitats. Dispersal was monitored by placing aquatic traps, tethered bulbils, and painted bulbil caches in a tributary of Drury Creek, Giant City State Park, Illinois. Results indicate that high-energy flow in the creek accelerated secondary dispersal of bulbils downstream and onto the floodplain. The longest recorded dispersal distance was 206.2 m downstream. Dispersal distance of tethered bulbils was not related to rainfall or flow velocity in the creek; however the total number of bulbils trapped was positively related to flow velocity. We conclude that secondary dispersal by water in streams can facilitate dispersal of vegetative bulbils of this exotic species.</p>","language":"English","publisher":"Torrey Botanical Society","doi":"10.3159/1095-5674(2005)132[187:WDOVBO]2.0.CO;2","issn":"10955674","usgsCitation":"Thomas, J., Gibson, D., and Middleton, B., 2005, Water dispersal of vegetative bulbils of the invasive exotic Dioscorea oppositifolia L. in southern Illinois: Journal of the Torrey Botanical Society, v. 132, no. 2, p. 187-196, https://doi.org/10.3159/1095-5674(2005)132[187:WDOVBO]2.0.CO;2.","productDescription":"10 p.","startPage":"187","endPage":"196","numberOfPages":"10","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":236551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","otherGeospatial":"Drury Creek watershed, Giant City State Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.21276092529297,\n              37.57097735996406\n            ],\n            [\n              -89.15542602539062,\n              37.57097735996406\n            ],\n            [\n              -89.15542602539062,\n              37.62592473385395\n            ],\n            [\n              -89.21276092529297,\n              37.62592473385395\n            ],\n            [\n              -89.21276092529297,\n              37.57097735996406\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"132","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc7dae4b08c986b32c673","contributors":{"authors":[{"text":"Thomas, J.R.","contributorId":64011,"corporation":false,"usgs":true,"family":"Thomas","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":420060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibson, D.J.","contributorId":65822,"corporation":false,"usgs":true,"family":"Gibson","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":420061,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Middleton, B.A. 0000-0002-1220-2326 middletonb@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-2326","contributorId":89108,"corporation":false,"usgs":true,"family":"Middleton","given":"B.A.","email":"middletonb@usgs.gov","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":420062,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028874,"text":"70028874 - 2005 - Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin","interactions":[],"lastModifiedDate":"2016-05-03T16:33:33","indexId":"70028874","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin","docAbstract":"<p>Fall Chinook salmon Oncorhynchus tshawytscha in the Snake River basin were listed under the Endangered Species Act in 1992. At the time of listing, it was assumed that fall Chinook salmon juveniles in the Snake River basin adhered strictly to an ocean-type life history characterized by saltwater entry at age 0 and first-year wintering in the ocean. Research showed, however, that some fall Chinook salmon juveniles in the Snake River basin spent their first winter in a reservoir and resumed seaward movement the following spring at age 1 (hereafter, reservoir-type juveniles). We collected wild and hatchery ocean-type fall Chinook salmon juveniles in 1997 and wild and hatchery reservoir-type juveniles in 1998 to assess the condition of the reservoir-type juveniles at the onset of seaward movement. The ocean-type juveniles averaged 112-139 mm fork length, and the reservoir-type juveniles averaged 222-224 mm fork length. The large size of the reservoir-type juveniles suggested a high potential for survival to salt water and subsequent return to freshwater. Scale pattern analyses of the fall Chinook salmon spawners we collected during 1998-2003 supported this point. Of the spawners sampled, an overall average of 41% of the wild fish and 51% of the hatchery fish had been reservoir-type juveniles. Males that had been reservoir-type juveniles often returned as small \"minijacks\" (wild, 16% of total; hatchery, 40% of total), but 84% of the wild males, 60% of the hatchery males, and 100% of the wild and hatchery females that had been reservoir-type juveniles returned at ages and fork lengths commonly observed in populations of Chinook salmon. We conclude that fall Chinook salmon in the Snake River basin exhibit two alternative juvenile life histories, namely ocean-type and reservoir-type. ?? Copyright by the American Fisheries Society 2005.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/T03-131.1","issn":"00028487","usgsCitation":"Connor, W., Sneva, J., Tiffan, K., Steinhorst, R., and Ross, D., 2005, Two alternative juvenile life history types for fall Chinook salmon in the Snake River basin: Transactions of the American Fisheries Society, v. 134, no. 2, p. 291-304, https://doi.org/10.1577/T03-131.1.","productDescription":"14 p.","startPage":"291","endPage":"304","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":236791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210005,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T03-131.1"}],"country":"United States","state":"Idaho, Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.76293945312499,\n              43.84245116699036\n            ],\n            [\n              -116.38916015624999,\n              42.85985981506279\n            ],\n            [\n              -117.48779296875,\n              44.000717834282774\n            ],\n            [\n              -117.520751953125,\n              45.87471224890479\n            ],\n            [\n              -118.004150390625,\n              46.41513877649202\n            ],\n            [\n              -119.44335937499999,\n              45.67548217560647\n            ],\n            [\n              -123.12377929687499,\n              45.42158812329091\n            ],\n            [\n              -124.002685546875,\n              46.057985244793024\n            ],\n            [\n              -123.93676757812499,\n              46.33175800051563\n            ],\n            [\n              -122.882080078125,\n              46.263442671779885\n            ],\n            [\n              -122.354736328125,\n              45.81348649679971\n            ],\n            [\n              -120.60791015625,\n              46.03510927947334\n            ],\n            [\n              -119.124755859375,\n              46.34692761055676\n            ],\n            [\n              -118.311767578125,\n              46.74738913515841\n            ],\n            [\n              -116.60888671874999,\n              46.73233101286786\n            ],\n            [\n              -116.290283203125,\n              46.36209301204985\n            ],\n            [\n              -116.03759765625,\n              44.645208223744035\n            ],\n            [\n              -115.850830078125,\n              44.10336537791152\n            ],\n            [\n              -115.76293945312499,\n              