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,{"id":45087,"text":"wri20024229 - 2002 - Observed and predicted pier scour in Maine","interactions":[],"lastModifiedDate":"2025-04-18T13:33:04.983561","indexId":"wri20024229","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4229","title":"Observed and predicted pier scour in Maine","docAbstract":"Pier-scour and related data were collected and analyzed for nine high river flows at eight bridges across Maine from 1997 through 2001. Six bridges had multiple piers. Fifteen of 23 piers where data were measured during a high flow had observed maximum scour depths ranging from 0.5 feet (ft) to 12.0 ft. No pier scour was observed at the remaining eight piers. The maximum predicted pier-scour depths associated with the 23 piers were computed using the equations in the Federal Highway Administration's Hydraulic Engineering Circular number 18 (HEC-18), with data collected for this study. The predicted HEC-18 maximum pier-scour depths were compared to the observed maximum pier-scour depths. The HEC-18 pier-scour equations are intended to be envelope equations, ideally never underpredicting scour depths and not appreciably overpredicting them. The HEC-18 pier-scour equations performed well for rivers in Maine. Twenty-two out of 23 pier-scour depths were overpredicted by 0.7 ft to 18.3 ft. One pier-scour depth was underpredicted by 4.5 ft. For one pier at each of two bridges, large amounts of debris lodged on the piers after high-flow measurements were made at those sites. The scour associated with the debris increased the maximum pier-scour depths by about 5 ft in each case.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri20024229","collaboration":"Prepared in cooperation with the Maine Department of Transportation","usgsCitation":"Hodgkins, G.A., and Lombard, P., 2002, Observed and predicted pier scour in Maine: U.S. Geological Survey Water-Resources Investigations Report 2002-4229, iv, 22 p., https://doi.org/10.3133/wri20024229.","productDescription":"iv, 22 p.","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":135867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9910,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4229/wrir024229.pdf","text":"Report","size":"1.37 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 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,{"id":50504,"text":"ofr02287 - 2002 - Barrier island elevations relevant to potential storm impacts; 1, Techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:11:19","indexId":"ofr02287","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-287","title":"Barrier island elevations relevant to potential storm impacts; 1, Techniques","language":"ENGLISH","doi":"10.3133/ofr02287","usgsCitation":"Elko, N.A., Sallenger, Guy, K.K., Stockdon, H.F., and Morgan, K., 2002, Barrier island elevations relevant to potential storm impacts; 1, Techniques: U.S. Geological Survey Open-File Report 2002-287, 1 folded sheet ([6] p.) : col. ill., maps (some col.) ; 28 cm., https://doi.org/10.3133/ofr02287.","productDescription":"1 folded sheet ([6] p.) : col. ill., maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":176274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0287/report-thumb.jpg"},{"id":86329,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0287/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649505","contributors":{"authors":[{"text":"Elko, Nicole A.","contributorId":50960,"corporation":false,"usgs":true,"family":"Elko","given":"Nicole","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sallenger, Jr.","contributorId":105768,"corporation":false,"usgs":true,"family":"Sallenger","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":241631,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guy, Kristy K. kguy@usgs.gov","contributorId":3546,"corporation":false,"usgs":true,"family":"Guy","given":"Kristy","email":"kguy@usgs.gov","middleInitial":"K.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":241628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stockdon, Hilary F. 0000-0003-0791-4676 hstockdon@usgs.gov","orcid":"https://orcid.org/0000-0003-0791-4676","contributorId":2153,"corporation":false,"usgs":true,"family":"Stockdon","given":"Hilary","email":"hstockdon@usgs.gov","middleInitial":"F.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":241627,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morgan, Karen L.M. 0000-0002-2994-5572","orcid":"https://orcid.org/0000-0002-2994-5572","contributorId":95553,"corporation":false,"usgs":true,"family":"Morgan","given":"Karen L.M.","affiliations":[],"preferred":false,"id":241630,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":44961,"text":"wri024186 - 2002 - Guidance on the use of passive-vapor-diffusion samplers to detect volatile organic compounds in ground-water-discharge areas, and example applications in New England","interactions":[],"lastModifiedDate":"2020-02-19T19:29:25","indexId":"wri024186","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4186","title":"Guidance on the use of passive-vapor-diffusion samplers to detect volatile organic compounds in ground-water-discharge areas, and example applications in New England","docAbstract":"Polyethylene-membrane passive-vapor-diffusion samplers, or PVD samplers, have been shown to be an effective and economical reconnaissance tool for detecting and identifying volatile organic compounds (VOCs) in bottom sediments of surface-water bodies in areas of ground-water discharge. The PVD samplers consist of an empty glass vial enclosed in two layers of polyethylene membrane tubing. When samplers are placed in contaminated sediments, the air in the vial equilibrates with VOCs in pore water. 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,{"id":44680,"text":"cir1196F - 2002 - Lead recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"cir1196F","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1196","chapter":"F","title":"Lead recycling in the United States in 1998","docAbstract":"This materials flow study includes a description of lead supply and \r\ndemand factors for the United States to illustrate the extent of lead recycling and to \r\nidentify recycling trends. Understanding the system of materials flow from source to \r\nultimate disposition can assist in improving the management of the use of natural \r\nresources in a manner that is compatible with sound environmental practices. The \r\nquantity of lead recycled in 1998, as a percentage of apparent lead supply, was estimated \r\nto be about 63 percent, and recycling efficiency, to be 95 percent. Of the total lead \r\nconsumed in products for the U.S. market in 1998, an estimated 10 percent was \r\nconsumed in products in which the lead was not readily recyclable.