{"pageNumber":"4232","pageRowStart":"105775","pageSize":"25","recordCount":184904,"records":[{"id":70016879,"text":"70016879 - 1992 - Abrupt uplift within the past 1700 years at southern Puget Sound, Washington","interactions":[],"lastModifiedDate":"2025-09-16T16:16:07.390858","indexId":"70016879","displayToPublicDate":"1992-12-04T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Abrupt uplift within the past 1700 years at southern Puget Sound, Washington","docAbstract":"<p><span>Shorelines rose as much as 7 meters along southern Puget Sound and Hood Canal between 500 and 1700 years ago. Evidence for this uplift consists of elevated wave-cut shore platforms near Seattle and emerged, peat-covered tidal flats as much as 60 kilometers to the southwest. The uplift was too rapid for waves to leave intermediate shorelines on even the best preserved platform. The tidal flats also emerged abruptly; they changed into freshwater swamps and meadows without first becoming tidal marshes. Where uplift was greatest, it adjoined an inferred fault that crosses Puget Sound at Seattle and it probably accompanied reverse slip on that fault 1000 to 1100 years ago. The uplift and probable fault slip show that the crust of the North America plate contains potential sources of damaging earthquakes in the Puget Sound region.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5088.1611","issn":"00368075","usgsCitation":"Bucknam, R., Hemphill-Haley, E., and Leopold, E.B., 1992, Abrupt uplift within the past 1700 years at southern Puget Sound, Washington: Science, v. 258, no. 5088, p. 1611-1614, https://doi.org/10.1126/science.258.5088.1611.","productDescription":"4 p.","startPage":"1611","endPage":"1614","costCenters":[],"links":[{"id":224900,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"southern Puget Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.40536936511256,\n              48.52482848310734\n            ],\n            [\n              -123.40536936511256,\n              47.0610802724176\n            ],\n            [\n              -122.17868034625329,\n              47.0610802724176\n            ],\n            [\n              -122.17868034625329,\n              48.52482848310734\n            ],\n            [\n              -123.40536936511256,\n              48.52482848310734\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"258","issue":"5088","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e647e4b0c8380cd472ed","contributors":{"authors":[{"text":"Bucknam, R.C.","contributorId":35744,"corporation":false,"usgs":true,"family":"Bucknam","given":"R.C.","affiliations":[],"preferred":false,"id":374742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemphill-Haley, E.","contributorId":69309,"corporation":false,"usgs":true,"family":"Hemphill-Haley","given":"E.","email":"","affiliations":[],"preferred":false,"id":374743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leopold, E. B.","contributorId":81162,"corporation":false,"usgs":true,"family":"Leopold","given":"E.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":374744,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016880,"text":"70016880 - 1992 - A tsunami about 1000 years ago in Puget Sound, Washington","interactions":[],"lastModifiedDate":"2025-09-16T16:22:38.910592","indexId":"70016880","displayToPublicDate":"1992-12-04T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"A tsunami about 1000 years ago in Puget Sound, Washington","docAbstract":"<p><span>Water surged from Puget Sound sometime between 1000 and 1100 years ago, overrunning tidal marshes and mantling them with centimeters of sand. One overrun site is 10 kilometers northwest of downtown Seattle; another is on Whidbey Island, some 30 kilometers farther north. Neither site has been widely mantled with sand at any other time in the past 2000 years. Deposition of the sand coincided—to the year or less—with abrupt, probably tectonic subsidence at the Seattle site and with landsliding into nearby Lake Washington. These findings show that a tsunami was generated in Puget Sound, and they tend to confirm that a large shallow earthquake occurred in the Seattle area about 1000 years ago.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5088.1614","issn":"00368075","usgsCitation":"Atwater, B., and Moore, A., 1992, A tsunami about 1000 years ago in Puget Sound, Washington: Science, v. 258, no. 5088, p. 1614-1617, https://doi.org/10.1126/science.258.5088.1614.","productDescription":"4 p.","startPage":"1614","endPage":"1617","costCenters":[],"links":[{"id":495739,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://zenodo.org/record/1231020","text":"External Repository"},{"id":224901,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.65886846523934,\n              49.00731757648293\n            ],\n            [\n              -123.65886846523934,\n              47.1048310775121\n            ],\n            [\n              -122.15457987611427,\n              47.1048310775121\n            ],\n            [\n              -122.15457987611427,\n              49.00731757648293\n            ],\n            [\n              -123.65886846523934,\n              49.00731757648293\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"258","issue":"5088","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e607e4b0c8380cd470f0","contributors":{"authors":[{"text":"Atwater, Brian F. atwater@usgs.gov","contributorId":149872,"corporation":false,"usgs":true,"family":"Atwater","given":"Brian F.","email":"atwater@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":374745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, A.L.","contributorId":70931,"corporation":false,"usgs":true,"family":"Moore","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":374746,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016878,"text":"70016878 - 1992 - Prehistoric rock avalanches in the Olympic Mountains, Washington","interactions":[],"lastModifiedDate":"2025-09-16T16:28:41.919201","indexId":"70016878","displayToPublicDate":"1992-12-04T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Prehistoric rock avalanches in the Olympic Mountains, Washington","docAbstract":"<p><span>Rock avalanches blocked streams in the Olympic Mountains southwest of Puget Sound during the past few thousand years. Limiting radiocarbon ages indicated that three or four of six avalanches occurred from 1000 to 1300 years ago or shortly thereafter. Most of the dates were from the outer preserved rings of trees drowned behind avalanche dams. These three or four avalanches may be coeval not only with one another but also with abrupt tectonic deformation in western Washington. No rock avalanches in the Olympic Mountains are known to have resulted from storms or earthquakes during the past century. The avalanches strengthen the case that a large prehistoric earthquake occurred in the Puget Sound region.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5088.1620","issn":"00368075","usgsCitation":"Schuster, R.L., Logan, R., and Pringle, P.T., 1992, Prehistoric rock avalanches in the Olympic Mountains, Washington: Science, v. 258, no. 5088, p. 1620-1621, https://doi.org/10.1126/science.258.5088.1620.","productDescription":"2 p.","startPage":"1620","endPage":"1621","costCenters":[],"links":[{"id":224857,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Olympic Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.39793161959817,\n              48.21488770425793\n            ],\n            [\n              -124.39793161959817,\n              47.36117002213089\n            ],\n            [\n              -122.77803533045658,\n              47.36117002213089\n            ],\n            [\n              -122.77803533045658,\n              48.21488770425793\n            ],\n            [\n              -124.39793161959817,\n              48.21488770425793\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"258","issue":"5088","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8227e4b0c8380cd7b93c","contributors":{"authors":[{"text":"Schuster, R. L.","contributorId":19135,"corporation":false,"usgs":true,"family":"Schuster","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":374739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Logan, R.L.","contributorId":23283,"corporation":false,"usgs":true,"family":"Logan","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":374740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pringle, P. T.","contributorId":39806,"corporation":false,"usgs":true,"family":"Pringle","given":"P.