43.84245116699036\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"134","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"505bb94ae4b08c986b327bac","contributors":{"authors":[{"text":"Connor, W.P.","contributorId":98090,"corporation":false,"usgs":true,"family":"Connor","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":420138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sneva, J.G.","contributorId":7066,"corporation":false,"usgs":true,"family":"Sneva","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":420135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tiffan, K.F.","contributorId":19327,"corporation":false,"usgs":true,"family":"Tiffan","given":"K.F.","email":"","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":420136,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steinhorst, R.K.","contributorId":89833,"corporation":false,"usgs":true,"family":"Steinhorst","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":420137,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ross, D.","contributorId":7049,"corporation":false,"usgs":true,"family":"Ross","given":"D.","affiliations":[],"preferred":false,"id":420134,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028876,"text":"70028876 - 2005 - Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:45","indexId":"70028876","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1905,"text":"Holocene","active":true,"publicationSubtype":{"id":10}},"title":"Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada","docAbstract":"The north-flowing, low-gradient section of the Red River in Manitoba has lost ???60% of its valley gradient since 8 ka cal. BP. An existing hydraulic model of the modern Red River flood zone was used to examine the change in flood extent and depth of a discharge equivalent to the 1997 Red River flood (3970 m3/s) for scenarios of gradients at 8, 6, 4 and 2 ka cal. BP as well as 2 ka in the future. The modelling indicates a broad, shallow flood zone for all of the gradient scenarios, with extent and depth increasing over time. Between the 8 ka cal. BP and present-day scenarios, the flood zone increased from 1186 km2 to 1531 km2 (???29%) with depth increasing along four east-west cross-sections by 0.69 m (???61%), 0.91 m (???82%), 0.56 m (???64%) and 0.48 m (???86%). The flood extent and depths increased by a further 18 km2 (???5%) and 0.04-0.06 m (2-5%), respectively, by 2 ka in the future. Most of these changes to the flood zone occurred between 8 and 2 ka cal. BP, reflecting an exponential loss of gradient. A rise in flood depth equivalent to that which occurred between 8 ka cal. BP and the present-day, is assessed as increasing the long-term flood hazard; in contrast, the slight rise in depth between the present-day and 2 ka in the future does not. ?? 2005 Edward Arnold (Publishers) Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Holocene","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1191/0959683605hl804rp","issn":"09596836","usgsCitation":"Brooks, G.R., Thorleifson, L.H., and Lewis, C., 2005, Influence of loss of gradient from postglacial uplift on Red River flood hazard, Manitoba, Canada: Holocene, v. 15, no. 3, p. 347-352, https://doi.org/10.1191/0959683605hl804rp.","startPage":"347","endPage":"352","numberOfPages":"6","costCenters":[],"links":[{"id":210006,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1191/0959683605hl804rp"},{"id":236793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-04-01","publicationStatus":"PW","scienceBaseUri":"505a3b50e4b0c8380cd62401","contributors":{"authors":[{"text":"Brooks, G. R.","contributorId":96312,"corporation":false,"usgs":true,"family":"Brooks","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":420141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorleifson, L. Harvey","contributorId":103430,"corporation":false,"usgs":true,"family":"Thorleifson","given":"L.","email":"","middleInitial":"Harvey","affiliations":[{"id":38105,"text":"Minnesota Geological Survey","active":true,"usgs":false}],"preferred":false,"id":420142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, C.F.M.","contributorId":39971,"corporation":false,"usgs":true,"family":"Lewis","given":"C.F.M.","email":"","affiliations":[],"preferred":false,"id":420140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70028775,"text":"70028775 - 2005 - Two-stage sequential sampling: A neighborhood-free adaptive sampling procedure","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028775","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2151,"text":"Journal of Agricultural, Biological, and Environmental Statistics","active":true,"publicationSubtype":{"id":10}},"title":"Two-stage sequential sampling: A neighborhood-free adaptive sampling procedure","docAbstract":"Designing an efficient sampling scheme for a rare and clustered population is a challenging area of research. Adaptive cluster sampling, which has been shown to be viable for such a population, is based on sampling a neighborhood of units around a unit that meets a specified condition. However, the edge units produced by sampling neighborhoods have proven to limit the efficiency and applicability of adaptive cluster sampling. We propose a sampling design that is adaptive in the sense that the final sample depends on observed values, but it avoids the use of neighborhoods and the sampling of edge units. Unbiased estimators of population total and its variance are derived using Murthy's estimator. The modified two-stage sampling design is easy to implement and can be applied to a wider range of populations than adaptive cluster sampling. We evaluate the proposed sampling design by simulating sampling of two real biological populations and an artificial population for which the variable of interest took the value either 0 or 1 (e.g., indicating presence and absence of a rare event). We show that the proposed sampling design is more efficient than conventional sampling in nearly all cases. The approach used to derive estimators (Murthy's estimator) opens the door for unbiased estimators to be found for similar sequential sampling designs. ?? 2005 American Statistical Association and the International Biometric Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Agricultural, Biological, and Environmental Statistics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1198/108571105X28183","issn":"10857117","usgsCitation":"Salehi, M., and Smith, D., 2005, Two-stage sequential sampling: A neighborhood-free adaptive sampling procedure: Journal of Agricultural, Biological, and Environmental Statistics, v. 10, no. 1, p. 84-103, https://doi.org/10.1198/108571105X28183.","startPage":"84","endPage":"103","numberOfPages":"20","costCenters":[],"links":[{"id":209714,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1198/108571105X28183"},{"id":236406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9a2e4b08c986b327ce0","contributors":{"authors":[{"text":"Salehi, M.","contributorId":94483,"corporation":false,"usgs":true,"family":"Salehi","given":"M.","email":"","affiliations":[],"preferred":false,"id":419700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, D. R. 0000-0001-6074-9257","orcid":"https://orcid.org/0000-0001-6074-9257","contributorId":44108,"corporation":false,"usgs":true,"family":"Smith","given":"D. R.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":419699,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70028860,"text":"70028860 - 2005 - Effect of tilt on strong motion data processing","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028860","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3418,"text":"Soil Dynamics and Earthquake Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Effect of tilt on strong motion data processing","docAbstract":"In the near-field of an earthquake the effects of the rotational components of ground motion may not be negligible compared to the effects of translational motions. Analyses of the equations of motion of horizontal and vertical pendulums show that horizontal sensors are sensitive not only to translational motion but also to tilts. Ignoring this tilt sensitivity may produce unreliable results, especially in calculations of permanent displacements and long-period calculations. In contrast to horizontal sensors, vertical sensors do not have these limitations, since they are less sensitive to tilts. In general, only six-component systems measuring rotations and accelerations, or three-component systems similar to systems used in inertial navigation assuring purely translational motion of accelerometers can be used to calculate residual displacements. ?? 