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Flow studies for recycling metal commodities in the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/cir1196F","usgsCitation":"Smith, G.R., 2002, Lead recycling in the United States in 1998 (Version 1.0): U.S. Geological Survey Circular 1196, p. F1-F9, https://doi.org/10.3133/cir1196F.","productDescription":"p. F1-F9","costCenters":[],"links":[{"id":167929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3771,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/c1196f/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8874","contributors":{"authors":[{"text":"Smith, Gerald R.","contributorId":36496,"corporation":false,"usgs":true,"family":"Smith","given":"Gerald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44697,"text":"fs11502 - 2002 - Assessment of stream quality using biological indices at selected sites in the Big Elk and Octoraro Creek basins, Chester County, Pennsylvania, 1981-97","interactions":[],"lastModifiedDate":"2018-02-09T12:44:53","indexId":"fs11502","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"115-02","title":"Assessment of stream quality using biological indices at selected sites in the Big Elk and Octoraro Creek basins, Chester County, Pennsylvania, 1981-97","docAbstract":"<h1>Introduction</h1><p>In 1970, the Chester County Water Resources Authority (Pennsylvania) and the U.S. Geological Survey (USGS) established a long-term water-quality network with the goal of assessing the quality of streams in the county and understanding stream changes in response to urbanization using benthic-macroinvertebrate data. This database represents one of the longest continuous water-quality data sets in the country. Benthic macroinvertebrates are aquatic insects, such as mayﬂies, caddisﬂies, rifﬂe beetles, and midges, and other invertebrates that live on the stream bottom. Benthic macroin-vertebrates are useful in evaluating stream quality because their habitat preference and low motility cause them to be affected directly by substances that enter the aquatic system. By evaluating the diversity and community structure of benthic-macroinvertebrate populations, a determination of stream quality can be made.</p><p>Between 1981 and 1997, the water-quality network consisted of 43 sites in 5 major basins in Chester County—Delaware, Schuylkill, Brandywine, Big Elk and Octoraro, and Red and White Clay. Benthic-macroinvertebrate, water-chemistry, and habitat data were collected each year in October or November during base-ﬂow conditions. Using these data, Reif evaluates the overall water-quality condition of Chester County streams. This Fact Sheet summarizes the key ﬁndings from Reif for streams in the Big Elk and Octoraro Creek Basins. These streams include <strong>East Branch Big Elk Creek</strong> (site 31), <strong>West Branch Big Elk Creek</strong> (site 32), <strong>East Branch Octoraro Creek</strong> (site 33) and <strong>Valley Creek</strong> (site 34). This summary includes an analysis of stream conditions based on benthic-macroinvertebrate samples and an analysis of trends in stream conditions for the 17-year study period.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11502","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority","usgsCitation":"Reif, A.G., 2002, Assessment of stream quality using biological indices at selected sites in the Big Elk and Octoraro Creek basins, Chester County, Pennsylvania, 1981-97: U.S. Geological Survey Fact Sheet 115-02, 4 p., https://doi.org/10.3133/fs11502.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":120555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0115/coverthb.jpg"},{"id":3744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0115/fs20020115.pdf","text":"Report","size":"232 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2002-0115"}],"contact":"<p><a href=\"mailto:dc_pa@usgs.gov\" data-mce-href=\"mailto:dc_pa@usgs.gov\">Director</a>, <a href=\"https://pa.water.usgs.gov/\" data-mce-href=\"https://pa.water.usgs.gov/\">Pennsylvania Water Science Center </a><br> U.S. Geological Survey <br> 215 Limekiln Road <br> New Cumberland, PA 17070</p>","tableOfContents":"<ul><li>Introduction</li><li>Study Approach</li><li>Stream-Quality Designation Criteria</li><li>Stream-Quality Assessment</li><li>Trends in Benthic-Macroinvertebrate and Chemical Data</li><li>Summary</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671d72","contributors":{"authors":[{"text":"Reif, Andrew G. 0000-0002-5054-5207 agreif@usgs.gov","orcid":"https://orcid.org/0000-0002-5054-5207","contributorId":2632,"corporation":false,"usgs":true,"family":"Reif","given":"Andrew","email":"agreif@usgs.gov","middleInitial":"G.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40021,"text":"fs13102 - 2002 - Earthquake Hazard in the Heart of the Homeland","interactions":[{"subject":{"id":40021,"text":"fs13102 - 2002 - Earthquake Hazard in the Heart of the Homeland","indexId":"fs13102","publicationYear":"2002","noYear":false,"title":"Earthquake Hazard in the Heart of the Homeland"},"predicate":"SUPERSEDED_BY","object":{"id":79554,"text":"fs20063125 - 2007 - Earthquake hazard in the heart of the homeland","indexId":"fs20063125","publicationYear":"2007","noYear":false,"title":"Earthquake hazard in the heart of the homeland"},"id":1}],"supersededBy":{"id":79554,"text":"fs20063125 - 2007 - Earthquake hazard in the heart of the homeland","indexId":"fs20063125","publicationYear":"2007","noYear":false,"title":"Earthquake hazard in the heart of the homeland"},"lastModifiedDate":"2012-02-02T00:09:56","indexId":"fs13102","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"131-02","title":"Earthquake Hazard in the Heart of the Homeland","language":"ENGLISH","doi":"10.3133/fs13102","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Earthquake Hazard in the Heart of the Homeland (Version 1.0): U.S. Geological Survey Fact Sheet 131-02, 4 p., https://doi.org/10.3133/fs13102.","productDescription":"4 p.","costCenters":[],"links":[{"id":122076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_131_02.jpg"},{"id":3531,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/fs-131-02/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b507","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529934,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156313,"text":"70156313 - 2002 - Tidal asymmetry and variability of bed shear stress and sediment bed flux at a site in San Francisco Bay, USA","interactions":[],"lastModifiedDate":"2018-10-02T09:24:38","indexId":"70156313","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Tidal asymmetry and variability of bed shear stress and sediment bed flux at a site in San Francisco Bay, USA","docAbstract":"<p><span>The relationship between sediment bed flux and bed shear stress during a pair of field experiments in a partially stratified estuary is examined in this paper. Time series of flow velocity, vertical density profiles, and suspended sediment concentration were measured continuously throughout the water column and intensely within 1 meter of the bed. These time series were analyzed to determine bed shear stress, vertical turbulent sediment flux, and mass of sediment suspended in the water column. Resuspension, as inferred from near-bed measurements of vertical turbulent sediment flux, was flood dominant, in accordance with the flood-dominant bed shear stress. Bathymetry-induced residual flow, gravitational circulation, and ebb tide salinity stratification contributed to the flood dominance. In addition to this flow-induced asymmetry, the erodibility of the sediment appears to increase during the first 2 hours of flood tide. Tidal asymmetry in bed shear stress and erodibility help explain an estuarine turbidity maximum that is present during flood tide but absent during ebb tide. Because horizontal advection was insignificant during most of the observation periods, the change in bed mass can be estimated from changes in the total suspended sediment mass. The square wave shape of the bed mass time series indicates that suspended sediment rapidly deposited in an unconsolidated or concentrated benthic suspension layer at slack tides and instantly resuspended when the shear stress became sufficiently large during a subsequent tide. The variability of bed mass associated with the spring/neap cycle (about 60 mg/cm2) is similar to that associated with the semidiurnal tidal cycle.