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":374741,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70169037,"text":"70169037 - 1992 - Herbicide and nitrate variation in alluvium underlying a cornfield at a site in Iowa County, Iowa","interactions":[],"lastModifiedDate":"2016-03-11T16:02:13","indexId":"70169037","displayToPublicDate":"1992-12-01T17:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Herbicide and nitrate variation in alluvium underlying a cornfield at a site in Iowa County, Iowa","docAbstract":"<p><span>A hydrologic investigation to determine vertical and seasonal variation of atrazine, alachlor, cyanazine, and nitrate at one location and to relate the variation to ground-water movement in the Iowa River alluvium was conducted in Iowa County, Iowa, from March 1986 to December 1987. Water samples were collected at discrete intervals through the alluvial sequence from the soil zone to the base of the aquifer. Alachlor, atrazine, and cyanazine were detected most frequently in the soil zone but also were present in the upper part of the alluvial aquifer. Alachlor was detected sporadically, whereas, atrazine, cyanazine, and nitrate were present throughout the year. In the alluvial aquifer, the herbicides generally were not detected during 1986 and were present in detectable concentrations for only a short period of time in the upper 1.6 meters of the aquifer during 1987. Nitrate was present throughout the alluvium and was stratified in the alluvial aquifer. The largest nitrate concentrations were detected in the middle part of the aquifer. Nitrate concentrations were variable only in the upper 2 meters of the aquifer. Vertical movement of herbicides and nitrate in the soil correlated with precipitation and degree of saturation. A clay layer retarded vertical movement of atrazine but not nitrate from the soil layer to the aquifer. Vertical movement could not account for the chemical variation in the alluvial aquifer.</span></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1752-1688.1992.tb04012.x","usgsCitation":"Kalkhoff, S., Detroy, M., Cherryholmes, K., and Kuzniar, R., 1992, Herbicide and nitrate variation in alluvium underlying a cornfield at a site in Iowa County, Iowa: Journal of the American Water Resources Association, v. 28, no. 6, p. 1001-1011, https://doi.org/10.1111/j.1752-1688.1992.tb04012.x.","productDescription":"11 p.","startPage":"1001","endPage":"1011","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","county":"Iowa County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.8318,41.8617],[-91.8327,41.775],[-91.8335,41.6865],[-91.8337,41.6006],[-91.827,41.6001],[-91.8291,41.5116],[-91.9463,41.5108],[-92.0659,41.5104],[-92.183,41.5098],[-92.2995,41.5096],[-92.2986,41.6008],[-92.3017,41.6008],[-92.3014,41.6889],[-92.2999,41.7765],[-92.299,41.8623],[-92.1832,41.8626],[-92.066,41.8627],[-91.949,41.8618],[-91.8318,41.8617]]]},\"properties\":{\"name\":\"Iowa\",\"state\":\"IA\"}}]}","volume":"28","issue":"6","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"56e3fa4fe4b0f59b85d49444","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":622648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detroy, M.G.","contributorId":6066,"corporation":false,"usgs":true,"family":"Detroy","given":"M.G.","affiliations":[],"preferred":false,"id":622649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cherryholmes, K.","contributorId":67672,"corporation":false,"usgs":true,"family":"Cherryholmes","given":"K.","email":"","affiliations":[],"preferred":false,"id":622650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kuzniar, R.L.","contributorId":44558,"corporation":false,"usgs":true,"family":"Kuzniar","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":622651,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70127584,"text":"70127584 - 1992 - Descriptive risk assessment of the effects of acidic deposition on Rocky Mountain amphibians","interactions":[],"lastModifiedDate":"2014-09-30T12:43:16","indexId":"70127584","displayToPublicDate":"1992-12-01T12:41:36","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Descriptive risk assessment of the effects of acidic deposition on Rocky Mountain amphibians","docAbstract":"We evaluated the risk of habitat acidification to the six species of amphibians that occur in the mountains of Colorado and Wyoming. Our evaluation included extrinsic environmental factors (habitat sensitivity and amount of acidic atmospheric deposition) and species-specific intrinsic factors (sensitivity to acid conditions, habitat preferences, and timing of breeding). Only one of 57 surveyed localities had both acid neutralizing capacity <200 <i>μ</i>eq/L and sulfate deposition >10 kg/ha/yr, extrinsic conditions with a possible risk of acidification. Amphibian breeding habitats in the Rocky Mountains do not appear to be sufficiently acidic to kill amphibian embryos. Some species breed in high-elevation vernal pools during snowmelt, and an acidic pulse during snowmelt may pose a risk to embryos of these species. However, the acidic pulse, if present, probably occurs before open water appears and before breeding begins. Although inherent variability of amphibian population size may make detection of declines from anthropogenic effects difficult, acidic deposition is unlikely to have caused the observed declines of <i>Bufo boreas</i> and <i>Rana pipiens</i> in Colorado and Wyoming. Amphibians in the Rocky Mountains are not likely to be at risk with acidification inputs at present levels.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for the Study of Amphibians and Reptiles","publisherLocation":"Athens, OH","doi":"10.2307/1565112","usgsCitation":"Corn, P., and Vertucci, F.A., 1992, Descriptive risk assessment of the effects of acidic deposition on Rocky Mountain amphibians: Journal of Herpetology, v. 26, no. 4, p. 361-369, https://doi.org/10.2307/1565112.","productDescription":"9 p.","startPage":"361","endPage":"369","numberOfPages":"9","costCenters":[],"links":[{"id":294648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294647,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1565112"}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542bc62ae4b0abfb4c809781","contributors":{"authors":[{"text":"Corn, Paul Stephen 0000-0002-4106-6335","orcid":"https://orcid.org/0000-0002-4106-6335","contributorId":107379,"corporation":false,"usgs":true,"family":"Corn","given":"Paul Stephen","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":502459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vertucci, Frank A.","contributorId":57388,"corporation":false,"usgs":true,"family":"Vertucci","given":"Frank","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":502458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70209660,"text":"70209660 - 1992 - Role of chemical change in the paleomagnetic record","interactions":[],"lastModifiedDate":"2020-04-20T15:57:27.298119","indexId":"70209660","displayToPublicDate":"1992-12-01T10:53:02","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"Role of chemical change in the paleomagnetic record","docAbstract":"<p><span>To produce an outline of how either to isolate or capitalize on changes in magnetic properties resulting from chemical changes, the workshop, “Effects of Chemical Changes on Magnetization,” was held in Santa Fe, N. Mex. from August 13 to 16. It was sponsored by the Institute for Rock Magnetism (IRM) in Minneapolis, Minn., and funded by the National Science Foundation. Graduate students and established researchers in rockand paleomagnetism, mostly from the United States and Canada, participated. Ian McGregor and Mike Mayhew represented NSF. A special feature of the conference was five guest speakers from outside the field of rock magnetism who bridged the gap between chemistry and magnetism.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/91EO00385","usgsCitation":"Banerjee, S., and Reynolds, R.L., 1992, Role of chemical change in the paleomagnetic record: Eos, Earth and Space Science News, v. 73, no. 48, p. 519-520, https://doi.org/10.1029/91EO00385.","productDescription":"2 p.","startPage":"519","endPage":"520","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374116,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"48","noUsgsAuthors":false,"publicationDate":"2006-10-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Banerjee, S.","contributorId":74606,"corporation":false,"usgs":true,"family":"Banerjee","given":"S.","email":"","affiliations":[],"preferred":false,"id":787426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787427,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70243288,"text":"70243288 - 1992 - Comment on “222Rn Premonitory signals for earthquakes?”","interactions":[],"lastModifiedDate":"2023-05-05T15:23:55.731599","indexId":"70243288","displayToPublicDate":"1992-12-01T10:08:08","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7458,"text":"Eos Science News","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Comment on “<sup>222</sup>Rn Premonitory signals for earthquakes?”","title":"Comment on “222Rn Premonitory signals for earthquakes?”","docAbstract":"<p><span>Radon and other terrestrial gases in groundwater and soil air have been studied in recent years in seismically active areas, especially in China, Japan, the former Soviet Union, and the United States, in search of changes that may be useful for earthquake prediction. Concentrations of radon, helim, hydrogen, mercury vapor, carbon dioxide, and several other gases have been found to be high along active faults. Faults may thus be paths of least resistance along which terrestrial gases generated or stored in the Earth can escape into the atmosphere. Gas-concentration changes with durations of hours to months have been observed before and after earthquakes at relatively few favorably situated sites, and their patterns have not always been repeated. Some of these sites are located as far as several hundred kilometers away from earthquake epicenters. These “sensitive” sites are generally situated along active faults, whether the seismogenic ones or not, especially at their intersections or bends, or at other structurally weak zones, possibly because of concentration of tectonic strain and abundance of pore fluids at such places (see review papers by </span><i>King</i><span>, 1986, 1990). Due to this selectivity and for two other important reasons, studies of terrestrial gases for earthquake prediction have not been viewed favorably by most geophysicists, especially those in the United States.