2004 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Soil Dynamics and Earthquake Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.soildyn.2004.10.008","issn":"02677261","usgsCitation":"Graizer, V., 2005, Effect of tilt on strong motion data processing: Soil Dynamics and Earthquake Engineering, v. 25, no. 3, p. 197-204, https://doi.org/10.1016/j.soildyn.2004.10.008.","startPage":"197","endPage":"204","numberOfPages":"8","costCenters":[],"links":[{"id":209824,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.soildyn.2004.10.008"},{"id":236552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0626e4b0c8380cd5110b","contributors":{"authors":[{"text":"Graizer, V.M.","contributorId":67259,"corporation":false,"usgs":true,"family":"Graizer","given":"V.M.","email":"","affiliations":[],"preferred":false,"id":420063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028776,"text":"70028776 - 2005 - Use of tracers and isotopes to evaluate vulnerability of water in domestic wells to septic waste","interactions":[],"lastModifiedDate":"2018-10-31T09:28:18","indexId":"70028776","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1864,"text":"Ground Water Monitoring and Remediation","active":true,"publicationSubtype":{"id":10}},"title":"Use of tracers and isotopes to evaluate vulnerability of water in domestic wells to septic waste","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>In Nebraska, a large number (&gt;200) of shallow sand‐point and cased wells completed in coarse alluvial sediments along rivers and lakes still are used to obtain drinking water for human consumption, even though construction of sand‐point wells for consumptive uses has been banned since 1987. The quality of water from shallow domestic wells potentially vulnerable to seepage from septic systems was evaluated by analyzing for the presence of tracers and multiple isotopes. Samples were collected from 26 sand‐point and perforated, cased domestic wells and were analyzed for bacteria, coliphages, nitrogen species, nitrogen and boron isotopes, dissolved organic carbon (DOC), prescription and nonprescription drugs, or organic waste water contaminants. At least 13 of the 26 domestic well samples showed some evidence of septic system effects based on the results of several tracers including DOC, coliphages, NH<sub>4</sub><sup>+</sup>, NO<sub>3</sub><sup>−</sup>, N<sub>2</sub>, δ<sup>15</sup>N[NO<sub>3</sub><sup>−</sup>] and boron isotopes, and antibiotics and other drugs. Sand‐point wells within 30 m of a septic system and &lt;14 m deep in a shallow, thin aquifer had the most tracers detected and the highest values, indicating the greatest vulnerability to contamination from septic waste.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6592.2005.0015.x","issn":"10693629","usgsCitation":"Verstraeten, I., Fetterman, G., Meyer, M., Bullen, T., and Sebree, S., 2005, Use of tracers and isotopes to evaluate vulnerability of water in domestic wells to septic waste: Ground Water Monitoring and Remediation, v. 25, no. 2, p. 107-117, https://doi.org/10.1111/j.1745-6592.2005.0015.x.","productDescription":"11 p.","startPage":"107","endPage":"117","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":486914,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.unl.edu/usgsstaffpub/1215","text":"External Repository"},{"id":236407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209715,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6592.2005.0015.x"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-27","publicationStatus":"PW","scienceBaseUri":"505bbfa5e4b08c986b329cab","contributors":{"authors":[{"text":"Verstraeten, Ingrid M.","contributorId":61033,"corporation":false,"usgs":true,"family":"Verstraeten","given":"Ingrid M.","affiliations":[],"preferred":false,"id":419702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fetterman, G.S.","contributorId":87349,"corporation":false,"usgs":true,"family":"Fetterman","given":"G.S.","affiliations":[],"preferred":false,"id":419704,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, M.J.","contributorId":20959,"corporation":false,"usgs":true,"family":"Meyer","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":419701,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bullen, T.","contributorId":102651,"corporation":false,"usgs":true,"family":"Bullen","given":"T.","email":"","affiliations":[],"preferred":false,"id":419705,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sebree, S.K.","contributorId":76814,"corporation":false,"usgs":true,"family":"Sebree","given":"S.K.","affiliations":[],"preferred":false,"id":419703,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028853,"text":"70028853 - 2005 - Determinants of wood thrush nest success: A multi-scale, model selection approach","interactions":[],"lastModifiedDate":"2012-03-12T17:20:56","indexId":"70028853","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Determinants of wood thrush nest success: A multi-scale, model selection approach","docAbstract":"We collected data on 212 wood thrush (Hylocichla mustelina) nests in central New York from 1998 to 2000 to determine the factors that most strongly influence nest success. We used an information-theoretic approach to assess and rank 9 models that examined the relationship between nest success (i.e., the probability that a nest would successfully fledge at least 1 wood thrush offspring) and habitat conditions at different spatial scales. We found that 4 variables were significant predictors of nesting success for wood thrushes: (1) total core habitat within 5 km of a study site, (2) distance to forest-field edge, (3) total forest cover within 5 km of the study site, and (4) density and variation in diameter of trees and shrubs surrounding the nest. The coefficients of these predictors were all positive. Of the 9 models evaluated, amount of core habitat in the 5-km landscape was the best-fit model, but the vegetation structure model (i.e., the density of trees and stems surrounding a nest) was also supported by the data. Based on AIC weights, enhancement of core area is likely to be a more effective management option than any other habitat-management options explored in this study. Bootstrap analysis generally confirmed these results; core and vegetation structure models were ranked 1, 2, or 3 in over 50% of 1,000 bootstrap trials. However, bootstrap results did not point to a decisive model, which suggests that multiple habitat factors are influencing wood thrush nesting success. Due to model uncertainty, we used a model averaging approach to predict the success or failure of each nest in our dataset. This averaged model was able to correctly predict 61.1% of nest outcomes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/0022-541X(2005)069[0699:DOWTNS]2.0.CO;2","issn":"0022541X","usgsCitation":"Driscoll, M.J., Donovan, T., Mickey, R., Howard, A., and Fleming, K., 2005, Determinants of wood thrush nest success: A multi-scale, model selection approach: Journal of Wildlife Management, v. 69, no. 2, p. 699-709, https://doi.org/10.2193/0022-541X(2005)069[0699:DOWTNS]2.0.CO;2.","startPage":"699","endPage":"709","numberOfPages":"11","costCenters":[],"links":[{"id":209745,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0022-541X(2005)069[0699:DOWTNS]2.0.CO;2"},{"id":236445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff84e4b0c8380cd4f226","contributors":{"authors":[{"text":"Driscoll, Melanie