{"pageNumber":"2559","pageRowStart":"63950","pageSize":"25","recordCount":184617,"records":[{"id":70161777,"text":"70161777 - 2005 - Population manipulations: Chapter","interactions":[],"lastModifiedDate":"2016-01-06T09:10:56","indexId":"70161777","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Population manipulations: Chapter","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Amphibian declines: The conservation status of United States species","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of California Press","usgsCitation":"Dodd, C.K., 2005, Population manipulations: Chapter, chap. <i>of</i> Amphibian declines: The conservation status of United States species, p. 265-270.","productDescription":"6 p.","startPage":"265","endPage":"270","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":313888,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313887,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.ucpress.edu/book.php?isbn=9780520235922"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4923e4b0e7a44bc41a35","contributors":{"editors":[{"text":"Lannoo, Michael J.","contributorId":46482,"corporation":false,"usgs":true,"family":"Lannoo","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":587730,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Dodd, C. Kenneth Jr.","contributorId":89215,"corporation":false,"usgs":true,"family":"Dodd","given":"C.","suffix":"Jr.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":587729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70608,"text":"wdrMS041 - 2005 - Water resources data Mississippi water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"wdrMS041","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MS-04-1","title":"Water resources data Mississippi water year 2004","docAbstract":"Water resources data for this water year for Mississippi consists of records of surface water and ground water in the State. Specifically, it contains: (1) Discharge records for 90 streamflow-gaging stations, stage records for 18 of these gaging stations, discharge records for 97 partial-record stations or miscellaneous streamflow sites, including 6 flood hydrograph partial-record stations, 91 crest-stage partial-record stations and 0 special study and miscellaneous sites; (2) stage only at 1 gaging station; (3) water-quality records for 12 streamflow-gaging stations, 0 stage-only stations, 13 water-quality monitor stations, 0 partial-record stations or miscellaneous sites, 0 short-term study sites, and 26 wells; and (4) water-level records for 19 observation wells. Records obtained from water-resources investigations are also included in special sections of the report. Records included for stream stages are only a small fraction of those obtained during the water year.","language":"ENGLISH","doi":"10.3133/wdrMS041","usgsCitation":"Morris, F., Runner, M., and Storm, J., 2005, Water resources data Mississippi water year 2004 (Online only): U.S. Geological Survey Water Data Report MS-04-1, 300 p., https://doi.org/10.3133/wdrMS041.","productDescription":"300 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6798,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ms-04-1/","linkFileType":{"id":5,"text":"html"}},{"id":192772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f80b0","contributors":{"authors":[{"text":"Morris, F. III","contributorId":76395,"corporation":false,"usgs":true,"family":"Morris","given":"F.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":282718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runner, M.S.","contributorId":28630,"corporation":false,"usgs":true,"family":"Runner","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":282716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storm, J.B.","contributorId":51838,"corporation":false,"usgs":true,"family":"Storm","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":282717,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70623,"text":"fs20043067 - 2005 - Ground-water vulnerability to nitrate contamination in the mid-atlantic region","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"fs20043067","displayToPublicDate":"2005-06-01T00:00:00","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":"2004-3067","title":"Ground-water vulnerability to nitrate contamination in the mid-atlantic region","docAbstract":"The U.S. Environmental Protection Agency?s (USEPA) Regional Vulnerability Assessment (ReVA) Program has developed a set of statistical tools to support regional-scale, integrated ecological risk-assessment studies. One of these tools, developed by the U.S. Geological Survey (USGS), is used with available water-quality data obtained from USGS National Water-Quality Assessment (NAWQA) and other studies in association with land cover, geology, soils, and other geographic data to develop logistic-regression equations that predict the vulnerability of ground water to nitrate concentrations exceeding specified thresholds in the Mid-Atlantic Region. The models were developed and applied to produce spatial probability maps showing the likelihood of elevated concentrations of nitrate in the region. These maps can be used to identify areas that currently are at risk and help identify areas where ground water has been affected by human activities. This information can be used by regional and local water managers to protect water supplies and identify land-use planning solutions and monitoring programs in these vulnerable areas.","language":"ENGLISH","doi":"10.3133/fs20043067","usgsCitation":"Greene, E.A., LaMotte, A.E., Cullinan, K., and Smith, E.R., 2005, Ground-water vulnerability to nitrate contamination in the mid-atlantic region: U.S. Geological Survey Fact Sheet 2004-3067, 4 p., https://doi.org/10.3133/fs20043067.","productDescription":"4 p.","costCenters":[],"links":[{"id":6805,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://md.water.usgs.gov/publications/fs-2004-3067/html/","linkFileType":{"id":5,"text":"html"}},{"id":125084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2004/3067/report-thumb.jpg"},{"id":90526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2004/3067/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65556b","contributors":{"authors":[{"text":"Greene, Earl A. 0000-0002-9479-0829 eagreene@usgs.gov","orcid":"https://orcid.org/0000-0002-9479-0829","contributorId":3518,"corporation":false,"usgs":true,"family":"Greene","given":"Earl","email":"eagreene@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cullinan, Kerri-Ann","contributorId":90821,"corporation":false,"usgs":true,"family":"Cullinan","given":"Kerri-Ann","email":"","affiliations":[],"preferred":false,"id":282736,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Elizabeth R.","contributorId":76023,"corporation":false,"usgs":true,"family":"Smith","given":"Elizabeth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282735,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185646,"text":"70185646 - 2005 - Environmental issues of petroleum exploration and production: Introduction","interactions":[],"lastModifiedDate":"2018-11-05T10:58:39","indexId":"70185646","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1541,"text":"Environmental Geosciences","active":true,"publicationSubtype":{"id":10}},"title":"Environmental issues of petroleum exploration and production: Introduction","docAbstract":"<p>Energy is the lifeblood of our planet Earth, an essential commod- ity that powers the expanding global economy. Starting in the 1950s, oil and natural gas became the main sources of primary energy for the increasing world population, and this dominance is expected to continue for several more decades (Edwards, 1997; Energy Information Administration (EIA), 2004). In the United States, petroleum production started in 1859 when Drake's well was drilled near Titusville, Pennsylvania, and oil and natural gas currently supply approximately 63% of the energy consumption; forecasts indicate that by 2025, their use will increase by about 40% to 28.3 million bbl/day and to 31.4 tcf/yr (EIA, 2004). The clear benefits of petroleum consumption, however, can carry major environmental impacts that may be regional or global in scale, in- cluding air pollution, global climate change, and oil spills. This vol- ume of Environmental Geosciences, covering environmental impacts of petroleum exploration and production, does not address these major impacts directly because air pollution and global warming are issues related primarily to petroleum and coal uses, and major oil spills are generally attributed to marine petroleum transportation, such as the Exxon Valdez's 1989 spill of 260,000 bbl of oil into Prince William Sound, Alaska. Exploration for and production of petroleum, however, have caused local detrimental impacts to soils, surface and groundwa- ters, and ecosystems in the 36 producing states in the United States (Richter and Kreitler, 1993; Kharaka and Hanor, 2003). These im- pacts arose primarily from the improper disposal of some of the large volumes (presently estimated at 20 billion bbl/yr total pro- duced) of saline water produced with oil and gas, from accidental hydrocarbon and produced-water releases, and from abandoned oil wells that were orphaned or not correctly plugged (Kharaka et al., 1995; Veil et al., 2004). Impacts and ground-surface disturbances, in the order of several acres per well, can also arise from related activities such as site clearance, construction of roads, tank bat- teries, brine pits and pipelines, and other land modifications nec- essary for the drilling of exploration and production wells and construction of production facilities. The cumulative impacts from these operations are high, because a total of about 3.5 million oil.