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Fine sediment dynamics in the marine environment","language":"English","publisher":"Elsevier","doi":"10.1016/S1568-2692(02)80010-9","usgsCitation":"Brennan, M.L., Schoellhamer, D., Burau, J.R., and Monismith, S., 2002, Tidal asymmetry and variability of bed shear stress and sediment bed flux at a site in San Francisco Bay, USA, chap. <i>of</i> Fine sediment dynamics in the marine environment, v. 5, p. 93-107, https://doi.org/10.1016/S1568-2692(02)80010-9.","productDescription":"15 p.","startPage":"93","endPage":"107","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":306951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"579889cce4b0589fa1c6bbaa","contributors":{"editors":[{"text":"Winterwerp, J.C.","contributorId":101161,"corporation":false,"usgs":true,"family":"Winterwerp","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":568644,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kranenburg, C.","contributorId":88585,"corporation":false,"usgs":true,"family":"Kranenburg","given":"C.","affiliations":[],"preferred":false,"id":568645,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Brennan, Matthew L.","contributorId":52820,"corporation":false,"usgs":true,"family":"Brennan","given":"Matthew","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":568640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoellhamer, David H. 0000-0001-9488-7340 dschoell@usgs.gov","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":631,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"David H.","email":"dschoell@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":568641,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burau, Jon R. 0000-0002-5196-5035 jrburau@usgs.gov","orcid":"https://orcid.org/0000-0002-5196-5035","contributorId":1500,"corporation":false,"usgs":true,"family":"Burau","given":"Jon","email":"jrburau@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":568642,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Monismith, Stephen G.","contributorId":57228,"corporation":false,"usgs":true,"family":"Monismith","given":"Stephen G.","affiliations":[],"preferred":false,"id":568643,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44934,"text":"wri20024292 - 2002 - Estimates of median flows for streams on the Kansas surface water register","interactions":[{"subject":{"id":44934,"text":"wri20024292 - 2002 - Estimates of median flows for streams on the Kansas surface water register","indexId":"wri20024292","publicationYear":"2002","noYear":false,"displayTitle":"Estimates of Median Flows for Streams on the Kansas Surface Water Register","title":"Estimates of median flows for streams on the Kansas surface water register"},"predicate":"SUPERSEDED_BY","object":{"id":55232,"text":"sir20045032 - 2004 - Estimates of median flows for streams on the 1999 Kansas Surface Water Register","indexId":"sir20045032","publicationYear":"2004","noYear":false,"title":"Estimates of median flows for streams on the 1999 Kansas Surface Water Register"},"id":1}],"supersededBy":{"id":55232,"text":"sir20045032 - 2004 - Estimates of median flows for streams on the 1999 Kansas Surface Water Register","indexId":"sir20045032","publicationYear":"2004","noYear":false,"title":"Estimates of median flows for streams on the 1999 Kansas Surface Water Register"},"lastModifiedDate":"2019-05-28T10:09:50","indexId":"wri20024292","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4292","displayTitle":"Estimates of Median Flows for Streams on the Kansas Surface Water Register","title":"Estimates of median flows for streams on the Kansas surface water register","docAbstract":"<p>The Kansas State Legislature, by enacting Kansas Statute KSA 82a-2001 et. seq., mandated the criteria for determining which Kansas stream segments would be subject to classification by the State. One criterion for the selection as a classified stream segment is based on the statistic of median flow being equal to or greater than 1 cubic foot per second. As specified by KSA 82a-2001 et. seq., median flows were determined from U.S. Geological Survey streamflow-gaging-station data by using the most-recent 10-years of gaged data (KSA) for each streamflow-gaging station. Median flows also were determined by using gaged data from the entire period of record (all-available hydrology, AAH). </p><p>Least-squares multiple regression techniques were used, along with Tobit analyses, to develop equations for estimating median flows for uncontrolled stream segments. The drainage area of the uncontrolled gaging stations used in the regression analyses ranged from 2.06 to 12,004 square miles. A logarithmic transformation of the data was needed to develop the best linear relation for computing median flows. In the regression analyses, the significant climatic and basin characteristics, in order of importance, were drainage area, mean annual precipitation, mean basin permeability, and mean basin slope. Tobit analyses of KSA data yielded a root mean square error of 0.285 logarithmic units, and the best equations using Tobit analyses of AAH data had a root mean square error of 0.247 logarithmic units. </p><p>These equations and an interpolation procedure were used to compute median flows for the uncontrolled stream segments on the Kansas Surface Water Register. Measured median flows from gaging stations were incorporated into the regression-estimated median flows along the stream segments where available. The segments that were uncontrolled were interpolated using gaged data weighted according to the drainage area and the bias between the regression-estimated and gaged flow information. On controlled reaches of Kansas streams, the median flow information was interpolated between gaging stations using only gaged data weighted by drainage area. </p><p>Of the 2,232 total stream segments on the Kansas Surface Water Register, 30 percent of the segments had an estimated median streamflow of less than 1 cubic foot per second when the KSA analysis was used. When the AAH analysis was used, 40 percent of the segments had an estimated median streamflow of less than 1 cubic foot per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri20024292","collaboration":"Prepared in cooperation with the Kansas Department of Health and Environment","usgsCitation":"Perry, C.A., Wolock, D.M., and Artman, J.C., 2002, Estimates of median flows for streams on the Kansas surface water register (Superseded by SIR 2004-5032): U.S. Geological Survey Water-Resources Investigations Report 2002-4292, vi, 107 p., https://doi.org/10.3133/wri20024292.","productDescription":"vi, 107 p.","numberOfPages":"114","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":360235,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4292/wrir20024292.pdf","text":"Report","size":"29.0 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 \"}}]}","edition":"Superseded by SIR 2004-5032","contact":"<p><a href=\"mailto:%20dc_ks@usgs.gov\" data-mce-href=\"mailto:%20dc_ks@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/kswsc\" data-mce-href=\"https://www.usgs.gov/centers/kswsc\">Kansas Water Science Center</a><br>U.S. Geological Survey<br>1217 Biltmore Drive<br>Lawrence, KS 66049</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Factors Affecting Streamflow</li><li>Methods for Estimating Median Flows</li><li>Kansas Surface Water Register</li><li>Basin Characteristics for Stream Segments</li><li>Estimates of Median Flows for Stream Segments</li><li>Internet Dissemination of Results</li><li>Summary</li><li>References Cited</li><li>Appendix A. Kansas Statute KSA 82a–2001 et. seq.