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/91EO00382","usgsCitation":"King, C., 1992, Comment on “222Rn Premonitory signals for earthquakes?”: Eos Science News, v. 73, no. 48, p. 517-518, https://doi.org/10.1029/91EO00382.","productDescription":"2 p.","startPage":"517","endPage":"518","costCenters":[],"links":[{"id":416765,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"48","noUsgsAuthors":false,"publicationDate":"2006-10-19","publicationStatus":"PW","contributors":{"authors":[{"text":"King, Chi-Yu","contributorId":49355,"corporation":false,"usgs":true,"family":"King","given":"Chi-Yu","email":"","affiliations":[],"preferred":false,"id":871861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003139,"text":"1003139 - 1992 - Classification of a wetland area along the upper Mississippi River with aerial videography","interactions":[],"lastModifiedDate":"2026-04-27T17:34:35.086856","indexId":"1003139","displayToPublicDate":"1992-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Classification of a wetland area along the upper Mississippi River with aerial videography","docAbstract":"<p><span>We evaluated the use of aerial videography for classifying wetland habitats along the upper Mississippi River and found the prompt availability of habitat feature maps to be the major advantage of the video imagery technique. We successfully produced feature maps from digitized video images that generally agreed with the known distribution and areal coverages of the major habitat types independently identified and quantified with photointerpretation techniques. However, video images were not sufficiently detailed to allow us to consistently discriminate among the classes of aquatic macrophytes present or to quantify their areal coverage. Our inability to consistently distinguish among emergent, floating, and submergent macrophytes from the feature maps may have been related to the structural complexity of the site, to our limited vegetation sampling, and to limitations in video imagery. We expect that careful site selection (i.e., the desired level of resolution is available from video imagery) and additional vegetation samples (e.g., along a transect) will allow improved assignment of spectral values to specific plant types and enhance plant classification from feature maps produced from video imagery.</span></p>","language":"English","publisher":"Springer Nature","doi":"10.1007/BF03160605","issn":"02775212","usgsCitation":"Jennings, C., Vohs, P., and Dewey, M.R., 1992, Classification of a wetland area along the upper Mississippi River with aerial videography: Wetlands, v. 12, no. 3, p. 163-170, https://doi.org/10.1007/BF03160605.","productDescription":"8 p.","startPage":"163","endPage":"170","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":133968,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Mississippi River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.91582109389182,\n              45.14621818801862\n            ],\n            [\n              -91.15321296418284,\n              41.88646796569946\n            ],\n            [\n              -91.72896027552285,\n              39.63440645907387\n            ],\n            [\n              -90.23622649306111,\n              36.363977833515634\n            ],\n            [\n              -92.03511775106587,\n              31.58923553653029\n            ],\n            [\n              -91.16842459726436,\n              29.495622458893266\n            ],\n            [\n              -89.91354630680497,\n              29.479659759855167\n            ],\n            [\n              -90.5381119064338,\n              31.367663697923973\n            ],\n            [\n              -89.24468703654418,\n              36.822670925119034\n            ],\n            [\n              -90.44680936281772,\n              39.8744053695478\n            ],\n            [\n              -89.89154502748079,\n              42.26677338595079\n            ],\n            [\n              -91.27141127890772,\n              45.283316378812\n            ],\n            [\n              -92.91582109389182,\n              45.14621818801862\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de142","contributors":{"authors":[{"text":"Jennings, Cecil A.","contributorId":38504,"corporation":false,"usgs":true,"family":"Jennings","given":"Cecil A.","affiliations":[],"preferred":false,"id":312812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vohs, P.A.","contributorId":64621,"corporation":false,"usgs":true,"family":"Vohs","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":312814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dewey, M. R.","contributorId":48908,"corporation":false,"usgs":true,"family":"Dewey","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":312813,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1001320,"text":"1001320 - 1992 - Effects of irrigation on seed production and vegetative characteristics of four moist-soil plants on impounded wetlands in California","interactions":[],"lastModifiedDate":"2026-04-27T17:39:38.60244","indexId":"1001320","displayToPublicDate":"1992-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Effects of irrigation on seed production and vegetative characteristics of four moist-soil plants on impounded wetlands in California","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>We examined the effects of irrigation on 4 moist-soil plants commonly managed for waterfowl in the Sacramento Valley, California. Irrigation resulted in taller and heavier swamp timothy (</span><i>Heleochloa schoenoides</i><span>), pricklegrass (</span><i>Crypsis niliaca</i><span>), and sprangletop (</span><i>Leptochloa fasicularis</i><span>). Barnyardgrass (</span><i>Echinochloa crusgalli</i><span>) grew taller in irrigated wetlands, but no significant difference in weight was detected. Only sprangletop yielded larger seed masses in response to irrigation. Without irrigation, swamp timothy and pricklegrass assumed a typical prostrate growth form, but with irrigation, they assumed a vertical growth form. Irrigation did not significantly affect plant density. Because of rising water costs, wetland managers should consider wildlife management objectives and plant responses before implementing irrigation practices.</span></span></p>","language":"English","publisher":"Springer Nature","doi":"10.1007/BF03160610","usgsCitation":"Mushet, D., Euliss, N., and Harris, S., 1992, Effects of irrigation on seed production and vegetative characteristics of four moist-soil plants on impounded wetlands in California: Wetlands, v. 12, no. 3, p. 204-207, https://doi.org/10.1007/BF03160610.","productDescription":"4 p.","startPage":"204","endPage":"207","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133758,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.37910254578382,\n              39.822500523112154\n            ],\n            [\n              -122.37910254578382,\n              38.107108797177375\n            ],\n            [\n              -120.84482767834879,\n              38.107108797177375\n            ],\n            [\n              -120.84482767834879,\n              39.822500523112154\n            ],\n            [\n              -122.37910254578382,\n              39.822500523112154\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611de0","contributors":{"authors":[{"text":"Mushet, D.M. 0000-0002-5910-2744","orcid":"https://orcid.org/0000-0002-5910-2744","contributorId":59377,"corporation":false,"usgs":true,"family":"Mushet","given":"D.M.","affiliations":[],"preferred":false,"id":310876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Euliss, N.H. Jr.","contributorId":54917,"corporation":false,"usgs":true,"family":"Euliss","given":"N.