&nbsp;</p>","language":"English","publisher":"AAPG","usgsCitation":"Kharaka, Y.K., and Dorsey, N.S., 2005, Environmental issues of petroleum exploration and production: Introduction: Environmental Geosciences, v. 12, no. 2, p. 61-63.","productDescription":"3 p. ","startPage":"61","endPage":"63","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338346,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":359151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://toxics.usgs.gov/pubs/KharakaIntro.PDF"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da251be4b0543bf7fda802","contributors":{"authors":[{"text":"Kharaka, Yousif K. 0000-0001-9861-8260 ykharaka@usgs.gov","orcid":"https://orcid.org/0000-0001-9861-8260","contributorId":1928,"corporation":false,"usgs":true,"family":"Kharaka","given":"Yousif","email":"ykharaka@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":686207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorsey, Nancy S.","contributorId":189835,"corporation":false,"usgs":false,"family":"Dorsey","given":"Nancy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":686208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156406,"text":"70156406 - 2005 - An online operational rainfall-monitoring resource for epidemic malaria early warning systems in Africa","interactions":[],"lastModifiedDate":"2017-05-22T23:04:13","indexId":"70156406","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2650,"text":"Malaria Journal","active":true,"publicationSubtype":{"id":10}},"title":"An online operational rainfall-monitoring resource for epidemic malaria early warning systems in Africa","docAbstract":"<p class=\"Para\">Periodic epidemics of malaria are a major public health problem for many sub-Saharan African countries. Populations in epidemic prone areas have a poorly developed immunity to malaria and the disease remains life threatening to all age groups. The impact of epidemics could be minimized by prediction and improved prevention through timely vector control and deployment of appropriate drugs. Malaria Early Warning Systems are advocated as a means of improving the opportunity for preparedness and timely response.</p><p class=\"Para\">Rainfall is one of the major factors triggering epidemics in warm semi-arid and desert-fringe areas. Explosive epidemics often occur in these regions after excessive rains and, where these follow periods of drought and poor food security, can be especially severe. Consequently, rainfall monitoring forms one of the essential elements for the development of integrated Malaria Early Warning Systems for sub-Saharan Africa, as outlined by the World Health Organization.</p><p class=\"Para\">The Roll Back Malaria Technical Resource Network on Prevention and Control of Epidemics recommended that a simple indicator of changes in epidemic risk in regions of marginal transmission, consisting primarily of rainfall anomaly maps, could provide immediate benefit to early warning efforts. In response to these recommendations, the Famine Early Warning Systems Network produced maps that combine information about dekadal rainfall anomalies, and epidemic malaria risk, available via their Africa Data Dissemination Service. These maps were later made available in a format that is directly compatible with HealthMapper, the mapping and surveillance software developed by the WHO's Communicable Disease Surveillance and Response Department. A new monitoring interface has recently been developed at the International Research Institute for Climate Prediction (IRI) that enables the user to gain a more contextual perspective of the current rainfall estimates by comparing them to previous seasons and climatological averages. These resources are available at no cost to the user and are updated on a routine basis.</p>","language":"English","publisher":"BioMed Central","doi":"10.1186/1475-2875-4-6","usgsCitation":"Grover-Kopec, E., Kawano, M., Klaver, R.W., Blumenthal, B., Ceccato, P., and Connor, S.J., 2005, An online operational rainfall-monitoring resource for epidemic malaria early warning systems in Africa: Malaria Journal, v. 4, no. 6, p. 1-5, https://doi.org/10.1186/1475-2875-4-6.","productDescription":"5 p.","startPage":"1","endPage":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":477660,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/1475-2875-4-6","text":"Publisher Index Page"},{"id":307070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-01-21","publicationStatus":"PW","scienceBaseUri":"55d6fa2fe4b0518e3546bc1e","contributors":{"authors":[{"text":"Grover-Kopec, Emily","contributorId":146813,"corporation":false,"usgs":false,"family":"Grover-Kopec","given":"Emily","email":"","affiliations":[],"preferred":false,"id":569048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kawano, Mika","contributorId":146814,"corporation":false,"usgs":false,"family":"Kawano","given":"Mika","email":"","affiliations":[],"preferred":false,"id":569049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klaver, Robert W. 0000-0002-3263-9701 bklaver@usgs.gov","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":3285,"corporation":false,"usgs":true,"family":"Klaver","given":"Robert","email":"bklaver@usgs.gov","middleInitial":"W.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":569050,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumenthal, Benno","contributorId":146815,"corporation":false,"usgs":false,"family":"Blumenthal","given":"Benno","email":"","affiliations":[],"preferred":false,"id":569051,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ceccato, Pietro","contributorId":64126,"corporation":false,"usgs":true,"family":"Ceccato","given":"Pietro","email":"","affiliations":[],"preferred":false,"id":569052,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Connor, Stephen J.","contributorId":104370,"corporation":false,"usgs":true,"family":"Connor","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":569053,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70179751,"text":"70179751 - 2005 - Is disease an important mortality factor for Pacific herring?","interactions":[],"lastModifiedDate":"2017-01-17T11:54:05","indexId":"70179751","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5266,"text":"American Association of Wildlife Veterinarians ","active":true,"publicationSubtype":{"id":10}},"title":"Is disease an important mortality factor for Pacific herring?","docAbstract":"<p>Marine pelagic forage fishes, including sardines, anchovies, and herring, undergo large oscillations in population abundance. Although over-fishing can have a dramatic impact in reducing population size, this anthropogenic perturbation cannot fully account for all population declines because natural oscillations in marine pelagic fish biomasses occurred prior to the onset of commercial fishing. Among the herring metapopulation in Puget Sound / Straight of Georgia, the mean estimated annual mortality, exclusive of commercial fishing, increased from 20% in the late 1970’s and early 1980’s to 64-87% during 1996-1999. This natural mortality affects primarily the older age cohorts and resulted in recent decreased median ages of adult herring from age 4-6 cohorts to age 2-3 cohorts that die prior to iteroparous spawning. Surveys of wild herring from the region indicate that the protozoan parasite Ichthyophonus sp., is currently ubiquitous among Pacific herring populations in Washington and British Columbia, and prevalence of infection increase directly with herring age, from 12% among juveniles to 58% among the underrepresented age 6+ cohorts. Ichthyophonus can be highly pathogenic to immunologically naïve Pacific herring, causing 80% mortality 2 mo. after exposure in the laboratory. Current laboratory-based studies are underway to determine whether natural Ichthyophonus infections are terminal for the host, and whether these infections account for the decreasing median age of wild Pacific herring populations in recent years. </p>","language":"English","publisher":"AAWV ","usgsCitation":"Hershberger, P., 2005, Is disease an important mortality factor for Pacific herring?: American Association of Wildlife Veterinarians , p. 1-3.","productDescription":"3 p. ","startPage":"1","endPage":"3","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"587f3dbae4b0d96de2564569","contributors":{"authors":[{"text":"Hershberger, Paul","contributorId":92557,"corporation":false,"usgs":true,"family":"Hershberger","given":"Paul","affiliations":[],"preferred":false,"id":658546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70161778,"text":"70161778 - 2005 - Red Hills salamander, <i>Phaeognathus hubrichti</i> Highton: Chapter","interactions":[],"lastModifiedDate":"2016-01-06T09:14:56","indexId":"70161778","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Red Hills salamander, <i>Phaeognathus hubrichti</i> Highton: Chapter","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Amphibian declines: The conservation status of  United States species","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"University of California Press","usgsCitation":"Dodd, C.K., 2005, Red Hills salamander, <i>Phaeognathus hubrichti</i> Highton: Chapter, chap. <i>of</i> Amphibian declines: The conservation status of  United States species, p. 785-787.","productDescription":"3 p.","startPage":"785","endPage":"787","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":313890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313889,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.ucpress.edu/book.php?isbn=9780520235922"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4927e4b0e7a44bc41a49","contributors":{"editors":[{"text":"Lannoo, Michael J.","contributorId":46482,"corporation":false,"usgs":true,"family":"Lannoo","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":587732,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Dodd, C. Kenneth Jr.","contributorId":89215,"corporation":false,"usgs":true,"family":"Dodd","given":"C.","suffix":"Jr.