J.L.","contributorId":105492,"corporation":false,"usgs":false,"family":"Driscoll","given":"Melanie","email":"","middleInitial":"J.L.","affiliations":[],"preferred":false,"id":420031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donovan, T.","contributorId":31965,"corporation":false,"usgs":true,"family":"Donovan","given":"T.","email":"","affiliations":[],"preferred":false,"id":420027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mickey, R.","contributorId":44725,"corporation":false,"usgs":true,"family":"Mickey","given":"R.","email":"","affiliations":[],"preferred":false,"id":420028,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howard, A.","contributorId":54392,"corporation":false,"usgs":true,"family":"Howard","given":"A.","email":"","affiliations":[],"preferred":false,"id":420029,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fleming, K.K.","contributorId":62392,"corporation":false,"usgs":true,"family":"Fleming","given":"K.K.","email":"","affiliations":[],"preferred":false,"id":420030,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":74333,"text":"ofr20051016 - 2005 - Gulf of Mexico Integrated Science - Tampa Bay Study - Historical and Prehistorical Record of Tampa Bay Environments","interactions":[],"lastModifiedDate":"2012-02-10T00:11:36","indexId":"ofr20051016","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1016","title":"Gulf of Mexico Integrated Science - Tampa Bay Study - Historical and Prehistorical Record of Tampa Bay Environments","docAbstract":"To study how Tampa Bay, Florida, has changed over time, the prehistorical conditions and natural variations in the bay environment are being evaluated. These variations can be tracked by examining the sediments that have accumulated in and around the bay. The prehistorical record, which pre-dates settlers' arrival in the Tampa Bay area around 1850, provides a baseline with which to compare and evaluate the magnitude and effects of sea-level, climate, biological, geochemical, and man-made changes. These data also are valuable for planning and conducting projects aimed at restoring wetlands and other estuarine habitats to their original state. In addition, the data provide a basis for judging efforts to improve the health of the bay.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051016","usgsCitation":"Edgar, T., 2005, Gulf of Mexico Integrated Science - Tampa Bay Study - Historical and Prehistorical Record of Tampa Bay Environments: U.S. Geological Survey Open-File Report 2005-1016, 2 p., https://doi.org/10.3133/ofr20051016.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":13261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://dl.cr.usgs.gov/net_prod_download/public/gom_net_pub_products/DOC/OFR_2005-1016_Edgar.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":193294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.83333333333333,27.5 ], [ -82.83333333333333,28 ], [ -82.33333333333333,28 ], [ -82.33333333333333,27.5 ], [ -82.83333333333333,27.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a226","contributors":{"authors":[{"text":"Edgar, Terry","contributorId":30701,"corporation":false,"usgs":true,"family":"Edgar","given":"Terry","email":"","affiliations":[],"preferred":false,"id":286587,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027352,"text":"70027352 - 2005 - Fault-dominated deformation in an ice dam during annual filling and drainage of a marginal lake","interactions":[],"lastModifiedDate":"2013-03-12T20:22:09","indexId":"70027352","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":794,"text":"Annals of Glaciology","active":true,"publicationSubtype":{"id":10}},"title":"Fault-dominated deformation in an ice dam during annual filling and drainage of a marginal lake","docAbstract":"Ice-dammed Hidden Creek Lake, Alaska, USA, outbursts annually in about 2-3 days. As the lake fills, a wedge of water penetrates beneath the glacier, and the surface of this 'ice dam' rises; the surface then falls as the lake drains. Detailed optical surveying of the glacier near the lake allows characterization of ice-dam deformation. Surface uplift rate is close to the rate of lake-level rise within about 400 m of the lake, then decreases by 90% over about 100 m. Such a steep gradient in uplift rate cannot be explained in terms of ice-dam flexure. Moreover, survey targets spanning the zone of steep uplift gradient move relative to one another in a nearly reversible fashion as the lake fills and drains. Evidently, the zone of steep uplift gradient is a fault zone, with the faults penetrating the entire thickness of the ice dam. Fault motion is in a reverse sense as the lake fills, but in a normal sense as the lake drains. As the overall fault pattern is the same from year to year, even though ice is lost by calving, the faults must be regularly regenerated, probably by linkage of surface and bottom crevasses as ice is advected toward the lake basin.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Annals of Glaciology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.3189/172756405781813456","issn":"02603055","usgsCitation":"Walder, J.S., Trabant, D., Cunico, M., Anderson, S., Anderson, R., Fountain, A.G., and Malm, A., 2005, Fault-dominated deformation in an ice dam during annual filling and drainage of a marginal lake: Annals of Glaciology, v. 40, p. 174-178, https://doi.org/10.3189/172756405781813456.","startPage":"174","endPage":"178","numberOfPages":"5","costCenters":[],"links":[{"id":235206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269196,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3189/172756405781813456"}],"volume":"40","noUsgsAuthors":false,"publicationDate":"2017-09-14","publicationStatus":"PW","scienceBaseUri":"505a0f1fe4b0c8380cd537a2","contributors":{"authors":[{"text":"Walder, J. S.","contributorId":32561,"corporation":false,"usgs":true,"family":"Walder","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":413297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trabant, D.C.","contributorId":42209,"corporation":false,"usgs":true,"family":"Trabant","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":413298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cunico, M.","contributorId":82905,"corporation":false,"usgs":true,"family":"Cunico","given":"M.","affiliations":[],"preferred":false,"id":413300,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Anderson, S.P.","contributorId":59600,"corporation":false,"usgs":true,"family":"Anderson","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":413299,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Anderson, R. Scott","contributorId":6983,"corporation":false,"usgs":false,"family":"Anderson","given":"R. Scott","affiliations":[{"id":7034,"text":"School of Earth Sciences and Environmental Sustainability at Northern Arizona University, in Flagstaff","active":true,"usgs":false}],"preferred":false,"id":413294,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fountain, A. G.","contributorId":29815,"corporation":false,"usgs":true,"family":"Fountain","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":413296,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Malm, A.","contributorId":17021,"corporation":false,"usgs":true,"family":"Malm","given":"A.","email":"","affiliations":[],"preferred":false,"id":413295,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":1015298,"text":"1015298 - 2005 - Core competencies for natural resource negotiation","interactions":[],"lastModifiedDate":"2018-01-01T17:22:12","indexId":"1015298","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1559,"text":"Environmental Practice","active":true,"publicationSubtype":{"id":10}},"title":"Core competencies for natural resource negotiation","docAbstract":"<div class=\"row row-md  \"><div class=\"col-md-7-12 \"><div class=\"contents\" data-pb-dropzone=\"contents1\"><div id=\"d29f04e9-776c-4996-a0d8-931023161e00\" class=\"widget literatumPublicationContentWidget none  widget-none  widget-compact-all\"><div class=\"wrapped \"><div class=\"widget-body body body-none  body-compact-all\"><div class=\"publication-tabs ja publication-tabs-dropdown\"><div class=\"tabs tabs-widget\"><div class=\"tab-content \"><div class=\"tab tab-pane active\"><div class=\"hlFld-Abstract test\"><div class=\"abstractSection abstractInFull\"><p>Natural resource negotiation often involves multiple parties with overlapping interests and issues that can provide opportunities for mutually beneficial solutions. These opportunities can be missed, however, if negotiators are unable to comprehend the facts of a negotiation, understand the interests of other parties, or accurately evaluate the options that increase the size of the negotiation pie. Through structured personal interviews with more than 60 representatives from seven different hydropower negotiations, respondents identified core competencies that help negotiators succeed at accurately comprehending the facts of a negotiation, comprehending the interests of other parties, and fully understanding the available options and alternatives. We categorized those core competencies into three dimensions of negotiation - interpersonal, organizational, and operational.