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":310875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, S.W.","contributorId":66201,"corporation":false,"usgs":true,"family":"Harris","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":310877,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185759,"text":"70185759 - 1992 - Deposition of aerially applied BT in an oak forest and its prediction with the FSCBG model","interactions":[],"lastModifiedDate":"2019-03-07T07:26:47","indexId":"70185759","displayToPublicDate":"1992-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2168,"text":"Journal of Applied Meteorology","active":true,"publicationSubtype":{"id":10}},"title":"Deposition of aerially applied BT in an oak forest and its prediction with the FSCBG model","docAbstract":"<p>Data are provided from 17 single-swath aerial spray trials that were conducted over a fully leafed, 16-m tall, mixed oak forest. The distribution of cross-swath spray deposits was sampled at the top of the canopy and below the canopy. Micrometeorological conditions were measured above and within the canopy during the spray trials. The USDA Forest Service FSCBG (Forest Service-Cramer-Barry-Grim) model was run to predict the target sampler catch for each trial using forest stand, airplane-application-equipment configuration, and micrometeorological conditions as inputs. Observations showed an average cross-swath deposition of 100 IU cm<sup>−2</sup> with large run-to-run variability in deposition patterns, magnitudes, and drift. Eleven percent of the spray material that reached the top of the canopy penetrated through the tree canopy to the forest floor.</p><p>The FSCBG predictions of the ensemble-averaged deposition were within 17% of the measured deposition at the canopy top and within 8% on the ground beneath the canopy. Run-to-run deposit predictions by FSCBG were considerably less variable than the measured deposits. Individual run predictions were much less accurate than the ensemble-averaged predictions as demonstrated by an average root-mean-square-error (rmse) of 27.9 IU CM<sup>−2</sup> at the top of the canopy. Comparisons of the differences between predicted and observed deposits indicated that the model accuracy was sensitive to atmospheric stability conditions. In neutral and stable conditions, a regular pattern of error was indicated by overprediction of the canopy-top deposit at distances from 0 to 20 m downwind from the flight line and underprediction of the deposit both farther downwind than 20 m and upwind of the flight line. In unstable conditions the model generally underpredicted the deposit downwind from the flight line, but showed no regular pattern of error.</p>","language":"English","publisher":"American Meteorological Society ","doi":"10.1175/1520-0450(1992)031<1457:DOAABI>2.0.CO;2","usgsCitation":"Anderson, D.E., Miller, D.R., Wang, Y., Yendol, W.G., Mierzejewski, K., and McManus, M.L., 1992, Deposition of aerially applied BT in an oak forest and its prediction with the FSCBG model: Journal of Applied Meteorology, v. 31, p. 1457-1466, https://doi.org/10.1175/1520-0450(1992)031<1457:DOAABI>2.0.CO;2.","productDescription":"10 p. ","startPage":"1457","endPage":"1466","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479562,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/1520-0450(1992)031<1457:doaabi>2.0.co;2","text":"Publisher Index Page"},{"id":338506,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","noUsgsAuthors":true,"publicationStatus":"PW","scienceBaseUri":"58db7639e4b0ee37af29e4ec","contributors":{"authors":[{"text":"Anderson, Dean E. deander@usgs.gov","contributorId":662,"corporation":false,"usgs":true,"family":"Anderson","given":"Dean","email":"deander@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":686684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, David R.","contributorId":189614,"corporation":false,"usgs":false,"family":"Miller","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":686685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wang, Yansen","contributorId":189613,"corporation":false,"usgs":false,"family":"Wang","given":"Yansen","email":"","affiliations":[],"preferred":false,"id":686686,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yendol, William G.","contributorId":189987,"corporation":false,"usgs":false,"family":"Yendol","given":"William","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":686687,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mierzejewski, Karl","contributorId":189988,"corporation":false,"usgs":false,"family":"Mierzejewski","given":"Karl","email":"","affiliations":[],"preferred":false,"id":686688,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McManus, Michael L.","contributorId":189612,"corporation":false,"usgs":false,"family":"McManus","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":686689,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70016800,"text":"70016800 - 1992 - High resolution late Pliocene sea-surface temperature record from the northeast Atlantic Ocean","interactions":[],"lastModifiedDate":"2024-09-30T17:54:57.44756","indexId":"70016800","displayToPublicDate":"1992-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"High resolution late Pliocene sea-surface temperature record from the northeast Atlantic Ocean","docAbstract":"<p><span>Application of quantitative micropaleontologic methods of sea-surface temperature (SST) estimation to the planktic foraminiferal faunas at Hole 548 in the northeast Atlantic between 3.5 and 2.0 Ma provide a detailed record of Pliocene surface temperature changes during the onset of major Northern Hemisphere glaciation. SST estimates indicate a relatively warm interval of “enhanced interglacials (warm peaks)” between 3.2 and 2.8 Ma followed by steady cooling with a significant step-like change toward colder temperatures occurring about 2.4 Ma. This record compares well with faunal and SST records from other North Atlantic sites.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0377-8398(92)90001-Z","usgsCitation":"Dowsett, H.J., and Loubere, P., 1992, High resolution late Pliocene sea-surface temperature record from the northeast Atlantic Ocean: Marine Micropaleontology, v. 20, no. 2, p. 91-105, https://doi.org/10.1016/0377-8398(92)90001-Z.","productDescription":"15 p.","startPage":"91","endPage":"105","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":224559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a30cae4b0c8380cd5d954","contributors":{"authors":[{"text":"Dowsett, Harry J. 0000-0003-1983-7524","orcid":"https://orcid.org/0000-0003-1983-7524","contributorId":269579,"corporation":false,"usgs":true,"family":"Dowsett","given":"Harry","email":"","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":374530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loubere, P.","contributorId":87697,"corporation":false,"usgs":true,"family":"Loubere","given":"P.","email":"","affiliations":[],"preferred":false,"id":374529,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016992,"text":"70016992 - 1992 - Change in failure stress on the southern San Andreas fault system caused by the 1992 magnitude = 7.4 Landers earthquake","interactions":[],"lastModifiedDate":"2025-09-16T16:38:35.657352","indexId":"70016992","displayToPublicDate":"1992-11-20T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Change in failure stress on the southern San Andreas fault system caused by the 1992 magnitude = 7.4 Landers earthquake","docAbstract":"The 28 June Landers earthquake brought the San Andreas fault significantly closer to failure near San Bernardino, a site that has not sustained a large shock since 1812. Stress also increased on the San Jacinto fault near San Bernardino and on the San Andreas fault southeast of Palm Springs. Unless creep or moderate earthquakes relieve these stress changes, the next great earthquake on the southern San Andreas fault is likely to be advanced by one to two decades. In contrast, stress on the San Andreas north of Los Angeles dropped, potentially delaying the next great earthquake there by 2 to 10 years.