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":587731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184392,"text":"70184392 - 2005 - Ground-water/surface-water responses to global climate simulations, Santa Clara-Calleguas basin, Ventura County, California, 1950-93","interactions":[],"lastModifiedDate":"2018-09-18T10:14:43","indexId":"70184392","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","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":"Ground-water/surface-water responses to global climate simulations, Santa Clara-Calleguas basin, Ventura County, California, 1950-93","docAbstract":"<p><span>Climate variations can play an important, if not always crucial, role in successful conjunctive management of ground water and surface water resources. This will require accurate accounting of the links between variations in climate, recharge, and withdrawal from the resource systems, accurate projection or predictions of the climate variations, and accurate simulation of the responses of the resource systems. To assess linkages and predictability of climate influences on conjunctive management, global climate model (GCM) simulated precipitation rates were used to estimate inflows and outflows from a regional ground water model (RGWM) of the coastal aquifers of the Santa Clara-Calleguas Basin at Ventura, California, for 1950 to 1993. Interannual to interdecadal time scales of the El Niño Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) climate variations are imparted to simulated precipitation variations in the Southern California area and are realistically imparted to the simulated ground water level variations through the climate-driven recharge (and discharge) variations. For example, the simulated average ground water level response at a key observation well in the basin to ENSO variations of tropical Pacific sea surface temperatures is 1.2 m/°C, compared to 0.9 m/°C in observations. This close agreement shows that the GCM-RGWM combination can translate global scale climate variations into realistic local ground water responses. Probability distributions of simulated ground water level excursions above a local water level threshold for potential seawater intrusion compare well to the corresponding distributions from observations and historical RGWM simulations, demonstrating the combination's potential usefulness for water management and planning. Thus the GCM-RGWM combination could be used for planning purposes and — when the GCM forecast skills are adequate — for near term predictions.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.2005.tb03752.x","usgsCitation":"Hanson, R.T., and Dettinger, M., 2005, Ground-water/surface-water responses to global climate simulations, Santa Clara-Calleguas basin, Ventura County, California, 1950-93: Journal of the American Water Resources Association, v. 41, no. 3, p. 517-536, https://doi.org/10.1111/j.1752-1688.2005.tb03752.x.","productDescription":"20 p. 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,{"id":70205404,"text":"70205404 - 2005 - Can nitrogen sequestration explain the unexpected nitrate decline in New Hampshire streams?","interactions":[],"lastModifiedDate":"2019-09-17T12:03:02","indexId":"70205404","displayToPublicDate":"2005-05-31T11:59:17","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1478,"text":"Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Can nitrogen sequestration explain the unexpected nitrate decline in New Hampshire streams?","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"Springer","doi":"10.1007/s10021-004-0105-z","usgsCitation":"Huntington, T.G., 2005, Can nitrogen sequestration explain the unexpected nitrate decline in New Hampshire streams?: Ecosystems, v. 8, no. 3, p. 331-333, https://doi.org/10.1007/s10021-004-0105-z.","productDescription":"3 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Hampshire\",\"nation\":\"USA  \"}}]}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-05-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":1884,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70595,"text":"sir20055090 - 2005 - Inventory of ground-water resources in the Kabul Basin, Afghanistan","interactions":[],"lastModifiedDate":"2021-09-28T15:59:10.570019","indexId":"sir20055090","displayToPublicDate":"2005-05-31T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5090","title":"Inventory of ground-water resources in the Kabul Basin, Afghanistan","docAbstract":"In 2004, the U.S. Geological Survey began working with engineers at the Afghanistan Geological Survey to provide hydrologic training and equipment and to apply these tools to build an inventory of water wells in the Kabul Basin of Afghanistan. An inventory of 148 wells now includes information on well location, depth, and access. Water-level and water-quality measurements have been made at most of these wells. A water-level elevation map has been constructed, and general directions of ground-water flow have been defined.\r\n\r\nGround-water flow in the Kabul Basin is primarily through saturated alluvium and other basin-fill sediments. The water-table surface generally mirrors topography, and ground water generally flows in the directions of surface-water discharge. The quality of ground water in the Kabul Basin varies widely. In some areas, ground-water quality is excellent, with low concentrations of dissolved solids and no problematic constituents. In other areas, however, high concentrations of dissolved solids and the presence of some constituents at concentrations deemed harmful to humans and crops render untreated ground water marginal or unsuitable for public supply and/or agricultural use. Of particular concern are elevated concentrations of nitrate, boron, and dissolved solids, and an indication of fecal pollution in some parts of the basin.\r\n\r\nAs Afghanistan emerges from years of conflict, as institutional capacities rejuvenate and grow, and as the need for wise water-management decisions continues, adequate data and a fuller understanding of the ground-water resource in the Kabul Basin will be imperative. The work described in this report represents only a modest beginning in what will be a long-term data-collection and interpretive effort.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055090","usgsCitation":"Broshears, R.E., Chornack, M.P., Mueller, D.K., and Ruddy, B.C., 2005, Inventory of ground-water resources in the Kabul Basin, Afghanistan: U.S. Geological Survey Scientific Investigations Report 2005-5090, 44 p., https://doi.org/10.3133/sir20055090.","productDescription":"44 p.","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":6892,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5090/","linkFileType":{"id":5,"text":"html"}},{"id":185921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"Afghanistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[61.21082,35.65007],[62.23065,35.27066],[62.98466,35.40404],[63.19354,35.85717],[63.9829,36.00796],[64.54648,36.31207],[64.74611,37.11182],[65.58895,37.30522],[65.74563,37.66116],[66.21738,37.39379],[66.51861,37.36278],[67.07578,37.35614],[67.83,37.14499],[68.13556,37.02312],[68.85945,37.34434],[69.19627,37.15114],[69.51879,37.609],[70.11658,37.58822],[70.27057,37.73516],[70.3763,38.1384],[70.80682,38.48628],[71.34813,38.25891],[71.2394,37.95327],[71.54192,37.90577],[71.44869,37.06564],[71.84464,36.73817],[72.19304,36.94829],[72.63689,37.04756],[73.26006,37.49526],[73.9487,37.42157],[74.98,37.41999],[75.15803,37.13303],[74.57589,37.02084],[74.06755,36.83618],[72.92002,36.72001],[71.84629,36.50994],[71.26235,36.07439],[71.49877,35.65056],[71.61308,35.1532],[71.11502,34.73313],[71.15677,34.34891],[70.8818,33.98886],[69.93054,34.02012],[70.32359,33.35853],[69.68715,33.1055],[69.26252,32.50194],[69.31776,31.90141],[68.92668,31.62019],[68.55693,31.71331],[67.79269,31.58293],[67.68339,31.30315],[66.93889,31.30491],[66.38146,30.7389],[66.34647,29.88794],[65.04686,29.47218],[64.35042,29.56003],[64.148,29.34082],[63.55026,29.46833],[62.54986,29.31857],[60.87425,29.82924],[61.78122,30.73585],[61.69931,31.37951],[60.94194,31.54807],[60.86365,32.18292],[60.53608,32.98127],[60.9637,33.52883],[60.52843,33.67645],[60.80319,34.4041],[61.21082,35.65007]]]},\"properties\":{\"name\":\"Afghanistan\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e479de4b07f02db491c7c","contributors":{"authors":[{"text":"Broshears, Robert E.","contributorId":40675,"corporation":false,"usgs":true,"family":"Broshears","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chornack, Michael P. mpchorna@usgs.gov","contributorId":2431,"corporation":false,"usgs":true,"family":"Chornack","given":"Michael","email":"mpchorna@usgs.gov","middleInitial":"P.