</p></div></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"Taylor & Francis","doi":"10.1017/S1466046605050210","usgsCitation":"Gillette, S., and Lamb, B.L., 2005, Core competencies for natural resource negotiation: Environmental Practice, v. 7, no. 3, p. 155-164, https://doi.org/10.1017/S1466046605050210.","productDescription":"10 p.","startPage":"155","endPage":"164","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":133015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-03-27","publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6849c8","contributors":{"authors":[{"text":"Gillette, S.C.","contributorId":102844,"corporation":false,"usgs":true,"family":"Gillette","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":322803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lamb, B. L.","contributorId":6395,"corporation":false,"usgs":true,"family":"Lamb","given":"B.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":322802,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1015295,"text":"1015295 - 2005 - Hybridization of Tamarix ramosissima and T. chinensis (saltcedars) with T. aphylla (athel) (tamaricaceae) in the southwestern USA dertermined from DNA sequence data","interactions":[],"lastModifiedDate":"2018-01-01T15:19:00","indexId":"1015295","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2639,"text":"Madroño","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Hybridization of i>Tamarix ramosissima</i> and <i>T. chinensis</i> (saltcedars) with <i>T. aphylla</i> (athel) (tamaricaceae) in the southwestern USA dertermined from DNA sequence data","title":"Hybridization of Tamarix ramosissima and T. chinensis (saltcedars) with T. aphylla (athel) (tamaricaceae) in the southwestern USA dertermined from DNA sequence data","docAbstract":"<p>Morphological intermediates between <i>Tamarix ramosissima</i> or <i>T. chinensis</i> (saltcedars) and <i>T. aphylla</i> (athel) were found recently in three locations in the southwestern USA, and were assumed to be hybrids or a previously unreported species. We sequenced chloroplast and nuclear DNA from putative parental and hybrid morphotypes and hybrid status of morphological intermediates was supported. Chloroplast data suggest that the seed source for these hybrids is <i>T. aphylla</i>. Invasive <i>T. aphylla</i> genotypes found in Australia match those found in the USA. Seed was collected from one of the hybrids, and a low percentage of it was viable. This hybrid combination has not been previously reported in the USA or the native ranges of the species. Although populations of this novel <i>Tamarix</i> hybrid appear to be uncommon at present, both parental species are considered invasive (saltcedars in North America; athel in Australia), and it is possible that more aggressive hybrid genotypes could be produced. Therefore, natural resource managers concerned with the potential spread of non-native species should be aware of the existence of these plants and monitor their future spread.</p>","language":"English","publisher":"California Botanical Society","doi":"10.3120/0024-9637(2005)52[1:HOTRAT]2.0.CO;2","usgsCitation":"Gaskin, J.F., and Shafroth, P.B., 2005, Hybridization of Tamarix ramosissima and T. chinensis (saltcedars) with T. aphylla (athel) (tamaricaceae) in the southwestern USA dertermined from DNA sequence data: Madroño, v. 52, no. 1, p. 1-10, https://doi.org/10.3120/0024-9637(2005)52[1:HOTRAT]2.0.CO;2.","productDescription":"10 p.","startPage":"1","endPage":"10","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":132558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a39a","contributors":{"authors":[{"text":"Gaskin, John F.","contributorId":39307,"corporation":false,"usgs":true,"family":"Gaskin","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":322791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shafroth, Patrick B. 0000-0002-6064-871X shafrothp@usgs.gov","orcid":"https://orcid.org/0000-0002-6064-871X","contributorId":2000,"corporation":false,"usgs":true,"family":"Shafroth","given":"Patrick","email":"shafrothp@usgs.gov","middleInitial":"B.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":322792,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027344,"text":"70027344 - 2005 - Mule deer and pronghorn migration in western Wyoming","interactions":[],"lastModifiedDate":"2012-03-12T17:20:27","indexId":"70027344","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Mule deer and pronghorn migration in western Wyoming","docAbstract":"Migratory mule deer (Odocoileus hemionus) and pronghorn (Antilocapra americana) populations rely on seasonal ranges to meet their annual nutritional and energetic requirements. Because seasonal ranges often occur great distances apart and across a mix of vegetation types and land ownership, maintaining migration corridors to and from these ranges can be difficult, especially if managers do not have detailed information on mule deer and pronghorn seasonal movements. We captured, radiomarked, and monitored mule deer (n = 171) and pronghorn (n = 34) in western Wyoming to document seasonal distribution patterns and migration routes. Mule deer and pronghorn migrated 20-158 km and 116-258 km, respectively, between seasonal ranges. These distances represented the longest recorded migrations for either species. We identified a number of bottlenecks along the migration routes of mule deer and pronghorn, but the most critical appeared to be the 1.6-km-wide Trapper's Point bottleneck, which was used by both mule deer and pronghorn during their spring and autumn migrations. Housing developments and roadways apparently have reduced the effective width of this bottleneck to <0.8 km. We estimate 2,500-3,500 mule deer and 1,500-2,000 pronghorn move through the bottleneck twice a year during spring and autumn migrations. Identification and protection of migration corridors and bottlenecks will be necessary to maintain mule deer and pronghorn populations throughout their range.