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5086.1328","issn":"00368075","usgsCitation":"Stein, R., King, G., and Lin, J., 1992, Change in failure stress on the southern San Andreas fault system caused by the 1992 magnitude = 7.4 Landers earthquake: Science, v. 258, no. 5086, p. 1328-1332, https://doi.org/10.1126/science.258.5086.1328.","productDescription":"5 p.","startPage":"1328","endPage":"1332","costCenters":[],"links":[{"id":225144,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"southern San Andreas fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.88802485821637,\n              34.614637166226984\n            ],\n            [\n              -118.88802485821637,\n              33.46807014457141\n            ],\n            [\n              -115.48694411992896,\n              33.46807014457141\n            ],\n            [\n              -115.48694411992896,\n              34.614637166226984\n            ],\n            [\n              -118.88802485821637,\n              34.614637166226984\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"258","issue":"5086","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f401e4b0c8380cd4baa2","contributors":{"authors":[{"text":"Stein, R.S.","contributorId":8875,"corporation":false,"usgs":true,"family":"Stein","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":375068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, G.C.P.","contributorId":18510,"corporation":false,"usgs":true,"family":"King","given":"G.C.P.","email":"","affiliations":[],"preferred":false,"id":375069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lin, J.","contributorId":33065,"corporation":false,"usgs":true,"family":"Lin","given":"J.","email":"","affiliations":[],"preferred":false,"id":375070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016993,"text":"70016993 - 1992 - Changes in static stress on southern California faults after the 1992 Landers earthquake","interactions":[],"lastModifiedDate":"2025-05-28T15:23:33.011107","indexId":"70016993","displayToPublicDate":"1992-11-19T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Changes in static stress on southern California faults after the 1992 Landers earthquake","docAbstract":"<p><span>The magnitude 7.5 Landers earthquake of 28 June 1992 was the largest earthquake to strike California in 40 years. The slip that occurs in such an earthquake would be expected to induce large changes in the static stress on neighbouring faults; these changes in stress should in turn affect the likelihood of future earthquakes. Stress changes that load faults towards failure have been cited as the cause of small</span><sup>1–5</sup><span>, moderate</span><sup>6</sup><span>&nbsp;and large</span><sup>7</sup><span>&nbsp;earthquakes; conversely, those that relax neighbouring faults have been related to a decrease in seismicity</span><sup>5</sup><span>. Here we use an elastic half-space model</span><sup>8</sup><span>&nbsp;to estimate the stress changes produced by the Landers earthquake on selected southern California faults, including the San Andreas. We find that the estimated stress changes are consistent with the triggering of four out of the five aftershocks with magnitude greater than 4.5, and that the largest changes (1–10 bar), occurring on part of the San Bernardino segment of the San Andreas fault, may have decreased the time to the next magnitude 8 earthquake by about 14 years.</span></p>","language":"English","publisher":"Springer Nature","doi":"10.1038/360251a0","issn":"00280836","usgsCitation":"Harris, R., and Simpson, R., 1992, Changes in static stress on southern California faults after the 1992 Landers earthquake: Nature, v. 360, no. 6401, p. 251-254, https://doi.org/10.1038/360251a0.","productDescription":"4 p.","startPage":"251","endPage":"254","costCenters":[],"links":[{"id":225145,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"southern California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.84276576650728,\n              35.04814633651593\n            ],\n            [\n              -120.84276576650728,\n              32.676049044840994\n            ],\n            [\n              -114.43216994056223,\n              32.676049044840994\n            ],\n            [\n              -114.43216994056223,\n              35.04814633651593\n            ],\n            [\n              -120.84276576650728,\n              35.04814633651593\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"360","issue":"6401","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f426e4b0c8380cd4bb8b","contributors":{"authors":[{"text":"Harris, R.A. 0000-0002-9247-0768","orcid":"https://orcid.org/0000-0002-9247-0768","contributorId":41849,"corporation":false,"usgs":true,"family":"Harris","given":"R.A.","affiliations":[],"preferred":false,"id":375071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simpson, R.W.","contributorId":76738,"corporation":false,"usgs":true,"family":"Simpson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":375072,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216448,"text":"70216448 - 1992 - The determination and fate of unstable constituents in contaminated ground water","interactions":[],"lastModifiedDate":"2020-11-18T15:04:01.209816","indexId":"70216448","displayToPublicDate":"1992-11-18T09:01:12","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The determination and fate of unstable constituents in contaminated ground water","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Groundwater quality and analysis at hazardous waste sites","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Marcel Dekker, Inc.","usgsCitation":"Baedecker, M.J., and Cozzarelli, I.M., 1992, The determination and fate of unstable constituents in contaminated ground water, chap. <i>of</i> Groundwater quality and analysis at hazardous waste sites, p. 425-461.","productDescription":"37 p.","startPage":"425","endPage":"461","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":380596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Baedecker, Mary Jo 0000-0002-4865-1043 mjbaedec@usgs.gov","orcid":"https://orcid.org/0000-0002-4865-1043","contributorId":197793,"corporation":false,"usgs":true,"family":"Baedecker","given":"Mary","email":"mjbaedec@usgs.gov","middleInitial":"Jo","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":805146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true}],"preferred":true,"id":805147,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016994,"text":"70016994 - 1992 - Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene","interactions":[],"lastModifiedDate":"2025-09-16T16:43:17.248068","indexId":"70016994","displayToPublicDate":"1992-11-13T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene","docAbstract":"<p><span>The Middle Pliocene (∼3 million years ago) has been identified as the last time the Earth was significantly warmer than it was during the Last Interglacial and Holocene. A quantitative micropaleontological paleotemperature transect from equator to high latitudes in the North Atlantic indicates that Middle Pliocene warmth involved increased meridional oceanic heat transport.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5085.1133","issn":"00368075","usgsCitation":"Dowsett, H., Cronin, T.M., Poore, R., Thompson, R., Whatley, R., and Wood, A., 1992, Micropaleontological evidence for increased meridional heat transport in the North Atlantic Ocean during the pliocene: Science, v. 258, no. 5085, p. 1133-1135, https://doi.org/10.1126/science.258.5085.1133.","productDescription":"3 p.","startPage":"1133","endPage":"1135","costCenters":[],"links":[{"id":225146,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"258","issue":"5085","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a568fe4b0c8380cd6d690","contributors":{"authors":[{"text":"Dowsett, H.J. 0000-0003-1983-7524","orcid":"https://orcid.org/0000-0003-1983-7524","contributorId":87924,"corporation":false,"usgs":true,"family":"Dowsett","given":"H.J.","affiliations":[],"preferred":false,"id":375077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cronin, T. M. 0000-0002-2643-0979","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":42613,"corporation":false,"usgs":true,"family":"Cronin","given":"T.","email":"","middleInitial":"M.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":false,"id":375075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":375074,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, R.S.","contributorId":106516,"corporation":false,"usgs":true,"family":"Thompson","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":375078,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Whatley, R.C.","contributorId":85211,"corporation":false,"usgs":true,"family":"Whatley","given":"R.C.","affiliations":[],"preferred":false,"id":375076,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wood, A.M.","contributorId":34271,"corporation":false,"usgs":true,"family":"Wood","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":375073,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70017246,"text":"70017246 - 1992 - A prediction of Mars seismicity from surface faulting","interactions":[],"lastModifiedDate":"2025-09-16T16:52:22.3581","indexId":"70017246","displayToPublicDate":"1992-11-06T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"A prediction of Mars seismicity from surface faulting","docAbstract":"<p><span>The shallow seismicity of Mars has been estimated by measurement of the total slip on faults visible on the surface of the planet throughout geologic time. Seismicity was calibrated with estimates based on surface structures on the moon and measured lunar seismicity that includes the entire seismogenic lithosphere. Results indicate that Mars is seismically active today, with a sufficient number of detectable marsquakes to allow seismic investigations of its interior.