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":282690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mueller, David K. mueller@usgs.gov","contributorId":1585,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"mueller@usgs.gov","middleInitial":"K.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":282689,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruddy, Barbara C. bcruddy@usgs.gov","contributorId":4163,"corporation":false,"usgs":true,"family":"Ruddy","given":"Barbara","email":"bcruddy@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":282691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70598,"text":"wdrNJ041 - 2005 - Water resources data, New Jersey, water year 2004-volume 1. surface-water data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"wdrNJ041","displayToPublicDate":"2005-05-31T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-04-1","title":"Water resources data, New Jersey, water year 2004-volume 1. surface-water data","docAbstract":"Water-resources data for the 2004 water year for New Jersey are presented in three volumes, and consists of records of stage, discharge, and water-quality of streams; stage and contents of lakes and reservoirs; and water levels and water-quality of ground water. Volume 1 contains discharge records for 105 gaging stations; tide summaries at 27 tidal gaging stations; stage and contents at 39 lakes and reservoirs; and diversions from 51 surface-water sources. Also included are stage and discharge for 108 crest-stage partial-record stations, stage-only at 34 tidal crest-stage gages, and discharge for 124 low-flow partial-record stations. Locations of these sites are shown in figures 8-11. Additional discharge measurements were made at 131 miscellaneous sites that are not part of the systematic data-collection program. Discontinued station tables for gaging stations, crest-stage gages, tidal crest-stage and tidal gaging stations show historical coverage. The data in this report represent that part of the National Water Information System (NWIS) data collected by the United States Geological Survey (USGS). Hydrologic conditions are also described for this water year, including stream-flow, precipitation, reservoir conditions, and air temperatures.","language":"ENGLISH","doi":"10.3133/wdrNJ041","usgsCitation":"Centinaro, G., White, B., Hoppe, H., Dudek, J., Protz, A., Reed, T., Shvanda, J., and Watson, A., 2005, Water resources data, New Jersey, water year 2004-volume 1. surface-water data: U.S. Geological Survey Water Data Report NJ-04-1, 412 p., https://doi.org/10.3133/wdrNJ041.","productDescription":"412 p.","costCenters":[],"links":[{"id":6895,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrnj041/","linkFileType":{"id":5,"text":"html"}},{"id":185990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f60","contributors":{"authors":[{"text":"Centinaro, G.L.","contributorId":61892,"corporation":false,"usgs":true,"family":"Centinaro","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":282705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, B.T.","contributorId":9710,"corporation":false,"usgs":true,"family":"White","given":"B.T.","email":"","affiliations":[],"preferred":false,"id":282700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoppe, H.L.","contributorId":36994,"corporation":false,"usgs":true,"family":"Hoppe","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":282704,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dudek, J.F.","contributorId":31818,"corporation":false,"usgs":true,"family":"Dudek","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":282702,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Protz, A.R.","contributorId":97976,"corporation":false,"usgs":true,"family":"Protz","given":"A.R.","affiliations":[],"preferred":false,"id":282707,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Reed, T.J. 0000-0002-9943-4081","orcid":"https://orcid.org/0000-0002-9943-4081","contributorId":15224,"corporation":false,"usgs":true,"family":"Reed","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":282701,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shvanda, J.C.","contributorId":34999,"corporation":false,"usgs":true,"family":"Shvanda","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":282703,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Watson, A.F.","contributorId":85653,"corporation":false,"usgs":true,"family":"Watson","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":282706,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70596,"text":"sir20055074 - 2005 - Generalized water-level contours, September-October 2000 and March-April 2001, and long-term water-level changes, at the U.S. Air Force Plant 42 and vicinity, Palmdale, California","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20055074","displayToPublicDate":"2005-05-31T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5074","title":"Generalized water-level contours, September-October 2000 and March-April 2001, and long-term water-level changes, at the U.S. Air Force Plant 42 and vicinity, Palmdale, California","docAbstract":"Historically, the U.S. Air Force Plant 42 has relied on ground water as the primary source of water owing, in large part, to the scarcity of surface water in the region. Groundwater withdrawal for municipal, industrial, and agricultural use has affected ground-water levels at U.S. Air Force Plant 42, and vicinity. A study to document changes in groundwater gradients and to present historical water-level data was completed by the U.S. Geological Survey in cooperation with the U.S. Air Force. This report presents historical water-level data, hydrographs, and generalized seasonal water-level and water-level contours for September?October 2000 and March?April 2001. The collection and interpretation of ground-water data helps local water districts, military bases, and private citizens gain a better understanding of the ground-water flow systems, and consequently water availability.\r\n\r\n    During September?October 2000 and March?April 2001 the U.S. Geological Survey and other agencies made a total of 102 water-level measurements, 46 during September?October 2000 and 56 during March?April 2001. These data document recent conditions and, when compared with historical data, document changes in ground-water levels. Two water-level contour maps were drawn: the first depicts water-level conditions for September?October 2000 map and the second depicts water-level conditions for March?April 2001 map. In general, the water-level contour maps show water-level depressions formed as result of ground-water withdrawal. One hundred sixteen long-term hydrographs, using water-level data from 1915 through 2000, were constructed to show water-level trends in the area. The hydrographs indicate that water-level decline occurred throughout the study area, with the greatest declines south of U.S. Air Force Plant 42.","language":"ENGLISH","doi":"10.3133/sir20055074","usgsCitation":"Christensen, A.H., 2005, Generalized water-level contours, September-October 2000 and March-April 2001, and long-term water-level changes, at the U.S. Air Force Plant 42 and vicinity, Palmdale, California: U.S. Geological Survey Scientific Investigations Report 2005-5074, 131 p., https://doi.org/10.3133/sir20055074.","productDescription":"131 p.","costCenters":[],"links":[{"id":6893,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055074/","linkFileType":{"id":5,"text":"html"}},{"id":185922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec16","contributors":{"authors":[{"text":"Christensen, Allen H. 0000-0002-7061-5591 ahchrist@usgs.gov","orcid":"https://orcid.org/0000-0002-7061-5591","contributorId":1510,"corporation":false,"usgs":true,"family":"Christensen","given":"Allen","email":"ahchrist@usgs.gov","middleInitial":"H.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70597,"text":"fs20053041 - 2005 - South Carolina coastal erosion study","interactions":[],"lastModifiedDate":"2016-12-07T08:43:27","indexId":"fs20053041","displayToPublicDate":"2005-05-31T00:00:00","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":"2005-3041","title":"South Carolina coastal erosion study","language":"ENGLISH","doi":"10.3133/fs20053041","usgsCitation":"Denny, J.F., Baldwin, W.E., Schwab, W.C., Warner, J., and DeVoe, M.R., 2005, South Carolina coastal erosion study: U.S. Geological Survey Fact Sheet 2005-3041, 4 p., https://doi.org/10.3133/fs20053041.","productDescription":"4 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":122457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3041.bmp"},{"id":6894,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3041/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.84677124023438,\n              33.89435731090067\n            ],\n            [\n              -82.72705078125,\n              33.28691595686207\n            ],\n            [\n              -82.13104248046875,\n              32.76649095995108\n            ],\n            [\n              -81.18072509765625,\n              33.5093393678006\n            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jdenny@usgs.gov","orcid":"https://orcid.org/0000-0002-3472-618X","contributorId":418,"corporation":false,"usgs":true,"family":"Denny","given":"Jane","email":"jdenny@usgs.gov","middleInitial":"F.