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2193/0091-7648(2005)33[1266:MDAPMI]2.0.CO;2","issn":"00917648","usgsCitation":"Sawyer, H., Lindzey, F., and McWhirter, D., 2005, Mule deer and pronghorn migration in western Wyoming: Wildlife Society Bulletin, v. 33, no. 4, p. 1266-1273, https://doi.org/10.2193/0091-7648(2005)33[1266:MDAPMI]2.0.CO;2.","startPage":"1266","endPage":"1273","numberOfPages":"8","costCenters":[],"links":[{"id":209335,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2193/0091-7648(2005)33[1266:MDAPMI]2.0.CO;2"},{"id":235642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5f8de4b0c8380cd7100d","contributors":{"authors":[{"text":"Sawyer, H.","contributorId":59910,"corporation":false,"usgs":false,"family":"Sawyer","given":"H.","email":"","affiliations":[],"preferred":false,"id":413260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindzey, F.","contributorId":76113,"corporation":false,"usgs":true,"family":"Lindzey","given":"F.","email":"","affiliations":[],"preferred":false,"id":413261,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McWhirter, D.","contributorId":106294,"corporation":false,"usgs":true,"family":"McWhirter","given":"D.","affiliations":[],"preferred":false,"id":413262,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027351,"text":"70027351 - 2005 - Monitored natural attenuation and enhanced attenuation for chlorinated solvent plumes - It's all about balance","interactions":[],"lastModifiedDate":"2020-05-01T18:43:54.133336","indexId":"70027351","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Monitored natural attenuation and enhanced attenuation for chlorinated solvent plumes - It's all about balance","docAbstract":"<p>Nature's inherent ability to cleanse itself is at the heart of Monitored Natural Attenuation (MNA). The complexity comes when one attempts to measure and calculate this inherent ability, called the Natural Attenuation Capacity (NAC), and determine if it is sufficient to cleanse the system to agreed upon criteria. An approach that is simple in concept for determining whether the NAC is sufficient for MNA to work is the concept of a mass balance. Mass balance is a robust framework upon which all decisions can be made. The inflows to and outflows from the system are balanced against the NAC of the subsurface system. For MNA to be acceptable, the NAC is balanced against the contaminant loading to the subsurface system with the resulting outflow from the system being in a range that is acceptable to the regulating and decision-making parties. When the system is such that the resulting outflow is not within an acceptable range, the idea of taking actions that are sustainable and that will bring the system within the acceptable range of outflows is evaluated. These sustainable enhancements are being developed under the Enhanced Attenuation (EA) concept.&nbsp;</p>","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":"May 15-19, 2005","conferenceLocation":"Anchorage, AK","language":"English","publisher":"ASCE","doi":"10.1061/40792(173)375","isbn":"","usgsCitation":"Adams, K., Vangelas, K., Looney, B., Chapelle, F., Early, T., Gilmore, T., and Sink, C., 2005, Monitored natural attenuation and enhanced attenuation for chlorinated solvent plumes - It's all about balance, <i>in</i> World Water Congress 2005: Impacts of global climate change - Proceedings of the 2005 World Water and Environmental Resources Congress, Anchorage, AK, May 15-19, 2005, https://doi.org/10.1061/40792(173)375.","startPage":"","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":235177,"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":"505a5d55e4b0c8380cd70302","contributors":{"authors":[{"text":"Adams, K.A.","contributorId":74555,"corporation":false,"usgs":true,"family":"Adams","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":413290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vangelas, K.M.","contributorId":57638,"corporation":false,"usgs":true,"family":"Vangelas","given":"K.M.","affiliations":[],"preferred":false,"id":413289,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Looney, B.B.","contributorId":54002,"corporation":false,"usgs":true,"family":"Looney","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":413288,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chapelle, F.","contributorId":103048,"corporation":false,"usgs":true,"family":"Chapelle","given":"F.","affiliations":[],"preferred":false,"id":413293,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Early, T.","contributorId":100168,"corporation":false,"usgs":true,"family":"Early","given":"T.","email":"","affiliations":[],"preferred":false,"id":413292,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gilmore, T.","contributorId":76916,"corporation":false,"usgs":true,"family":"Gilmore","given":"T.","email":"","affiliations":[],"preferred":false,"id":413291,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sink, C.H.","contributorId":40779,"corporation":false,"usgs":true,"family":"Sink","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":413287,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":1015262,"text":"1015262 - 2005 - Recent water temperature trends in the Lower Klamath River, California","interactions":[],"lastModifiedDate":"2017-12-27T19:35:45","indexId":"1015262","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Recent water temperature trends in the Lower Klamath River, California","docAbstract":"<p>Elevated water temperatures have been implicated as a factor limiting the recovery of anadromous salmonids in the Klamath River basin. This article reviews evidence of a multidecade trend of increasing temperatures in the lower main-stem Klamath River above the ocean and, based on model simulations, finds a high probability that water temperature has been increasing by approximately 0.5°C/decade (95% confidence interval (CI) = 0.42–0.60°C/decade) since the early 1960s. The season of high temperatures that are potentially stressful to salmonids has lengthened by about 1 month over the period studied, and the average length of main-stem river with cool summer temperatures has declined by about 8.2 km/decade. Water temperature trends seem unrelated to any change in main-stem water availability but are consistent with measured basinwide air temperature increases. Main-stem warming may be related to the cyclic Pacific Decadal Oscillation, but if this trend continues it might jeopardize the recovery of anadromous salmonids in the Klamath River basin.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/M04-007.1","usgsCitation":"Bartholow, J.M., 2005, Recent water temperature trends in the Lower Klamath River, California: North American Journal of Fisheries Management, v. 25, no. 1, p. 152-162, https://doi.org/10.1577/M04-007.1.","productDescription":"11 p.","startPage":"152","endPage":"162","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":132874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Klamath River","volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-01","publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689fb6","contributors":{"authors":[{"text":"Bartholow, John M.","contributorId":77598,"corporation":false,"usgs":true,"family":"Bartholow","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":322703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1004049,"text":"1004049 - 2005 - USGS/National Wildlife Health Center's Quarterly Wildlife Mortality Report","interactions":[],"lastModifiedDate":"2015-01-26T14:01:09","indexId":"1004049","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3499,"text":"Supplement to the Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"USGS/National Wildlife Health Center's Quarterly Wildlife Mortality Report","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Supplement to the Journal of Wildlife Diseases","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lemanski, C., Converse, K., Sohn, R., and McLaughlin, G., 2005, USGS/National Wildlife Health Center's Quarterly Wildlife Mortality Report: Supplement to the Journal of Wildlife Diseases, v. 41, no. 2, 3 p.","productDescription":"3 p.","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":129649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -180.17578125,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              72.71190310803662\n            ],\n            [\n              -65.7421875,\n              17.14079039331665\n            ],\n            [\n              -180.17578125,\n              17.14079039331665\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"41","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f880","contributors":{"authors":[{"text":"Lemanski, C.","contributorId":9611,"corporation":false,"usgs":true,"family":"Lemanski","given":"C.","email":"","affiliations":[],"preferred":false,"id":315045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Converse, K.","contributorId":40157,"corporation":false,"usgs":true,"family":"Converse","given":"K.","affiliations":[],"preferred":false,"id":315047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sohn, R.","contributorId":8042,"corporation":false,"usgs":true,"family":"Sohn","given":"R.","email":"","affiliations":[],"preferred":false,"id":315044,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McLaughlin, G.","contributorId":38506,"corporation":false,"usgs":true,"family":"McLaughlin","given":"G.","email":"","affiliations":[],"preferred":false,"id":315046,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1015261,"text":"1015261 - 2005 - Resilience of willow stems after release from intense elk browsing","interactions":[],"lastModifiedDate":"2017-12-28T10:13:11","indexId":"1015261","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3228,"text":"Rangeland Ecology and Management","onlineIssn":"1551-5028","printIssn":"1550-7424","active":true,"publicationSubtype":{"id":10}},"title":"Resilience of willow stems after release from intense elk browsing","docAbstract":"<p>The resilience of willow (<i>Salix monticola</i> Bebb, <i>Salix geyeriana</i> Anderss., <i>Salix planifolia</i> Pursh) stems released from intense elk (<i>Cervus elaphus</i>) browsing in Rocky Mountain National Park, Colorado, was quantified in 1998 with a retrospective study that compared biomass, number, and length of segments on willow stems located inside (protected) and outside (browsed) elk exclosures. Segment biomass increased each year after protection by about 3–12 g year<sup>−1</sup> on browsed stems and 10–27 g year<sup>−1</sup> on protected stems. The number of segments on stems was similar for browsed and protected stems in the first 2 years after exclusion but differed in the next 3 years, when they increased exponentially on protected stems. Nearly 80% of segments on browsed stems were &lt; 5 cm in length in 1994–1997, which caused stems to develop a short-hedged morphology. Protected stems had more long segments and fewer short segments than browsed stems for the first 3 years, but then increased their number of short segments as stems became tall and bushy. Thus, evidence suggests short-hedged willow stems are highly resilient and can rapidly recover height and vigor after protection from intense elk browsing.</p>","language":"English","publisher":"Society for Range Management","doi":"10.2111/05-043R.1","usgsCitation":"Baker, B., Peinetti, H., and Coughenour, M., 2005, Resilience of willow stems after release from intense elk browsing: Rangeland Ecology and Management, v. 58, no. 6, p. 575-581, https://doi.org/10.2111/05-043R.1.","productDescription":"7 p.","startPage":"575","endPage":"581","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":477845,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10150/643383","text":"External Repository"},{"id":132873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629eae","contributors":{"authors":[{"text":"Baker, B.W.","contributorId":18707,"corporation":false,"usgs":true,"family":"Baker","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":322700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peinetti, H.R.","contributorId":38115,"corporation":false,"usgs":true,"family":"Peinetti","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":322701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coughenour, M.B.","contributorId":46473,"corporation":false,"usgs":true,"family":"Coughenour","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":322702,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027346,"text":"70027346 - 2005 - ASTER DEM performance","interactions":[],"lastModifiedDate":"2017-04-10T13:00:20","indexId":"70027346","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1944,"text":"IEEE Transactions on Geoscience and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"ASTER DEM performance","docAbstract":"<p><span>The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument onboard the National Aeronautics and Space Administration's Terra spacecraft has an along-track stereoscopic capability using its a near-infrared spectral band to acquire the stereo data. ASTER has two telescopes, one for nadir-viewing and another for backward-viewing, with a base-to-height ratio of 0.6. The spatial resolution is 15 m in the horizontal plane. Parameters such as the line-of-sight vectors and the pointing axis were adjusted during the initial operation period to generate Level-1 data products with a high-quality stereo system performance. The evaluation of the digital elevation model (DEM) data was carried out both by Japanese and U.S. science teams separately using different DEM generation software and reference databases. The vertical accuracy of the DEM data generated from the Level-1A data is 20 m with 95% confidence without ground control point (GCP) correction for individual scenes. Geolocation accuracy that is important for the DEM datasets is better than 50 m. This appears to be limited by the spacecraft position accuracy. In addition, a slight increase in accuracy is observed by using GCPs to generate the stereo data.</span></p>","language":"English","publisher":"IEEE","doi":"10.1109/TGRS.2005.847924","issn":"01962892","usgsCitation":"Fujisada, H., Bailey, G., Kelly, G.G., Hara, S., and Abrams, M.J., 2005, ASTER DEM performance: IEEE Transactions on Geoscience and Remote Sensing, v. 43, no. 12, p. 2707-2713, https://doi.org/10.1109/TGRS.2005.847924.","productDescription":"7 p.","startPage":"2707","endPage":"2713","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":235108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":208970,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1109/TGRS.2005.847924"}],"volume":"43","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e638e4b0c8380cd4726b","contributors":{"authors":[{"text":"Fujisada, H.","contributorId":37906,"corporation":false,"usgs":true,"family":"Fujisada","given":"H.","email":"","affiliations":[],"preferred":false,"id":413267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, G. B.","contributorId":105041,"corporation":false,"usgs":true,"family":"Bailey","given":"G. B.","affiliations":[],"preferred":false,"id":413270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelly, Glen G.","contributorId":90916,"corporation":false,"usgs":true,"family":"Kelly","given":"Glen","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":413269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hara, S.","contributorId":50699,"corporation":false,"usgs":true,"family":"Hara","given":"S.","email":"","affiliations":[],"preferred":false,"id":413268,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Abrams, M. J.","contributorId":29859,"corporation":false,"usgs":true,"family":"Abrams","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":413266,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027833,"text":"70027833 - 2005 - Stress distribution along the Fairweather-Queen Charlotte transform fault system","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70027833","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Stress distribution along the Fairweather-Queen Charlotte transform fault system","docAbstract":"Tectonic loading and Coulomb stress transfer are modeled along the right-lateral Fairweather-Queen Charlotte transform fault system using a threedimensional boundary element program. The loading model includes slip below 12 km along the transform as well as motion of the Pacific plate, and it is consistent with most available Global Positioning System (GPS) displacement rate data. Coulomb stress transfer is shown to have been a weak contributing factor in the failure of the southeastern (Sitka) segment of the Fairweather fault in 1972, hastening the occurrence of the earthquake by only about 8 months. Failure of the Sitka segment was enhanced by a combination of cumulative loading from below (95%) by slip of about 5 cm/yr since 1848, by stress transfer (about 1%) from major earthquakes on straddling segments of the Queen Charlotte fault (M 8.1 in 1949) and the Fairweather fault (M 7.8 in 1958), and by viscoelastic relaxation (about 4%) following the great 1964 Alaska earthquake, modeled by Pollitz et al. (1998). Cumulative stress increases in excess of 7 MPa at a depth of 8 km are projected prior to the M 7.6 earthquake. Coulomb stress transferred by the rupture of the great M 9.2 Alaska earthquake in 1964 (Bufe, 2004a) also hastened the occurrence of the 1972 event, but only by a month or two. Continued tectonic loading over the last half century and stress transfer from the M 7.6 Sitka event has resulted in restressing of the adjacent segments by about 3 MPa at 8 km depth. The occurrence of a M 6.8 earthquake on the northwestern part of the Queen Charlotte fault on 28 June 2004, the largest since 1949, also suggests increased stress. The Cape St. James segment of the fault immediately southeast of the 1949 Queen Charlotte rupture has accumulated about 6 MPa at 8 km through loading since 1900 and stress transfer in 1949. A continued rise in earthquake hazard is indicated for the Alaska panhandle and Queen Charlotte Islands region in the decades ahead as the potential for damaging earthquakes increases.