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.258.5084.979","issn":"00368075","usgsCitation":"Golombek, M., Banerdt, W., Tanaka, K.L., and Tralli, D., 1992, A prediction of Mars seismicity from surface faulting: Science, v. 258, no. 5084, p. 979-981, https://doi.org/10.1126/science.258.5084.979.","productDescription":"3 p.","startPage":"979","endPage":"981","costCenters":[],"links":[{"id":224968,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"258","issue":"5084","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4eae4b0c8380cd46a0d","contributors":{"authors":[{"text":"Golombek, M.P.","contributorId":52696,"corporation":false,"usgs":true,"family":"Golombek","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":375881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banerdt, W.B.","contributorId":36684,"corporation":false,"usgs":true,"family":"Banerdt","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":375880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":375879,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tralli, D.M.","contributorId":65234,"corporation":false,"usgs":true,"family":"Tralli","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":375882,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70127592,"text":"70127592 - 1992 - Dynamic land surface/atmospheric parameterization for the South Platte River drainage","interactions":[],"lastModifiedDate":"2014-09-30T13:04:51","indexId":"70127592","displayToPublicDate":"1992-11-05T13:02:09","publicationYear":"1992","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Dynamic land surface/atmospheric parameterization for the South Platte River drainage","docAbstract":"No abstract available.","largerWorkTitle":"AWRA Symposium Proceedings: Managing water resources during global change","conferenceTitle":"AWRA Symposium Proceedings: Managing water resources during global change","conferenceDate":"1992-11-01T00:00:00","conferenceLocation":"Reno, NV","language":"English","publisher":"American Water Resources Association","publisherLocation":"Bethesda, MD","usgsCitation":"Baron, J., Pielke, R., Parton, W., Ojima, D., Kirchner, T., Running, S.W., and Kittel, T., 1992, Dynamic land surface/atmospheric parameterization for the South Platte River drainage, 10 p.","productDescription":"10 p.","numberOfPages":"10","costCenters":[],"links":[{"id":294653,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"South Platte River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.3188,40.9416 ], [ -102.3188,41.1551 ], [ -100.6757,41.1551 ], [ -100.6757,40.9416 ], [ -102.3188,40.9416 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542bc62fe4b0abfb4c8097b5","contributors":{"authors":[{"text":"Baron, Jill S. 0000-0002-5902-6251 jill_baron@usgs.gov","orcid":"https://orcid.org/0000-0002-5902-6251","contributorId":822,"corporation":false,"usgs":true,"family":"Baron","given":"Jill S.","email":"jill_baron@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":502478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pielke, R.A.","contributorId":56814,"corporation":false,"usgs":true,"family":"Pielke","given":"R.A.","affiliations":[],"preferred":false,"id":502482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parton, W.J.","contributorId":89685,"corporation":false,"usgs":true,"family":"Parton","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":502483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ojima, D.S.","contributorId":49549,"corporation":false,"usgs":true,"family":"Ojima","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":502480,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kirchner, T.B.","contributorId":97330,"corporation":false,"usgs":true,"family":"Kirchner","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":502484,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Running, S. W.","contributorId":51257,"corporation":false,"usgs":false,"family":"Running","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":502481,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kittel, T.G.F.","contributorId":21500,"corporation":false,"usgs":true,"family":"Kittel","given":"T.G.F.","email":"","affiliations":[],"preferred":false,"id":502479,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70127887,"text":"70127887 - 1992 - Influence of landscape structure on the hydrologic cycle and regional and global climate","interactions":[],"lastModifiedDate":"2018-02-21T15:52:46","indexId":"70127887","displayToPublicDate":"1992-11-05T10:21:00","publicationYear":"1992","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Influence of landscape structure on the hydrologic cycle and regional and global climate","docAbstract":"No abstract available.","largerWorkTitle":"Influence of Landscape Structure on the Hydrologic Cycle and Regional and Global Climate: AWRA Symposium on Managing Water Resources During Global Change","conferenceTitle":"Influence of Landscape Structure on the Hydrologic Cycle and Regional and Global Climate: AWRA Symposium on Managing Water Resources During Global Change","conferenceDate":"1992-11-01T00:00:00","conferenceLocation":"Reno, NV","language":"English","publisher":"American Water Resources Association","publisherLocation":"Bethesda, MD","usgsCitation":"Pielke, R.A., Baron, J., Kittel, T.G., Lee, T.J., Chase, T.N., and Cram, J.M., 1992, Influence of landscape structure on the hydrologic cycle and regional and global climate, 14 p.","productDescription":"14 p.","numberOfPages":"14","costCenters":[],"links":[{"id":294776,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542e6964e4b092f17df5a8be","contributors":{"authors":[{"text":"Pielke, R. A.","contributorId":13163,"corporation":false,"usgs":true,"family":"Pielke","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":502596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baron, Jill 0000-0002-5902-6251 jill_baron@usgs.gov","orcid":"https://orcid.org/0000-0002-5902-6251","contributorId":194124,"corporation":false,"usgs":true,"family":"Baron","given":"Jill","email":"jill_baron@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":502599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kittel, Timothy G.F.","contributorId":66612,"corporation":false,"usgs":true,"family":"Kittel","given":"Timothy","email":"","middleInitial":"G.F.","affiliations":[],"preferred":false,"id":502600,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lee, T. J.","contributorId":26234,"corporation":false,"usgs":true,"family":"Lee","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":502597,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chase, T. N.","contributorId":30927,"corporation":false,"usgs":true,"family":"Chase","given":"T.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":502598,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cram, J. M.","contributorId":78260,"corporation":false,"usgs":true,"family":"Cram","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":502601,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1476,"text":"1476 - 1992 - Guide to preparing illustrations","interactions":[],"lastModifiedDate":"2014-07-11T14:54:52","indexId":"1476","displayToPublicDate":"1992-11-01T14:53:06","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Guide to preparing illustrations","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/1476","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Guide to preparing illustrations, iii, 5 p., https://doi.org/10.3133/1476.","productDescription":"iii, 5 p.","numberOfPages":"8","costCenters":[],"links":[{"id":289810,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c0ec3ee4b065ccca5fe3b9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70126968,"text":"70126968 - 1992 - Resilience of a heavily logged grove of giant sequoia (<i>Sequoiadendron giganteum</i>) in Kings Canyon National Park, California","interactions":[],"lastModifiedDate":"2014-09-25T11:46:30","indexId":"70126968","displayToPublicDate":"1992-11-01T11:43:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Resilience of a heavily logged grove of giant sequoia (<i>Sequoiadendron giganteum</i>) in Kings Canyon National Park, California","docAbstract":"The Big Stump Grove of giant sequoia (<i>Sequoiadendron giganteum</i> (Lindl.) Buchholz) was heavily logged between 1883 and 1889 and the stand naturally regenerated from seed following logging. In 1968, as part of a 100% sequoia tree inventory, all living sequoias (<i>n</i> = 3587) and dead trees and stumps (<i>n</i>=588) were measured (diameter at breast height, dbh) and mapped. A comparison of pre- to post-logging (85 years later in 1968) stand characteristics showed the estimated basal area of 56.7 m<sup>2</sup> ha<sup>−1</sup> in the pre-cut 1883 Big Stump Grove was very similar to the population mean basal area of 30 other giant sequoia groves (with more than 30 trees) in Sequoia and Kings Canyon National Parks. Sequoia density in 1968 was 1.5 times higher than the population mean, and over 45% of the basal area had been recovered after only 85 years. Assuming most re-establishment occurred over roughly a 9 year period (1883–1892), the diameter growth rate of trees less than 1.95 m dbh, averaged 6.1–6.8 mm year<sup>−1</sup> but greatly varied as the 24 trees in the 1.8 m size class had a mean diameter growth rate of 21–24 mm year<sup>−1</sup>. Data generated by dividing the grove into 0.25 ha contiguous plots indicated that only about 3.3 ha of the pre-cut 1883 grove did not have sequoia regeneration whereas 16.5 ha of the 1968 grove had sequoia regeneration but no sign of logs or stumps. The proportion of only-regeneration plots was significantly greater (<i>P</i><0.05) in peripheral areas compared to core areas of the grove. A stage projection model showed that with typical natality, growth, and mortality rates in the current (<i>t</i>=0; 1968) stand, overrepresentation of 0.3–1.2 m dbh trees may produce a bimodal size distribution lasting perhaps 800 years or more into the future. Giant sequoia stand characteristics such as age and size structure are not highly resilient and may take several centuries to approach the ‘domain’ of age or size structure typical of old-growth sequoia forests. Grove boundaries may be less stable following a major disturbance.