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldwin, Wayne E. 0000-0001-5886-0917 wbaldwin@usgs.gov","orcid":"https://orcid.org/0000-0001-5886-0917","contributorId":1321,"corporation":false,"usgs":true,"family":"Baldwin","given":"Wayne","email":"wbaldwin@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwab, William C. 0000-0001-9274-5154 bschwab@usgs.gov","orcid":"https://orcid.org/0000-0001-9274-5154","contributorId":417,"corporation":false,"usgs":true,"family":"Schwab","given":"William","email":"bschwab@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282695,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282698,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeVoe, M. Richard","contributorId":53887,"corporation":false,"usgs":true,"family":"DeVoe","given":"M.","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":282699,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70601,"text":"fs20043141 - 2005 - Shells as recorders of environmental change -- a study in Florida Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20043141","displayToPublicDate":"2005-05-31T00:00:00","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":"2004-3141","title":"Shells as recorders of environmental change -- a study in Florida Bay","language":"ENGLISH","doi":"10.3133/fs20043141","usgsCitation":"Stamm, R.G., and Wingard, G., 2005, Shells as recorders of environmental change -- a study in Florida Bay: U.S. Geological Survey Fact Sheet 2004-3141, 1 folded sheet ([4] p.) : col. ill., col. map ; 28 cm., https://doi.org/10.3133/fs20043141.","productDescription":"1 folded sheet ([4] p.) : col. ill., col. map ; 28 cm.","costCenters":[],"links":[{"id":121168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3141.bmp"},{"id":6896,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2004/3141/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3fd2","contributors":{"authors":[{"text":"Stamm, Robert G. 0000-0001-9141-5364 rstamm@usgs.gov","orcid":"https://orcid.org/0000-0001-9141-5364","contributorId":4702,"corporation":false,"usgs":true,"family":"Stamm","given":"Robert","email":"rstamm@usgs.gov","middleInitial":"G.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":282708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wingard, G. Lynn","contributorId":44969,"corporation":false,"usgs":true,"family":"Wingard","given":"G. Lynn","affiliations":[],"preferred":false,"id":282709,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70238533,"text":"70238533 - 2005 - East Molokai and other Kea-trend volcanoes: Magmatic processes and sources as they migrate away from the Hawaiian hot spot","interactions":[],"lastModifiedDate":"2022-11-28T18:44:04.83895","indexId":"70238533","displayToPublicDate":"2005-05-28T12:26:04","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":"East Molokai and other Kea-trend volcanoes: Magmatic processes and sources as they migrate away from the Hawaiian hot spot","docAbstract":"<p><span class=\"paraNumber\">[1]<span>&nbsp;</span></span><span>There are geochemical differences between shield lavas from the two parallel trends, Kea and Loa, defined by young Hawaiian volcanoes. The shield of East Molokai volcano, at greater than 1.5 Ma, is the oldest volcano on the Kea trend. Sequences of older tholeiitic to younger alkalic basalt that erupted as this volcano evolved from the shield to postshield stage of volcanism are well exposed. Much younger, ∼0.34–0.57 Ma, alkalic basalt and basanite erupted during rejuvenated stage volcanism. Like rejuvenated stage lavas erupted at other Hawaiian volcanoes, rejuvenated stage East Molokai lavas have relatively low&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr and high&nbsp;</span><sup>143</sup><span>Nd/</span><sup>144</sup><span>Nd. Such ratios reflect a source component with a long-term depletion in abundance of incompatible elements. On the basis of positive correlations of&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr versus&nbsp;</span><sup>206</sup><span>Pb/</span><sup>204</sup><span>Pb and negative correlations of these isotopic ratios with Nb/Zr, a smaller proportion of this depleted component also contributed to the late shield/postshield lavas erupted at East Molokai and the other Kea-trend volcanoes, Haleakala and Mauna Kea. At each of these Kea-trend volcanoes, as the volcano moved away from the hot spot, the extent of melting and magma supply from the mantle decreased, the depth of melt segregation increased, and there was an increasing role for a component with long-term relative depletion in incompatible elements. This depleted component has Kea-trend Pb isotopic characteristics and relatively low&nbsp;</span><sup>208</sup><span>Pb/</span><sup>204</sup><span>Pb at a given&nbsp;</span><sup>206</sup><span>Pb/</span><sup>204</sup><span>Pb, and it is probably not related to oceanic lithosphere or the source of mid-ocean ridge basalt. The overlap in Sr, Nd, and Pb isotope ratios of recent Kilauea shield lavas and 550 ka Mauna Kea shield lavas has been used to argue that Kea-trend shield volcanism samples a vertically continuous, geochemically distinct stripe which persisted in the hot spot source for 550 kyr (Eisele et al., 2003; Abouchami et al., 2005). As Kea-trend volcanoes migrate away from the hot spot and evolve from the shield to postshield stage, there are systematic changes in Sr, Nd, and Pb isotope ratios. However, the overlap of Sr, Nd, and Pb isotope ratios in late shield/postshield lavas from Mauna Kea (&lt;350 ka) and East Molokai (∼1.5 Ma) show that the periphery of the hot spot sampled by Kea-trend postshield lavas also had long-term geochemical homogeneity.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004GC000830","usgsCitation":"Xu, G., Frey, F.A., Clague, D.A., Weis, D., and Beeson, M.H., 2005, East Molokai and other Kea-trend volcanoes: Magmatic processes and sources as they migrate away from the Hawaiian hot spot: Geochemistry, Geophysics, Geosystems, v. 6, no. 5, 28 p., https://doi.org/10.1029/2004GC000830.","productDescription":"28 p.","costCenters":[],"links":[{"id":477661,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004gc000830","text":"Publisher Index 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A.","contributorId":167154,"corporation":false,"usgs":false,"family":"Frey","given":"Frederick","email":"","middleInitial":"A.","affiliations":[{"id":24632,"text":"Earth, Atmospheric & Planetary Sciences, MIT","active":true,"usgs":false}],"preferred":false,"id":857757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clague, David A.","contributorId":77105,"corporation":false,"usgs":false,"family":"Clague","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":857758,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weis, Dominique","contributorId":121531,"corporation":false,"usgs":true,"family":"Weis","given":"Dominique","affiliations":[],"preferred":false,"id":857759,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beeson, Melvin H. 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,{"id":70210257,"text":"70210257 - 2005 - Molecular identification of cypripedioid orchids in international trade","interactions":[],"lastModifiedDate":"2020-05-26T21:17:59.620552","indexId":"70210257","displayToPublicDate":"2005-05-26T16:12:15","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3373,"text":"Selbyana","active":true,"publicationSubtype":{"id":10}},"title":"Molecular identification of cypripedioid orchids in international trade","docAbstract":"<p> Two cypripedioid orchid genera, Paphiopedilum and Phragmipedium, are listed in Appendix I of CITES and are restricted from international trade. Because of their morphological similarity to other genera, however, they may be disguised as belonging to one of the other cypripedioids listed along with other orchids in Appendix II of CITES. Sequence analysis was performed on the internal transcribed spacer region (ITS) of ribosomal DNA of cypripedioid orchids to develop a molecular marker system capable of discriminating among rare species in trade. Molecular analyses concentrated on rare cypripedioid orchids from the genera Paphiopedilum and Phragmipedium, which are known to be poached from the wild and smuggled across international borders disguised as common species. A total of 48 taxa representing two genera {Paphiopedilum, N = 43; Phragmipedium, N = 5) have been sequenced and compared for distinc- tiveness. Phylogenetic analyses clearly distinguish between these two genera and among other cypripedioid genera, with 5-10 fixed nucleotide differences reported between genera. Within a genus, sections of closely related taxa are recoverable in phylogenetic analyses, in most cases, with low sequence divergence within sections. ITS sequences available in GenBank have been aligned with data generated for this project, resulting in a comprehensive sequence library of 151 sequences representing all genera of cypripedioid orchids: 70 Paphiopedilum taxa, 16 Phragmipedium taxa, and 14 Cypripedium taxa, as well as represen- tatives from Selenipedium and the monotypic genus Mexipedium (Phragmipedium) xerophyticum. Addi- tionally, several organelle intron regions have been screened for variation among genera and species. Both the chloroplast řrnS-M and the mitochondrial NAD1 intron regions, which varied between genera in nu- cleotide substitutions and indels, hold promise for increasing ability to distinguish between these orchids. The set of DNA markers examined for this project are diagnostic of these genera, appear to be robust, and are suitable for rapid assay to avoid unnecessary complication in the legitimate trade of orchids listed in CITES Appendix </p>","language":"English","publisher":"Marie Selby Botanical Gardens Inc","usgsCitation":"Morrison, C., Hovatter, K., Eackles, M.S., Spidle, A., and King, T., 2005, Molecular identification of cypripedioid orchids in international trade: Selbyana, v. 26, no. 1-2, p. 196-216.","productDescription":"21 p.","startPage":"196","endPage":"216","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":375048,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morrison, Cheryl 0000-0001-9425-691X cmorrison@usgs.gov","orcid":"https://orcid.org/0000-0001-9425-691X","contributorId":202644,"corporation":false,"usgs":true,"family":"Morrison","given":"Cheryl","email":"cmorrison@usgs.gov","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":789781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hovatter, Katie","contributorId":224949,"corporation":false,"usgs":false,"family":"Hovatter","given":"Katie","email":"","affiliations":[],"preferred":false,"id":789782,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eackles, Michael S. meackles@usgs.gov","contributorId":4371,"corporation":false,"usgs":true,"family":"Eackles","given":"Michael","email":"meackles@usgs.gov","middleInitial":"S.