</li><li>Appendix B. Median flow information for streamflow-gaging stations used in the interpolation procedure</li><li>Appendix C. Estimated median flows at downstream end of stream segments on the Kansas Surface Water Register</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca94","contributors":{"authors":[{"text":"Perry, Charles A. cperry@usgs.gov","contributorId":2093,"corporation":false,"usgs":true,"family":"Perry","given":"Charles","email":"cperry@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":230717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolock, David M. 0000-0002-6209-938X dwolock@usgs.gov","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":540,"corporation":false,"usgs":true,"family":"Wolock","given":"David","email":"dwolock@usgs.gov","middleInitial":"M.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":230716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Artman, Joshua C.","contributorId":28942,"corporation":false,"usgs":true,"family":"Artman","given":"Joshua","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":230718,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45086,"text":"wri024266 - 2002 - Duration and Frequency Analysis of Lowland Flooding in Western Murfreesboro, Rutherford County, Tennessee, 1998-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:05:00","indexId":"wri024266","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4266","title":"Duration and Frequency Analysis of Lowland Flooding in Western Murfreesboro, Rutherford County, Tennessee, 1998-2000","docAbstract":"Periodic flooding occurs at lowlands and sinkholes in and adjacent to the flood plain of the West Fork Stones River in the western part of Murfreesboro, Tennessee. Flooding in this area commonly occurs during the winter months from December through March. The maximum water level that flood waters will reach in a lowland or sinkhole is controlled by the elevation of the land surrounding the site or the overflow outlet. \r\n\r\nMaximum water levels, independent of overflow from the river, were estimated to be reached in lowlands and sinkholes in the study area every 1 to 4 years. Minor overflow from the West Fork Stones River (less than 1 foot in depth) into the study area has been estimated to occur every 10 to 20 years. Moderate overflow from the river (1 to 2 feet in depth) occurs on average every 20 to 50 years, while major river overflow (in excess of 2 feet in depth) can be expected every 50 years. \r\n\r\nRainfall information for the area, and streamflow and water-level measurements from the West Fork Stones River, lowlands, sinkholes, caves, and wells in the study area were used to develop a flood-prone area map, independent of overflow from the river, for the study area. Water-level duration and frequency relations, independent of overflow from the river, were estimated for several lowlands, sinkholes, and wells in the study area. These relations are used to characterize flooding in lowland areas of western Murfreesboro, Rutherford County, Tennessee.","language":"ENGLISH","doi":"10.3133/wri024266","usgsCitation":"Law, G.S., 2002, Duration and Frequency Analysis of Lowland Flooding in Western Murfreesboro, Rutherford County, Tennessee, 1998-2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4266, iv, 30 p. : ill. (some col.), maps ; 28 cm., https://doi.org/10.3133/wri024266.","productDescription":"iv, 30 p. : ill. (some col.), maps ; 28 cm.","costCenters":[],"links":[{"id":135866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3932,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024266","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db628019","contributors":{"authors":[{"text":"Law, George S. gslaw@usgs.gov","contributorId":2731,"corporation":false,"usgs":true,"family":"Law","given":"George","email":"gslaw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":231082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45090,"text":"wri024213 - 2002 - Use of isotopes to identify sources of ground water, estimate ground-water-flow rates, and assess aquifer vulnerability in the Calumet region of northwestern Indiana and northeastern Illinois","interactions":[],"lastModifiedDate":"2022-09-29T20:47:27.983334","indexId":"wri024213","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4213","title":"Use of isotopes to identify sources of ground water, estimate ground-water-flow rates, and assess aquifer vulnerability in the Calumet region of northwestern Indiana and northeastern Illinois","docAbstract":"<p>Isotope data collected in the Calumet Region of northwestern Indiana and northeastern Illinois, one of the most heavily industrialized regions of the United States, indicated that water in the surficial Calumet aquifer is well mixed. The Calumet aquifer is recharged areally by precipitation and locally may be recharged by surface water. The residence time of ground water in the Calumet aquifer is approximately 5 to 15 years. Ground-water-flow rates through the Calumet aquifer are estimated to be 400 to 2,300 feet per year. The permeable deposits, shallow water table, lack of an overlying confining unit, and proximity to numerous contaminant sources indicate that the Calumet aquifer is vulnerable to contamination.</p><p>Isotopic data indicate that ground water in the confining unit underlying the Calumet aquifer is derived from a variety of sources that include Lake Michigan, modern precipitation, and discharge from the basal Silurian-Devonian bedrock aquifer. The source and apparent age of the water are variable and appear to be affected locally by various geologic and hydraulic factors. The vertical ground-water-flow rate through the unweathered part of the confining unit is about 0.20 feet per year and is about 6.3 feet per year through the weathered part. The data indicate the weathered part of the confining unit may be more vulnerable to contamination than the unweathered confining unit.</p><p>Ground water in the basal Silurian-Devonian aquifer is derived from Lake Michigan, glacial-age water, and modern precipitation. Post-1952 recharge has occurred in the vicinity of Stony Island, Ill. Ground-water recharge of the Silurian-Devonian aquifer may be occurring near Calumet Harbor. The Silurian-Devonian aquifer is vulnerable to contamination where the confining unit is thin or absent or where the integrity of the confining unit has been compromised.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024213","usgsCitation":"Kay, R.T., Bayless, E.R., and Solak, R.A., 2002, Use of isotopes to identify sources of ground water, estimate ground-water-flow rates, and assess aquifer vulnerability in the Calumet region of northwestern Indiana and northeastern Illinois: U.S. Geological Survey Water-Resources Investigations Report 2002-4213, v, 60 p., https://doi.org/10.3133/wri024213.","productDescription":"v, 60 p.","numberOfPages":"70","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":407654,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53971.htm","linkFileType":{"id":5,"text":"html"}},{"id":135956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4213/coverthb.jpg"},{"id":3935,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4213/wri20024213.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2002-4213"}],"country":"United States","state":"Illinois, Indiana","otherGeospatial":"Calumut region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.7333,\n              41.5589\n            ],\n            [\n              -87.0833,\n              41.5589\n            ],\n            [\n              -87.0833,\n              41.7472\n            ],\n            [\n              -87.7333,\n              41.7472\n            ],\n            [\n              -87.7333,\n              41.5589\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Director, Indiana Water Science Center</a><br>U.S. Geological Survey<br>5957 Lakeside Blvd.