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Forest Ecology and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier Science","publisherLocation":"Amsterdam","doi":"10.1016/0378-1127(92)90008-W","usgsCitation":"Stohlgren, T.J., 1992, Resilience of a heavily logged grove of giant sequoia (<i>Sequoiadendron giganteum</i>) in Kings Canyon National Park, California: Forest Ecology and Management, v. 54, no. 1-4, p. 115-140, https://doi.org/10.1016/0378-1127(92)90008-W.","productDescription":"26 p.","startPage":"115","endPage":"140","numberOfPages":"26","costCenters":[],"links":[{"id":294508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294507,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0378-1127(92)90008-W"}],"volume":"54","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54252ec8e4b0e641df8a7100","contributors":{"authors":[{"text":"Stohlgren, Thomas J. 0000-0001-9696-4450 stohlgrent@usgs.gov","orcid":"https://orcid.org/0000-0001-9696-4450","contributorId":2902,"corporation":false,"usgs":true,"family":"Stohlgren","given":"Thomas","email":"stohlgrent@usgs.gov","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":502232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70243291,"text":"70243291 - 1992 - Discussion of “Derivation of Infiltration Equation Using Systems Approach” by V. P. Singh and F. X. Yu (November/December, 1990, Vol. 116, No. 6)","interactions":[],"lastModifiedDate":"2023-05-05T16:10:36.327085","indexId":"70243291","displayToPublicDate":"1992-11-01T11:04:49","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2362,"text":"Journal of Irrigation and Drainage Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of “Derivation of Infiltration Equation Using Systems Approach” by V. P. Singh and F. X. Yu (November/December, 1990, Vol. 116, No. 6)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/(ASCE)0733-9437(1992)118:6(996)","usgsCitation":"Chen, C., 1992, Discussion of “Derivation of Infiltration Equation Using Systems Approach” by V. P. Singh and F. X. Yu (November/December, 1990, Vol. 116, No. 6): Journal of Irrigation and Drainage Engineering, v. 118, no. 6, p. 996-999, https://doi.org/10.1061/(ASCE)0733-9437(1992)118:6(996).","productDescription":"4 p.","startPage":"996","endPage":"999","costCenters":[],"links":[{"id":416777,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Chen, Cheng-lung","contributorId":30752,"corporation":false,"usgs":true,"family":"Chen","given":"Cheng-lung","email":"","affiliations":[],"preferred":false,"id":871870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70127561,"text":"70127561 - 1992 - Non-random pairing in American kestrels: mate choice versus intra-sexual competition","interactions":[],"lastModifiedDate":"2014-09-30T10:48:54","indexId":"70127561","displayToPublicDate":"1992-11-01T10:46:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":770,"text":"Animal Behaviour","active":true,"publicationSubtype":{"id":10}},"title":"Non-random pairing in American kestrels: mate choice versus intra-sexual competition","docAbstract":"Natural selection may influence the arrangement of individuals into mated pairs through either inter-sexual (mate choice) or intra-sexual selection (competition). A study of the American kestrel, <i>Falco sparverius</i>, in northern Saskatchewan distinguished between these two processes using size as a measure of the bird's competitive ability, and condition (mass scaled to body size) as an index of quality. Both sexes arrive on the study area after spring migration in equal numbers and males establish territories. Males and females that moved among territories at the time of pair formation were not different in size or condition from those that did not move, suggesting that birds were not being displaced by superior competitors, and that females moved to encounter potential mates. Within mated pairs, there was no relationship between a bird's size and the condition of its mate for either sex as would be predicted if intra-sexual competitition explained mating patterns. Instead, there was positive assortative mating by condition, suggesting that both sexes used quality as the criterion in choosing mates. There was no correlation between the sizes of males and females in mated paird. Because there were no differences in size or condition of breeding and non-breeding males, factors other than physical attributes, such as prior experience with the area, may determine a male's success in obtaining a territory. Because females that did not obtain mates were in poorer condition than those that did, males may have rejected poor quality females. The results suggest that intra-sexual competition was not important for pair formation, and that kestrels chose mates on the basis of quality.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Animal Behaviour","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Association for the Study of Animal Behaviour","publisherLocation":"London","doi":"10.1016/S0003-3472(05)80577-9","usgsCitation":"Bortolotti, G.R., and Iko, W.M., 1992, Non-random pairing in American kestrels: mate choice versus intra-sexual competition: Animal Behaviour, v. 44, no. 5, p. 811-821, https://doi.org/10.1016/S0003-3472(05)80577-9.","productDescription":"11 p.","startPage":"811","endPage":"821","numberOfPages":"11","costCenters":[],"links":[{"id":294625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294624,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0003-3472(05)80577-9"}],"volume":"44","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542bc640e4b0abfb4c80985a","contributors":{"authors":[{"text":"Bortolotti, Gary R.","contributorId":71491,"corporation":false,"usgs":true,"family":"Bortolotti","given":"Gary","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":502407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iko, William M. ikob@usgs.gov","contributorId":2289,"corporation":false,"usgs":true,"family":"Iko","given":"William","email":"ikob@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":502406,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70243225,"text":"70243225 - 1992 - Analytical comparison of geomagnetic total field between Sino-US stations","interactions":[],"lastModifiedDate":"2023-05-04T13:07:06.398021","indexId":"70243225","displayToPublicDate":"1992-11-01T07:52:19","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":646,"text":"Acta Seismologica Sinica","active":true,"publicationSubtype":{"id":10}},"title":"Analytical comparison of geomagnetic total field between Sino-US stations","docAbstract":"<p><span>Using observational data of geomagnetic total intensity from 13 stations in the Beijing-Tianjin region, 3 stations in the western Yunnan region of China, and 6 stations in California of U. S. A., the daily variations and their spectra of geomagnetic total intensity were analyzed and compared. The results show that the morphology, the range and spectrum of daily variations in geomagnetic total intensity are basically the same within the local extent of 100–200 km and are different in the large extent of 500 km. The latitude factor of the daily variation range of geomagnetic total intensity is about 1–2 nT/degree within the latitude extent of 25°–40°.