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":789783,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Spidle, A.P.","contributorId":93429,"corporation":false,"usgs":true,"family":"Spidle","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":789784,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"King, T.L.","contributorId":93416,"corporation":false,"usgs":true,"family":"King","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":789785,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70589,"text":"fs20053046 - 2005 - USGS California Water Science Center water programs in California","interactions":[],"lastModifiedDate":"2016-08-17T14:17:51","indexId":"fs20053046","displayToPublicDate":"2005-05-26T00:00:00","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":"2005-3046","title":"USGS California Water Science Center water programs in California","docAbstract":"<p><span>California is threatened by many natural hazards&mdash;fire, floods, landslides, earthquakes. The State is also threatened by longer-term problems, such as hydrologic effects of climate change, and human-induced problems, such as overuse of ground water and degradation of water quality. The threats and problems are intensified by increases in population, which has risen to nearly 36.8 million. For the USGS California Water Science Center, providing scientific information to help address hazards, threats, and hydrologic issues is a top priority. To meet the demands of a growing California, USGS scientific investigations are helping State and local governments improve emergency management, optimize resources, collect contaminant-source and -mobility information, and improve surface- and ground-water quality. USGS hydrologic studies and data collection throughout the State give water managers quantifiable and detailed scientific information that can be used to plan for development and to protect and more efficiently manage resources. The USGS, in cooperation with state, local, and tribal agencies, operates more than 500 instrument stations, which monitor streamflow, ground-water levels, and surface- and ground-water constituents to help protect water supplies and predict the threats of natural hazards. 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,{"id":70590,"text":"sir20055092 - 2005 - Historic and naturalized monthly streamflow for selected sites in the Red River of the North Basin in North Dakota, Minnesota, and South Dakota, 1931-2001","interactions":[],"lastModifiedDate":"2018-03-05T16:09:32","indexId":"sir20055092","displayToPublicDate":"2005-05-26T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5092","title":"Historic and naturalized monthly streamflow for selected sites in the Red River of the North Basin in North Dakota, Minnesota, and South Dakota, 1931-2001","docAbstract":"<p><span>Historic monthly streamflow data were compiled and missing historic and naturalized monthly streamflow data were estimated to develop a database of updated streamflow data for January 1931 through December 2001 (the data-development period) for 35 sites in the Red River of the North Basin. Of the 35 sites, 4 had gaged historic monthly streamflow data for the entire data-development period, 10 had gaged historic monthly streamflow data for part of the data-development period, and 21 had no gaged historic monthly streamflow data. To develop the database, a modified drainage-area ratio method, a maintenance of variance extension type 1 method, and a water-balance method were used to estimate the missing historic monthly streamflow data. Naturalized streamflow for the 35 sites was estimated by eliminating the hydrologic effects of Orwell Dam, Reservation Dam, White Rock Dam, Baldhill Dam, surfacewater withdrawals, and return flows.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055092","usgsCitation":"Emerson, D.G., 2005, Historic and naturalized monthly streamflow for selected sites in the Red River of the North Basin in North Dakota, Minnesota, and South Dakota, 1931-2001 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5092, vi, 228 p., https://doi.org/10.3133/sir20055092.","productDescription":"vi, 228 p.","numberOfPages":"235","onlineOnly":"Y","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":185832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6891,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5092/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.1,45.96666666666667 ], [ -100.1,49 ], [ -94.43333333333334,49 ], [ -94.43333333333334,45.96666666666667 ], [ -100.1,45.96666666666667 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691287","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70585,"text":"fs20053065 - 2005 - USGS California Water Science Center Streamgage Program","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20053065","displayToPublicDate":"2005-05-25T00:00:00","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":"2005-3065","title":"USGS California Water Science Center Streamgage Program","language":"ENGLISH","doi":"10.3133/fs20053065","usgsCitation":"Shulters, M.V., 2005, USGS California Water Science Center Streamgage Program (Online only): U.S. Geological Survey Fact Sheet 2005-3065, 2 p., https://doi.org/10.3133/fs20053065.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6889,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2005-3065/","linkFileType":{"id":5,"text":"html"}},{"id":121167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3065.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a81","contributors":{"authors":[{"text":"Shulters, Michael V. shulters@usgs.gov","contributorId":1023,"corporation":false,"usgs":true,"family":"Shulters","given":"Michael","email":"shulters@usgs.gov","middleInitial":"V.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":282686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70584,"text":"sir20055095 - 2005 - Water quality of streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001","interactions":[],"lastModifiedDate":"2018-03-16T13:36:05","indexId":"sir20055095","displayToPublicDate":"2005-05-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5095","title":"Water quality of streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001","docAbstract":"<p>Data for the Red River of the North (Red River) Basin in Minnesota, North Dakota, and South Dakota were analyzed to determine whether the water quality of streams in the basin is adequate to meet future needs. For the Red River at Emerson, Manitoba, site, pH values, water temperatures, and dissolved-oxygen concentrations generally were within the criteria established for the protection of aquatic life. Dissolved-solids concentrations ranged from 245 to 1,100 milligrams per liter. Maximum sulfate and chloride concentrations were near, but did not exceed, the established secondary maximum contaminant level. The trace elements considered potentially harmful generally were at concentrations that were less than the established guidelines, standards, and criteria. The concentrations of lead that were detected may have occurred as a result of sample contamination.&nbsp;</p><p>&nbsp;For the Red River upstream from Emerson, Manitoba, sites, pH and other field values rarely exceeded the criteria established for the protection of aquatic life. Many constituent concentrations for the Red River below Fargo, N. site exceeded water-quality guidelines, standards, and criteria. However, the trace-element exceedances could be natural or could be related to pollution or sample contamination.</p><p>&nbsp;Many of the tributaries in the western part of the Red River Basin had median specific-conductance values that were greater than 1,000 microsiemens per centimeter. Sulfate concentrations occasionally exceeded the established drinking-water standard. Median arsenic concentrations were 6 micrograms per liter or less, and maximum concentrations rarely exceeded the 10-microgram-per-liter drinking-water standard that is scheduled to take effect in 2006. The small concentrations of lead, mercury, and selenium that occasionally were detected may have been a result of sample contamination or other factors. The tributaries in the eastern part of the Red River Basin had median specific-conductance values that were less than 1,000 microsiemens per centimeter.