<br>Indianapolis, IN 46278</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Description of the Study Area</li><li>Study Methods</li><li>Distribution of Isotopes in Ground Water</li><li>Recharge and Sources of Ground Water</li><li>Ground-Wate-Flow Rates and Aquifer Vulnerability</li><li>Summary and Conclusions</li><li>References</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe83","contributors":{"authors":[{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":231088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayless, E. Randall 0000-0002-0357-3635","orcid":"https://orcid.org/0000-0002-0357-3635","contributorId":42586,"corporation":false,"usgs":true,"family":"Bayless","given":"E.","email":"","middleInitial":"Randall","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":231089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Solak, Robert A.","contributorId":50035,"corporation":false,"usgs":true,"family":"Solak","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":231090,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44976,"text":"wri024085 - 2002 - Occurrence and status of volatile organic compounds in ground water from rural, untreated, self-supplied domestic wells in the United States, 1986-99","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024085","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4085","title":"Occurrence and status of volatile organic compounds in ground water from rural, untreated, self-supplied domestic wells in the United States, 1986-99","docAbstract":"Samples of untreated ground water from 1,926 rural, self-supplied domestic wells were analyzed for volatile organic compounds (VOCs) during 1986-99. This information was used to characterize the occurrence and status of VOCs in domestic well water. The samples were either collected as part of the U.S. Geological Survey?s National Water-Quality Assessment (NAWQA) Program occurrence-assessment studies or were compiled by NAWQA from existing ambient ground-water or source-water-quality monitoring programs conducted by local, State, and other Federal agencies. Water samples were collected at the wellhead prior to treatment or storage. In most samples, 55 target VOCs were analyzed, and occurrence and status information generally was computed at an assessment level of 0.2 mg/L (microgram per liter). \r\n\r\nAt least one VOC was detected in 12 percent of samples (232 samples) at an assessment level of 0.2 mg/L. This detection frequency is relatively low compared to the 26 percent detection frequency of at least one VOC in public sup-ply wells sampled by NAWQA, and the difference may be due, in part, to the higher pumping rates, pumping stress factors, and larger contributing areas of public supply wells. Samples with detections of at least one VOC were collected from wells located in 31 of 39 States. \r\n\r\nSolvents were the most frequently detected VOC group with detections in 4.6 percent of samples (89 samples) at an assessment level of 0.2 mg/L. The geographic distribution of detections of some VOC groups, such as fumigants and oxygenates, relates to the use pattern of com-pounds in that group. With the exception of com-pounds used in organic synthesis, detection frequencies of VOCs by group are proportional to the average half-life of compounds in the group. When the organic synthesis group is excluded from the analysis, a good correlation exists between the detection frequency of VOCs by group and average half-life of compounds in the group. \r\n\r\nIndividually, VOCs were not commonly detected at an assessment level of 0.2 mg/L, with the seven most frequently detected VOCs found in only 1 to 5 percent of samples. Mixtures (two or more compounds) were a common mode of occurrence for VOCs when no assessment level was applied, and mixtures occurred in one-half of all samples that contained at least one VOC. Only 1.4 percent of samples (27 samples) had one or more VOC concentrations that exceeded a federally established drinking-water standard or health criterion. Only 0.1 percent of samples (2 samples) had one or more VOC concentrations that exceeded a taste/odor threshold. \r\n\r\nPotential point sources of VOCs near domestic wells are numerous. Leaks from under-ground storage tanks and aboveground storage tanks that hold gasoline, diesel fuel, or heating oil have the potential to be major point sources of contaminants to domestic wells. Shock chlorination may be a source of trichloromethane and other trihalomethanes in some domestic wells. Septic systems are believed to be an important source of contaminants to domestic wells, but extensive research on this subject does not exist. VOCs frequently are ingredients in household products such as cleansers and insecticides, and some VOCs have been found in septic systems.","language":"ENGLISH","doi":"10.3133/wri024085","usgsCitation":"Moran, M.J., Lapham, W.W., Rowe, B.L., and Zogorski, J.S., 2002, Occurrence and status of volatile organic compounds in ground water from rural, untreated, self-supplied domestic wells in the United States, 1986-99: U.S. Geological Survey Water-Resources Investigations Report 2002-4085, ix, 51 p. : ill. (some col.), map (some col.) ; 28 cm., https://doi.org/10.3133/wri024085.","productDescription":"ix, 51 p. : ill. (some col.), map (some col.) ; 28 cm.","costCenters":[],"links":[{"id":3849,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wwwsd.cr.usgs.gov/nawqa/pubs/wrir/wrir02_4085.html","linkFileType":{"id":5,"text":"html"}},{"id":123508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4085/report-thumb.jpg"},{"id":82255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af7e4b07f02db693b61","contributors":{"authors":[{"text":"Moran, Michael J. mjmoran@usgs.gov","contributorId":1047,"corporation":false,"usgs":true,"family":"Moran","given":"Michael","email":"mjmoran@usgs.gov","middleInitial":"J.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":230818,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, Barbara L. blrowe@usgs.gov","contributorId":2673,"corporation":false,"usgs":true,"family":"Rowe","given":"Barbara","email":"blrowe@usgs.gov","middleInitial":"L.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230817,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":230815,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44919,"text":"wri024195 - 2002 - A statistical model for estimating stream temperatures in the Salmon and Clearwater River basins, central Idaho","interactions":[],"lastModifiedDate":"2012-12-06T11:47:57","indexId":"wri024195","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4195","title":"A statistical model for estimating stream temperatures in the Salmon and Clearwater River basins, central Idaho","docAbstract":"A water-quality standard for temperature is critical for the protection of threatened and endangered salmonids, which need cold, clean water to sustain life. The Idaho Department of Environmental Quality has established temperature standards to protect salmonids, yet little is known about the normal range of temperatures of most Idaho streams. A single temperature standard for all streams does not take into account the natural temperature variation of streams or the existence of naturally warm waters. To address these issues and to help the Idaho Department of Environmental Quality revise the existing State temperature standards for aquatic life, temperature data from more than 200 streams and rivers in the salmon and Clearwater River Basins were collected. From these data, a statistical model was developed for estimating stream temperatures on the basis of subbasin and site characteristics and climatic factors. Stream temperatures were monitored hourly for approximately 58 days during July, August, and September 2000 at relatively undisturbed sites in subbasins in the Salmon and Clearwater River Basins in central