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF02651028","usgsCitation":"Zhan, Z., Yao, F., Johnston, M., Mueller, R., and Gao, J., 1992, Analytical comparison of geomagnetic total field between Sino-US stations: Acta Seismologica Sinica, v. 5, p. 807-813, https://doi.org/10.1007/BF02651028.","productDescription":"7 p.","startPage":"807","endPage":"813","costCenters":[],"links":[{"id":416710,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China, United States","state":"Beijing-Tianjin, California, Yunnan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.2581438860185,\n     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M.","contributorId":88091,"corporation":false,"usgs":true,"family":"Johnston","given":"M.","email":"","affiliations":[],"preferred":false,"id":871548,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mueller, R.","contributorId":23398,"corporation":false,"usgs":true,"family":"Mueller","given":"R.","email":"","affiliations":[],"preferred":false,"id":871549,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gao, Jintian","contributorId":304754,"corporation":false,"usgs":false,"family":"Gao","given":"Jintian","email":"","affiliations":[],"preferred":false,"id":871550,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70243346,"text":"70243346 - 1992 - Momentum and energy coefficients based on power-law velocity profile","interactions":[],"lastModifiedDate":"2023-05-09T11:48:09.080688","indexId":"70243346","displayToPublicDate":"1992-11-01T06:43:41","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Momentum and energy coefficients based on power-law velocity profile","docAbstract":"<p><span>The theoretical momentum coefficient (β) and energy coefficient (α) for turbulent shear flow in circular pipes and wide channels are derived from the power law, then compared with their counterparts on the basis of the logarithmic law. For such unidirectional flows, the exponent (m) of the power‐law velocity distribution is the sole parameter that determines the values of β and α. A comparison of the corresponding expressions for β and α derived using both laws shows that their values differ only slightly within a valid range of small m's. Use of a power‐law‐based β expression along with a power‐law resistance formula in the cross‐section‐averaged equation of momentum cannot only eliminate the theoretical incompatibility that results from mixing logarithmic and power laws in the equation but also remove the inconsistent assumption of&nbsp;</span><span class=\"equationTd\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot; overflow=&quot;scroll&quot;><mrow><mi>&amp;#x3B2;</mi><mspace width=&quot;0.16em&quot; /><mo>=</mo><mspace width=&quot;0.16em&quot; /><mn>1</mn></mrow></math>\"><span id=\"MathJax-Span-1\" class=\"math\"><span><span id=\"MathJax-Span-2\" class=\"mrow\"><span id=\"MathJax-Span-3\" class=\"mrow\"><span id=\"MathJax-Span-4\" class=\"mi\">β</span><span id=\"MathJax-Span-5\" class=\"mspace\"></span><span id=\"MathJax-Span-6\" class=\"mo\">=</span><span id=\"MathJax-Span-7\" class=\"mspace\"></span><span id=\"MathJax-Span-8\" class=\"mn\">1 </span></span></span></span></span></span></span><span>made in the equation. Improvement on the accuracy of the flow computation by incorporating a power‐law‐based p expression in the equation of momentum is demonstrated through an example in which a new stability limit for the Froude number for turbulent shear flow in wide channels can be accurately derived without assuming&nbsp;</span><span class=\"equationTd\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot; overflow=&quot;scroll&quot;><mrow><mi>&amp;#x3B2;</mi><mspace width=&quot;0.16em&quot; /><mo>=</mo><mspace width=&quot;0.16em&quot; /><mn>1</mn><mtext>.</mtext></mrow></math>\"><span id=\"MathJax-Span-9\" class=\"math\"><span><span id=\"MathJax-Span-10\" class=\"mrow\"><span id=\"MathJax-Span-11\" class=\"mrow\"><span id=\"MathJax-Span-12\" class=\"mi\">β</span><span id=\"MathJax-Span-13\" class=\"mspace\"></span><span id=\"MathJax-Span-14\" class=\"mo\">=</span><span id=\"MathJax-Span-15\" class=\"mspace\"></span><span id=\"MathJax-Span-16\" class=\"mn\">1</span><span id=\"MathJax-Span-17\" class=\"mtext\">.</span></span></span></span></span></span></span></p>","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/(ASCE)0733-9429(1992)118:11(1571)","usgsCitation":"Chen, C., 1992, Momentum and energy coefficients based on power-law velocity profile: Journal of Hydraulic Engineering, v. 118, no. 11, p. 1571-1584, https://doi.org/10.1061/(ASCE)0733-9429(1992)118:11(1571).","productDescription":"14 p.","startPage":"1571","endPage":"1584","costCenters":[],"links":[{"id":416849,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Chen, Cheng-lung","contributorId":30752,"corporation":false,"usgs":true,"family":"Chen","given":"Cheng-lung","email":"","affiliations":[],"preferred":false,"id":872116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003133,"text":"1003133 - 1992 - Evaluating fishery rehabilitation under uncertainty: A bioeconomic analysis of quota management for the Green Bay yellow perch fishery","interactions":[],"lastModifiedDate":"2025-03-28T16:35:38.383158","indexId":"1003133","displayToPublicDate":"1992-11-01T00:00:00","publicationYear":"1992","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":"Evaluating fishery rehabilitation under uncertainty: A bioeconomic analysis of quota management for the Green Bay yellow perch fishery","docAbstract":"<p><span>The fishery for yellow perch&nbsp;</span><i>Perca flavescens</i><span>&nbsp;in Green Bay, Lake Michigan, is currently operating under a rehabilitation plan based on a commercial harvest quota. We developed a bioeconomic computer model that included links between population density and growth, recruitment, and fishing effort for this fishery. Random variability was included in the stock–recruitment relation and in a simulated population assessment. We used the model in an adaptive management framework to evaluate the effects of the rehabilitation plan on both commercial and sport fisheries and to search for ways to improve the plan. Results indicate that the current quota policy is a member of a set of policies that would meet most management goals and increase total value of the fishery. Sensitivity analyses indicate that this conclusion is robust over a wide range of biological conditions. We predict that commercial fishers will lose money relative to the baseline condition, but they may receive other benefits from the elimination of the common‐property nature of the fishery. The prospect exists for managing variability in harvest and stock size and for maximizing economic returns in the fishery, but more information is required, primarily on sportfishing effort dynamics and angler preferences. Stock‐recruitment relations, density dependence of growth, and dynamics of sportfishing effort are the primary sources of uncertainty limiting the precision of our predictions. The current quota policy is about as good as other policies at reducing this uncertainty and appears, overall, to be one of the best choices for this fishery. The analytical techniques used in this study were primarily simple, heuristic approaches that could be easily transferred to other studies.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8675(1992)012<0703:EFRUUA>2.3.CO;2","usgsCitation":"Johnson, B., Milliman, S., Bishop, R., and Kitchell, J., 1992, Evaluating fishery rehabilitation under uncertainty: A bioeconomic analysis of quota management for the Green Bay yellow perch fishery: North American Journal of Fisheries Management, v. 12, no. 4, p. 703-720, https://doi.org/10.1577/1548-8675(1992)012<0703:EFRUUA>2.3.CO;2.","productDescription":"18 p.","startPage":"703","endPage":"720","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134350,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Green Bay","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.03861528382518,\n              44.5806619990727\n            ],\n            [\n              -88.03861528382518,\n              44.52036667216541\n            ],\n            [\n              -87.93610890800826,\n              44.52036667216541\n            ],\n            [\n              -87.93610890800826,\n              44.5806619990727\n            ],\n            [\n              -88.03861528382518,\n              44.5806619990727\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb08a","contributors":{"authors":[{"text":"Johnson, Barry L.","contributorId":95009,"corporation":false,"usgs":true,"family":"Johnson","given":"Barry L.","affiliations":[],"preferred":false,"id":312806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milliman, S.R.","contributorId":100809,"corporation":false,"usgs":true,"family":"Milliman","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":312807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bishop, R.C.","contributorId":79439,"corporation":false,"usgs":true,"family":"Bishop","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":312805,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kitchell, J.F.","contributorId":33259,"corporation":false,"usgs":true,"family":"Kitchell","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":312804,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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