&nbsp;</p><p>&nbsp;Concentrations of pesticides that were detected and that had regulatory limits were less than the cited water-quality guidelines, standards, and criteria. Concentrations of compounds that were detected generally were less than the sediment- quality standards and criteria.</p><p>&nbsp;The data considered in this report generally provide a good baseline from which to evaluate changes in water-quality conditions. However, because many of the trace elements detected, including lead and mercury, may have been the result of sample contamination, additional data are needed to confirm that trace-element concentrations generally are low. Concentrations of major ions, including sulfate, and specific conductance may continue to approach drinking-water standards during periods of low flow because the streams, particularly those in the western part of the basin, are sustained mostly by ground-water discharge that generally has large dissolved-solids concentrations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055095","usgsCitation":"Tornes, L.H., 2005, Water quality of streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001: U.S. Geological Survey Scientific Investigations Report 2005-5095, vi, 81 p., https://doi.org/10.3133/sir20055095.","productDescription":"vi, 81 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":185743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6888,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055095/","linkFileType":{"id":5,"text":"html"}},{"id":352611,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5095/pdf/report.pdf"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -101,45.8 ], [ -101,79 ], [ -94.43333333333334,79 ], [ -94.43333333333334,45.8 ], [ -101,45.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699125","contributors":{"authors":[{"text":"Tornes, Lan H.","contributorId":70484,"corporation":false,"usgs":true,"family":"Tornes","given":"Lan","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184413,"text":"70184413 - 2005 - Saline tracer visualized with three-dimensional electrical resistivity tomography: Field-scale spatial moment analysis","interactions":[],"lastModifiedDate":"2018-10-31T10:27:27","indexId":"70184413","displayToPublicDate":"2005-05-24T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Saline tracer visualized with three-dimensional electrical resistivity tomography: Field-scale spatial moment analysis","docAbstract":"<p><span>Cross-well electrical resistivity tomography (ERT) was used to monitor the migration of a saline tracer in a two-well pumping-injection experiment conducted at the Massachusetts Military Reservation in Cape Cod, Massachusetts. After injecting 2200 mg/L of sodium chloride for 9 hours, ERT data sets were collected from four wells every 6 hours for 20 days. More than 180,000 resistance measurements were collected during the tracer test. Each ERT data set was inverted to produce a sequence of 3-D snapshot maps that track the plume. In addition to the ERT experiment a pumping test and an infiltration test were conducted to estimate horizontal and vertical hydraulic conductivity values. Using modified moment analysis of the electrical conductivity tomograms, the mass, center of mass, and spatial variance of the imaged tracer plume were estimated. Although the tomograms provide valuable insights into field-scale tracer migration behavior and aquifer heterogeneity, standard tomographic inversion and application of Archie's law to convert electrical conductivities to solute concentration results in underestimation of tracer mass. Such underestimation is attributed to (1) reduced measurement sensitivity to electrical conductivity values with distance from the electrodes and (2) spatial smoothing (regularization) from tomographic inversion. The center of mass estimated from the ERT inversions coincided with that given by migration of the tracer plume using 3-D advective-dispersion simulation. The 3-D plumes seen using ERT exhibit greater apparent dispersion than the simulated plumes and greater temporal spreading than observed in field data of concentration breakthrough at the pumping well.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/2004WR003460","usgsCitation":"Singha, K., and Gorelick, S.M., 2005, Saline tracer visualized with three-dimensional electrical resistivity tomography: Field-scale spatial moment analysis: Water Resources Research, v. 41, no. 5, W05023; 17 p. , https://doi.org/10.1029/2004WR003460.","productDescription":"W05023; 17 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477662,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004wr003460","text":"Publisher Index Page"},{"id":337104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-24","publicationStatus":"PW","scienceBaseUri":"58c1263fe4b014cc3a3d34c2","contributors":{"authors":[{"text":"Singha, Kamini","contributorId":76733,"corporation":false,"usgs":true,"family":"Singha","given":"Kamini","affiliations":[],"preferred":false,"id":681369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorelick, Steven M.","contributorId":8784,"corporation":false,"usgs":true,"family":"Gorelick","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":681370,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70581,"text":"wdrMARI041 - 2005 - Water resources data for Massachusetts and Rhode Island, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"wdrMARI041","displayToPublicDate":"2005-05-20T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MA-RI-04-1","title":"Water resources data for Massachusetts and Rhode Island, water year 2004","docAbstract":"This report includes records of stage, discharge, and water quality of streams; contents and elevation of lakes and ponds; and water levels of ground-water wells. This volume contains discharge records for 112 gaging stations; stage records for 2 gaging stations; stage records for 2 ponds; month-end contents of 1 reservoir; precipitation totals at 6 gaging stations; water quality for 21 gaging stations; air temperature at 2 climatological stations; and water levels for 131 observation wells. Locations of these sites are shown in figures 1 and 2. Hydrologic data were collected at many sites that were not involved in the systematic data-collection program; these data are published as miscellaneous discharge measurements, miscellaneous surface-water-quality, and miscellaneous ground-water-quality data. The data in this report represent that part of the National Water Information System (NWIS) operated by the U.S. Geological Survey and cooperating State and Federal agencies in Massachusetts and Rhode Island.","language":"ENGLISH","doi":"10.3133/wdrMARI041","usgsCitation":"Socolow, R., Comeau, L., and Murino, D., 2005, Water resources data for Massachusetts and Rhode Island, water year 2004: U.S. Geological Survey Water Data Report MA-RI-04-1, 326 p. : photographs, https://doi.org/10.3133/wdrMARI041.","productDescription":"326 p. : photographs","costCenters":[],"links":[{"id":185742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6887,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ma-04/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f400f","contributors":{"authors":[{"text":"Socolow, R.S.","contributorId":17639,"corporation":false,"usgs":true,"family":"Socolow","given":"R.S.","affiliations":[],"preferred":false,"id":282682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Comeau, L.Y.","contributorId":52254,"corporation":false,"usgs":true,"family":"Comeau","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":282684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murino, Domenic Jr.","contributorId":42649,"corporation":false,"usgs":true,"family":"Murino","given":"Domenic","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":282683,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70578,"text":"fs20053029 - 2005 - Assessing sandhill crane roosting habitatalong the Platte River, Nebraska","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"fs20053029","displayToPublicDate":"2005-05-19T00:00:00","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":"2005-3029","title":"Assessing sandhill crane roosting habitatalong the Platte River, Nebraska","docAbstract":"Each spring approximately 500,000 sandhill cranes and some endangered whooping cranes use the Central Platte River Valley in Nebraska as a staging habitat during their migration north to breeding and nesting grounds in Canada, Alaska, and the Siberian Arctic. Over the last century changes in the flow of the river have altered the river channels and the distribution of roost sites. USGS researchers studied linkages between water flow, sediment supply, channel morphology, and preferred sites for crane roosting. These results are useful for estimating crane populations and for providing resource managers with techniques to understand crane habitats.","language":"ENGLISH","doi":"10.3133/fs20053029","usgsCitation":"Kinzel, P., Nelson, J.M., and Parker, R.S., 2005, Assessing sandhill crane roosting habitatalong the Platte River, Nebraska: U.S. Geological Survey Fact Sheet 2005-3029, 2 p., https://doi.org/10.3133/fs20053029.","productDescription":"2 p.","costCenters":[],"links":[{"id":6860,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2005-3029/","linkFileType":{"id":5,"text":"html"}},{"id":121206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3029.