Idaho. The monitored subbasins vary widely in size, elevation, drainage area, vegetation cover, and other characteristics. The resulting data were analyzed for statistical correlations with subbasin and site characteristics to establish the most important factors affecting stream temperature. Maximum daily average stream temperatures were strongly correlated with elevation and total upstream drainage area; weaker correlations were noted with stream depth and width and aver-age subbasin slope. Stream temperatures also were correlated with certain types of vegetation cover, but these variables were not significant in the final model. The model takes into account seasonal temperature fluctuations, site elevation, total drainage area, average subbasin slope, and the deviation of daily average air temperature from a 30-year normal daily average air temperature. The goodness-of-fit of the model varies with day of the year. Overall, temperatures can be estimated with 95-percent confidence to within approximately plus or minus 4 degrees Celsius. The model performed well when tested on independent stream-temperature data previously collected by the U.S. Geological Survey and other agencies. Although the model provides insight into the natural temperature potential of a wide variety of streams and rivers in the Salmon and Clearwater River Basins, it has limitations. It is based on data collected in only one summer, during which temperatures were higher and streamflows were lower than normal. The effects of changes in streamflow on the effectiveness of the model are not known. Because the model is based on data from minimally disturbed or undisturbed streams, it should not be applied to streams known to be significantly affected by human activities such as disturbance of the streambed, diversion and return of water by irrigation ditches, and removal of riparian vegetation. Finally, because the model is based on data from streams in the Salmon and Clearwater River Basins and reflects climatological and landscape characteristics of those basins, it should not be applied to streams outside this region.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024195","collaboration":"Prepared in cooperation with Idaho Department of Environmental Quality","usgsCitation":"Donato, M.M., 2002, A statistical model for estimating stream temperatures in the Salmon and Clearwater River basins, central Idaho: U.S. Geological Survey Water-Resources Investigations Report 2002-4195, v, 39 p., https://doi.org/10.3133/wri024195.","productDescription":"v, 39 p.","numberOfPages":"46","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":262358,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4195/report.pdf"},{"id":262359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4195/report-thumb.jpg"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0436,43.8741 ], [ -117.0436,47.1367 ], [ -112.9881,47.1367 ], [ -112.9881,43.8741 ], [ -117.0436,43.8741 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62e2","contributors":{"authors":[{"text":"Donato, Mary M.","contributorId":30962,"corporation":false,"usgs":true,"family":"Donato","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":230680,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44009,"text":"ofr02356 - 2002 - Water use in Wisconsin, 2000","interactions":[],"lastModifiedDate":"2015-10-14T12:51:19","indexId":"ofr02356","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-356","title":"Water use in Wisconsin, 2000","docAbstract":"<p>As part of the National Water-Use Information Program, the U.S. Geological Survey (USGS) stores water-use data in standardized format for different catego ries of water use. Information about amounts of water withdrawn, sources of wa ter, how the water was used, and how much water was returned is available to those involved in establishing water-resource policy and to those managing water resources. In 1978, the USGS entered into a cooperative program with the Wisconsin De partment of Natural Resources (WDNR) to inventory water use in Wisconsin. Since that time, four reports summarizing water use have been published (Law rence and Ellefson, 1982; Ellefson and others, 1987; Ellefson and others, 1993; Ellefson and others, 1997). Ellefson and others (1997) present 1995 water-use data in a map and graph format. Because water use changes with time, an update report is periodically required. This report presents 2000 data in the same format as the 1997 report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02356","usgsCitation":"Ellefson, B., Mueller, C., and Buchwald, C., 2002, Water use in Wisconsin, 2000: U.S. Geological Survey Open-File Report 2002-356, 1 Sheet: 36.00 x 27.00 inches, https://doi.org/10.3133/ofr02356.","productDescription":"1 Sheet: 36.00 x 27.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":169311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3767,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://wi.water.usgs.gov/pubs/ofr-02-356/ofr-02-356.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":50573,"text":"ofr02465 - 2002 - A bibliography of terrain modeling (geomorphometry), the quantitative representation of topography: Supplement 4.0","interactions":[],"lastModifiedDate":"2023-06-23T16:51:47.889016","indexId":"ofr02465","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-465","title":"A bibliography of terrain modeling (geomorphometry), the quantitative representation of topography: Supplement 4.0","docAbstract":"<p>Terrain modeling, the practice of ground-surface quantification, is an amalgam of Earth science, mathematics, engineering, and computer science. The discipline is known variously as geomorphometry (or simply morphometry), terrain analysis, and quantitative geomorphology. It continues to grow through myriad applications to hydrology, geohazards mapping, tectonics, sea-floor and planetary exploration, and other fields. Dating nominally to the co-founders of academic geography, Alexander von Humboldt (1808, 1817) and Carl Ritter (1826, 1828), the field was revolutionized late in the 20th Century by the computer manipulation of spatial arrays of terrain heights, or digital elevation models (DEMs), which can quantify and portray ground-surface form over large areas (Maune, 2001). Morphometric procedures are implemented routinely by commercial geographic information systems (GIS) as well as specialized software (Harvey and Eash, 1996; Köthe and others, 1996; ESRI, 1997; Drzewiecki et al., 1999; Dikau and Saurer, 1999; Djokic and Maidment, 2000; Wilson and Gallant, 2000; Breuer, 2001; Guth, 2001; Eastman, 2002). The new Earth Surface edition of the Journal of Geophysical Research, specializing in surficial processes, is the latest of many publication venues for terrain modeling.