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Seismological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1785/0120040171","issn":"00371106","usgsCitation":"Bufe, C., 2005, Stress distribution along the Fairweather-Queen Charlotte transform fault system: Bulletin of the Seismological Society of America, v. 95, no. 5, p. 2001-2008, https://doi.org/10.1785/0120040171.","startPage":"2001","endPage":"2008","numberOfPages":"8","costCenters":[],"links":[{"id":210986,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1785/0120040171"},{"id":238109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9b55e4b08c986b31cdef","contributors":{"authors":[{"text":"Bufe, C. G.","contributorId":79443,"corporation":false,"usgs":true,"family":"Bufe","given":"C. G.","affiliations":[],"preferred":false,"id":415433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027959,"text":"70027959 - 2005 - Volcanic-ash hazard to aviation during the 2003-2004 eruptive activity of Anatahan volcano, Commonwealth of the Northern Mariana Islands","interactions":[],"lastModifiedDate":"2019-05-02T11:43:14","indexId":"70027959","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Volcanic-ash hazard to aviation during the 2003-2004 eruptive activity of Anatahan volcano, Commonwealth of the Northern Mariana Islands","docAbstract":"<p>Within the Commonwealth of the Northern Mariana Islands (CNMI), Anatahan is one of nine active subaerial volcanoes that pose hazards to major air-traffic routes from airborne volcanic ash. The 2003-2004 eruptive activity of Anatahan volcano affected the region's aviation operations for 3 days in May 2003. On the first day of the eruption (10 May 2003), two international flights from Saipan to Japan were cancelled, and several flights implemented ash-avoidance procedures. On 13 May 2003, a high-altitude flight through volcanic gas was reported, with no perceptible damage to the aircraft. TOMS and MODIS analysis of satellite data strongly suggests that no significant ash and only minor amounts of SO2 were involved in the incident, consistent with crew observations. On 23 May 2003, airport operations were disrupted when tropical-cyclone winds dispersed ash to the south, dusting Saipan with light ashfall and causing flight cancellations there and at Guam 320 km south of the volcano. Operational (near-real-time) monitoring of ash clouds produced by Anatahan has been conducted since the first day of the eruption on 10 May 2003 by the Washington Volcanic Ash Advisory Center (VAAC). The VAAC was among the first groups outside of the immediate area of the volcano to detect and report on the unexpected eruption of Anatahan. After being contacted about an unusual cloud by National Weather Service forecasters in Guam at 1235 UTC on 10 May 2003, the VAAC analyzed GOES 9 images, confirming Anatahan as the likely source of an ash cloud and estimating that the eruption began at about 0730 UTC. The VAAC issued its first Volcanic Ash Advisory for Anatahan at 1300 UTC on 10 May 2003 more than 5 h after the start of the eruption, the delay reflecting the difficulty of detecting and confirming a surprise eruption at a remote volcano with no in situ real-time geophysical monitoring. The initial eruption plume reached 10.7-13.4 km (35,000-44,000 ft), well into jet cruise altitudes; thereafter, the maximum plume height decreased and during the rest of the eruption usually did not exceed ???5 km (???17,000 ft), which lessened the potential hazard to aircraft at higher cruise altitudes. Drifting ash clouds commonly extended hundreds of kilometers from the volcano, occasionally as far west as the Philippines. Over the course of the eruptive activity in 2003-2004, the VAAC issued 323 advisories (168 with graphical depictions of ash clouds) for Anatahan, serving as a reliable source of ash-cloud information for aviation-related meteorological offices and air carriers. With a record of frequent eruptions in the CNMI, continued satellite and in situ real-time geophysical monitoring is needed at Anatahan and other Marianas volcanoes so that potential hazards to aviation from any future eruptive activity can be quickly and correctly assessed. 2005 Elsevier B.V. All rights reserved.</p>","largerWorkTitle":"Journal of Volcanology and Geothermal Research","language":"English","doi":"10.1016/j.jvolgeores.2004.12.011","issn":"03770273","usgsCitation":"Guffanti, M., Ewert, J., Gallina, G., Bluth, G., and Swanson, G., 2005, Volcanic-ash hazard to aviation during the 2003-2004 eruptive activity of Anatahan volcano, Commonwealth of the Northern Mariana Islands: Journal of Volcanology and Geothermal Research, v. 146, no. 1-3 SPEC. ISS., p. 241-255, https://doi.org/10.1016/j.jvolgeores.2004.12.011.","productDescription":"15 p.","startPage":"241","endPage":"255","numberOfPages":"15","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":237251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210356,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jvolgeores.2004.12.011"}],"country":"United States","state":"Northern Mariana Islands","otherGeospatial":"Anatahan volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              145.623779296875,\n              16.325411207783855\n            ],\n            [\n              145.74188232421875,\n              16.325411207783855\n            ],\n            [\n              145.74188232421875,\n              16.375485785675078\n            ],\n            [\n              145.623779296875,\n              16.375485785675078\n            ],\n            [\n              145.623779296875,\n              16.325411207783855\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"146","issue":"1-3 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc30fe4b08c986b32af34","contributors":{"authors":[{"text":"Guffanti, M.","contributorId":75693,"corporation":false,"usgs":true,"family":"Guffanti","given":"M.","affiliations":[],"preferred":false,"id":415922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ewert, J.W.","contributorId":91885,"corporation":false,"usgs":true,"family":"Ewert","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":415924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gallina, G.M.","contributorId":105183,"corporation":false,"usgs":true,"family":"Gallina","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":415925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bluth, G.J.S.","contributorId":79258,"corporation":false,"usgs":true,"family":"Bluth","given":"G.J.S.","email":"","affiliations":[],"preferred":false,"id":415923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Swanson, G.L.","contributorId":42493,"corporation":false,"usgs":true,"family":"Swanson","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":415921,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}