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672a52","contributors":{"authors":[{"text":"Kinzel, P.J.","contributorId":27834,"corporation":false,"usgs":true,"family":"Kinzel","given":"P.J.","affiliations":[],"preferred":false,"id":282679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, J. M.","contributorId":68687,"corporation":false,"usgs":true,"family":"Nelson","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":282680,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":282681,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70577,"text":"fs20053034 - 2005 - People and water in the Assabet River basin, eastern Massachusetts","interactions":[],"lastModifiedDate":"2018-04-03T11:33:24","indexId":"fs20053034","displayToPublicDate":"2005-05-19T00:00:00","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":"2005-3034","title":"People and water in the Assabet River basin, eastern Massachusetts","docAbstract":"An accounting of the inflows, outflows, and uses of water in the rapidly developing Assabet River Basin, along Interstate 495 in eastern Massachusetts, was done to quantify how people's activities alter the hydrologic system. The study identified subbasins and seasons in which outflows resulting from people's activities were relatively large percentages of total flows, and quantified the fraction of streamflow in the Assabet River that is treated wastewater. Computer models of ground-water flow were also used to test how the components of the hydrologic system, particularly streamflow, would change with future development and increased water use. Computer simulations showed that, when water use was increased to currently permitted levels, streamflows in tributaries would decrease, particularly during the low-flow period. In the Assabet River, increased wastewater discharges resulted in a slight increase in total streamflow and an increase in the fraction of streamflow in the river that is wastewater, relative to existing conditions.","language":"ENGLISH","doi":"10.3133/fs20053034","usgsCitation":"DeSimone, L.A., 2005, People and water in the Assabet River basin, eastern Massachusetts: U.S. Geological Survey Fact Sheet 2005-3034, 6 p., https://doi.org/10.3133/fs20053034.","productDescription":"6 p.","costCenters":[],"links":[{"id":121205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3034.bmp"},{"id":6859,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2005-3034/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688755","contributors":{"authors":[{"text":"DeSimone, Leslie A. 0000-0003-0774-9607 ldesimon@usgs.gov","orcid":"https://orcid.org/0000-0003-0774-9607","contributorId":195635,"corporation":false,"usgs":true,"family":"DeSimone","given":"Leslie","email":"ldesimon@usgs.gov","middleInitial":"A.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70573,"text":"sir20045202 - 2005 - Precipitation-runoff processes in the Feather River basin, northeastern California, and streamflow predictability, water years 1971-97","interactions":[],"lastModifiedDate":"2026-01-09T16:01:36.591205","indexId":"sir20045202","displayToPublicDate":"2005-05-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5202","title":"Precipitation-runoff processes in the Feather River basin, northeastern California, and streamflow predictability, water years 1971-97","docAbstract":"<p>Precipitation-runoff processes in the Feather River Basin of northern California determine short- and long-term streamflow variations that are of considerable local, State, and Federal concern. The river is an important source of water and power for the region. The basin forms the headwaters of the California State Water Project. Lake Oroville, at the outlet of the basin, plays an important role in flood management, water quality, and the health of fisheries as far downstream as the Sacramento-San Joaquin Delta. Existing models of the river simulate streamflow in hourly, daily, weekly, and seasonal time steps, but cannot adequately describe responses to climate and land-use variations in the basin. New spatially detailed precipitation-runoff models of the basin have been developed to simulate responses to climate and land-use variations at a higher spatial resolution than was available previously. This report characterizes daily rainfall, snowpack evolution, runoff, water and energy balances, and streamflow variations from, and within, the basin above Lake Oroville. The new model's ability to predict streamflow is assessed. The Feather River Basin sits astride geologic, topographic, and climatic divides that establish a hydrologic character that is relatively unusual among the basins of the Sierra Nevada. It straddles a north-south geologic transition in the Sierra Nevada between the granitic bedrock that underlies and forms most of the central and southern Sierra Nevada and volcanic bedrock that underlies the northernmost parts of the range (and basin). Because volcanic bedrock generally is more permeable than granitic, the northern, volcanic parts of the basin contribute larger fractions of ground-water flow to streams than do the southern, granitic parts of the basin. The Sierra Nevada topographic divide forms a high altitude ridgeline running northwest to southeast through the middle of the basin. The topography east of this ridgeline is more like the rain-shadowed basins of the northeastern Sierra Nevada than the uplands of most western Sierra Nevada river basins. The climate is mediterranean, with most of the annual precipitation occurring in winter. Because the basin includes large areas that are near the average snowline, rainfall and rain-snow mixtures are common during winter storms. Consequently, the overall timing and rates of runoff from the basin are highly sensitive to winter temperature fluctuations. The models were developed to simulate runoff-generating processes in eight drainages of the Feather River Basin. Together, these models simulate streamflow from 98 percent of the basin above Lake Oroville. The models simulate daily water and heat balances, snowpack evolution and snowmelt, evaporation and transpiration, subsurface water storage and outflows, and streamflow to key streamflow gage sites. The drainages are modeled as 324 hydrologic-response units, each of which is assumed homogeneous in physical characteristics and response to precipitation and runoff. The models were calibrated with emphasis on reproducing monthly streamflow rates, and model simulations were compared to the total natural inflows into Lake Oroville as reconstructed by the California Department of Water Resources for April-July snowmelt seasons from 1971 to 1997. The models are most sensitive to input values and patterns of precipitation and soil characteristics. The input precipitation values were allowed to vary on a daily basis to reflect available observations by making daily transformations to an existing map of long-term mean monthly precipitation rates that account for altitude and rain-shadow effects. The models effectively simulate streamflow into Lake Oroville during water years (October through September) 1971-97, which is demonstrated in hydrographs and statistical results presented in this report.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045202","usgsCitation":"Koczot, K.M., Jeton, A.E., McGurk, B., and Dettinger, M., 2005, Precipitation-runoff processes in the Feather River basin, northeastern California, and streamflow predictability, water years 1971-97: U.S. Geological Survey Scientific Investigations Report 2004-5202, 92 p., https://doi.org/10.3133/sir20045202.","productDescription":"92 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":6857,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5202/index.html","linkFileType":{"id":5,"text":"html"}},{"id":186650,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","country":"United States","otherGeospatial":"Northeastern California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.84912109375,\n              39.04478604850143\n            ],\n            [\n              -119.94873046875,\n              39.04478604850143\n            ],\n            [\n              -119.94873046875,\n              41.96765920367816\n            ],\n            [\n              -122.84912109375,\n              41.96765920367816\n            ],\n            [\n              -122.84912109375,\n              39.04478604850143\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b98d","contributors":{"authors":[{"text":"Koczot, Kathryn M. 0000-0001-5728-9798 kmkoczot@usgs.gov","orcid":"https://orcid.org/0000-0001-5728-9798","contributorId":2039,"corporation":false,"usgs":true,"family":"Koczot","given":"Kathryn","email":"kmkoczot@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jeton, Anne E.","contributorId":45351,"corporation":false,"usgs":true,"family":"Jeton","given":"Anne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGurk, Bruce","contributorId":74457,"corporation":false,"usgs":true,"family":"McGurk","given":"Bruce","affiliations":[],"preferred":false,"id":282675,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dettinger, Michael D. 0000-0002-7509-7332","orcid":"https://orcid.org/0000-0002-7509-7332","contributorId":31743,"corporation":false,"usgs":true,"family":"Dettinger","given":"Michael D.","affiliations":[],"preferred":false,"id":282673,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}