</p>\n<br/>\n<p>This is the fourth update of a bibliography and introduction to terrain modeling (Pike, 1993, 1995, 1996, 1999) designed to collect the diverse, scattered literature on surface measurement as a resource for the research community. The use of DEMs in science and technology continues to accelerate and diversify (Pike, 2000a). New work appears so frequently that a sampling must suffice to represent the vast literature. This report adds 1636 entries to the 4374 in the four earlier publications1. Forty-eight additional entries correct dead Internet links and other errors found in the prior listings. Chronicling the history of terrain modeling, many entries in this report predate the 1999 supplement. Coverage is representative from about 1800 through early–mid 2002. Papers increasingly are published exclusively or in duplicate on the Internet's World Wide Web; the dates given here for Web addresses (URLs) that lack a print publication indicate a Web site's last update or my last access of it. The bibliography is arranged alphabetically and thus is not readily summarized. This introduction cites about 500 entries, a third of them grouped under 24 morphometric topics, as a guide to the listing's contents. Continuing the practice of previous bibliographies in the series to provide more information on a few applications (see summary of past topics in Pike, 2000a), this report elaborates further on topographic data, putative new parameters, tectonic geomorphology/neo-orometry, biogeography, ice-cap morphometry, results from the Mars Global DEM, landslide-hazard mapping, terrain modeling as physics, Hack's law, and broad-scale computer visualization. The literature of some of these subjects is large, and none of the summaries is intended to more than introduce the topic and comment on some of the current contributions of terrain modeling. Closing the essay is a discussion of pre-1900 papers that trace the evolution of ridge-line and watercourse quantification by descriptive geometry, as well as comments on some new books and an on-line bulletin board.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02465","usgsCitation":"Pike, R.J., 2002, A bibliography of terrain modeling (geomorphometry), the quantitative representation of topography: Supplement 4.0: U.S. Geological Survey Open-File Report 2002-465, 158 p., https://doi.org/10.3133/ofr02465.","productDescription":"158 p.","numberOfPages":"158","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":176704,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02465.jpg"},{"id":283911,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0465/pdf/of02-465.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":283912,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0465/of02-465.txt"},{"id":4381,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0465/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4975e4b0b290850ef30e","contributors":{"authors":[{"text":"Pike, Richard J. rpike@usgs.gov","contributorId":5753,"corporation":false,"usgs":true,"family":"Pike","given":"Richard","email":"rpike@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":241872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50570,"text":"ofr2002460 - 2002 - Sulfur dioxide emission rates from Kīlauea Volcano, Hawai‘i, an update: 1998-2001","interactions":[],"lastModifiedDate":"2021-09-10T11:48:38.670852","indexId":"ofr2002460","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-460","title":"Sulfur dioxide emission rates from Kīlauea Volcano, Hawai‘i, an update: 1998-2001","docAbstract":"<p>Introduction Sulfur dioxide (SO<sub>2</sub>) emission rates from Kilauea Volcano were first measured by Stoiber and Malone (1975) and have been measured on a regular basis since 1979 (Greenland and others, 1985; Casadevall and others, 1987; Elias and others, 1998; Sutton and others, 2001). A compilation of SO<sub>2</sub> emission-rate and wind-vector data from 1979 through 1997 is available as Open-File Report 98-462 (Elias and others, 1998) and on the web at http://hvo.wr.usgs.gov/products/OF98462/. The purpose of this report is to update the existing database through 2001. Kilauea releases SO<sub>2</sub> gas predominantly from its summit caldera and east rift zone (ERZ) (fig. 1), as described in previous reports (Elias and others, 1998; Sutton and others, 2001). These two distinct sources are quantified independently. The summit and east rift zone emission rates reported here were derived using vehicle-based Correlation Spectrometry (COSPEC) measurements as described in Elias and others (1998). In 1998 and 1999, these measurements were augmented with airborne and tripod-based surveys.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2002460","usgsCitation":"Elias, T., and Sutton, A.J., 2002, Sulfur dioxide emission rates from Kīlauea Volcano, Hawai‘i, an update: 1998-2001: U.S. Geological Survey Open-File Report 2002-460, 29 p., https://doi.org/10.3133/ofr2002460.","productDescription":"29 p.","additionalOnlineFiles":"Y","costCenters":[{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":176619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9570,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-460/","linkFileType":{"id":5,"text":"html"}},{"id":389010,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53980.htm"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.30067443847656,\n              19.25605301966429\n            ],\n            [\n              -155.0397491455078,\n              19.25605301966429\n            ],\n            [\n              -155.0397491455078,\n              19.445226820142476\n            ],\n            [\n              -155.30067443847656,\n              19.445226820142476\n            ],\n            [\n              -155.30067443847656,\n              19.25605301966429\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69984c","contributors":{"authors":[{"text":"Elias, Tamar 0000-0002-9592-4518 telias@usgs.gov","orcid":"https://orcid.org/0000-0002-9592-4518","contributorId":3916,"corporation":false,"usgs":true,"family":"Elias","given":"Tamar","email":"telias@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":241855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutton, A. Jefferson","contributorId":47860,"corporation":false,"usgs":true,"family":"Sutton","given":"A.","email":"","middleInitial":"Jefferson","affiliations":[],"preferred":false,"id":241856,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50505,"text":"ofr02288 - 2002 - Barrier island elevations relevant to potential storm impacts: 2, South Atlantic","interactions":[],"lastModifiedDate":"2022-12-12T19:07:06.957123","indexId":"ofr02288","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-288","title":"Barrier island elevations relevant to potential storm impacts: 2, South Atlantic","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02288","usgsCitation":"Elko, N.A., Sallenger, Guy, K.K., and Morgan, K., 2002, Barrier island elevations relevant to potential storm impacts: 2, South Atlantic: U.S. Geological Survey Open-File Report 2002-288, 2 p., https://doi.org/10.3133/ofr02288.","productDescription":"2 p.","costCenters":[],"links":[{"id":410288,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52810.htm","linkFileType":{"id":5,"text":"html"}},{"id":86330,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0288/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0288/report-thumb.jpg"}],"country":"United States","otherGeospatial":"South Atlantic","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.5,\n              25.6167\n            ],\n            [\n              -75.4583,\n              25.6167\n            ],\n            [\n              -75.4583,\n              36.5833\n            ],\n            [\n              -81.5,\n              36.5833\n            ],\n            [\n              -81.5,\n              25.6167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649508","contributors":{"authors":[{"text":"Elko, Nicole A.","contributorId":50960,"corporation":false,"usgs":true,"family":"Elko","given":"Nicole","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sallenger, Jr.","contributorId":105768,"corporation":false,"usgs":true,"family":"Sallenger","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":241635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guy, Kristy K. kguy@usgs.gov","contributorId":3546,"corporation":false,"usgs":true,"family":"Guy","given":"Kristy","email":"kguy@usgs.gov","middleInitial":"K.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":241632,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morgan, Karen L.M. 0000-0002-2994-5572","orcid":"https://orcid.org/0000-0002-2994-5572","contributorId":95553,"corporation":false,"usgs":true,"family":"Morgan","given":"Karen L.M.","affiliations":[],"preferred":false,"id":241634,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50503,"text":"ofr02286 - 2002 - Daily values flow comparison and estimates using program HYCOMP, version 1.0","interactions":[],"lastModifiedDate":"2012-02-02T00:11:19","indexId":"ofr02286","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-286","title":"Daily values flow comparison and estimates using program HYCOMP, version 1.0","docAbstract":"A method used by the U.S. Geological Survey for quality control in computing daily value flow records is to compare hydrographs of computed flows at a station under review to hydrographs of computed flows at a selected index station. The hydrographs are placed on top of each other (as hydrograph overlays) on a light table, compared, and missing daily flow data estimated. This method, however, is subjective and can produce inconsistent results, because hydrographers can differ when calculating acceptable limits of deviation between observed and estimated flows. Selection of appropriate index stations also is judgemental, giving no consideration to the mathematical correlation between the review station and the index station(s).\r\n\r\n \r\n\r\nTo address the limitation of the hydrograph overlay method, a set of software programs, written in the SAS macrolanguage, was developed and designated Program HYDCOMP. The program automatically selects statistically comparable index stations by correlation and regression, and performs hydrographic comparisons and estimates of missing data by regressing daily mean flows at the review station against -8 to +8 lagged flows at one or two index stations and day-of-week. Another advantage that HYDCOMP has over the graphical method is that estimated flows, the criteria for determining the quality of the data, and the selection of index stations are determined statistically, and are reproducible from one user to another.\r\n\r\n \r\n\r\n            HYDCOMP will load the most-correlated index stations into another file containing the ?best index stations,? but will not overwrite stations already in the file. A knowledgeable user should delete unsuitable index stations from this file based on standard error of estimate, hydrologic similarity of candidate index stations to the review station, and knowledge of the individual station characteristics. Also, the user can add index stations not selected by HYDCOMP, if desired.\r\n\r\n \r\n\r\nOnce the file of best-index stations is created, a user may do hydrographic comparison and data estimates by entering the number of the review station, selecting an index station, and specifying the periods to be used for regression and plotting. For example, the user can restrict the regression to ice-free periods of the year to exclude flows estimated during iced conditions. However, the regression could still be used to estimate flow during iced conditions.\r\n\r\n \r\n\r\nHYDCOMP produces the standard error of estimate as a measure of the central scatter of the regression and R-square (coefficient of determination) for evaluating the accuracy of the regression. Output from HYDCOMP includes plots of percent residuals against (1) time within the regression and plot periods, (2) month and day of the year for evaluating seasonal bias in the regression, and (3) the magnitude of flow. For hydrographic comparisons, it plots 2-month segments of hydrographs over the selected plot period showing the observed flows, the regressed flows, the 95 percent confidence limit flows, flow measurements, and regression limits. If the observed flows at the review station remain outside the 95 percent confidence limits for a prolonged period, there may be some error in the flows at the review station or at the index station(s). In addition, daily minimum and maximum temperatures and daily rainfall are shown on the hydrographs, if available, to help indicate whether an apparent change in flow may result from rainfall or from changes in backwater from melting ice or freezing water.\r\n\r\n \r\n\r\nHYDCOMP statistically smooths estimated flows from non-missing flows at the edges of the gaps in data into regressed flows at the center of the gaps using the Kalman smoothing algorithm. Missing flows are automatically estimated by HYDCOMP, but the user also can specify that periods of erroneous, but nonmissing flows, be estimated by the program.","language":"ENGLISH","doi":"10.3133/ofr02286","usgsCitation":"Sanders, C., 2002, Daily values flow comparison and estimates using program HYCOMP, version 1.0 (Version 1.0): U.S. Geological Survey Open-File Report 2002-286, iv, 52 p. : col. ill. ; 28 cm.; 4 refs, https://doi.org/10.3133/ofr02286.","productDescription":"iv, 52 p. : col. ill. ; 28 cm.; 4 refs","costCenters":[],"links":[{"id":176273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4317,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr02286/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e86a","contributors":{"authors":[{"text":"Sanders, Curtis L.","contributorId":94734,"corporation":false,"usgs":true,"family":"Sanders","given":"Curtis L.","affiliations":[],"preferred":false,"id":241626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50582,"text":"ofr02488 - 2002 - Water quality and aquatic toxicity data of 2002 spring thaw conditions in the upper Animas River watershed, Silverton, Colorado","interactions":[],"lastModifiedDate":"2016-12-05T11:13:10","indexId":"ofr02488","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-488","title":"Water quality and aquatic toxicity data of 2002 spring thaw conditions in the upper Animas River watershed, Silverton, Colorado","docAbstract":"This report presents hydrologic, water-quality, and biologic toxicity data collected during the annual spring thaw of 2002 in the upper Animas River watershed near Silverton, Colorado. The spring-thaw runoff is a concern because elevated concentrations of iron oxyhydroxides can contain sorbed trace metals that are potentially toxic to aquatic life. Water chemistry of streams draining the San Juan Mountains is affected by natural acid drainage and weathering of hydrothermal altered volcanic rocks and by more than a century of mining activities. The timing of the spring-thaw sampling effort was determined by reviewing historical climate and stream-flow hydrographs and current weather conditions. Twenty-one water-quality samples were collected between 11:00 AM March 27, 2002 and 6:00 PM March 30, 2002 to characterize water chemistry at the A-72 gage on the upper Animas River below Silverton. Analyses of unfiltered water at the A-72 gage showed a relation between turbidity and total-recoverable iron concentrations, and showed diurnal patterns. Copper and lead concentrations were related to iron concentrations, indicating that these elements are probably sorbed to colloidal iron material. Calcium, strontium, and sulfate concentrations showed overall decreasing trends due to dilution, but the loads of those constituents increased over the sampling period. Nine water-quality samples were collected near the confluence of Mineral Creek with the Animas River, the confluence of Cement Creek with the Animas River, and on the upper Animas River above the confluence with Cement Creek (three samples at each site). A total of six bulk water-toxicity samples were collected before, during, and after the spring thaw from the Animas River at the A-72 gage site. Toxicity tests conducted with the bulk water samples on amphipods did not show strong differences in toxicity among the three sampling periods; however, toxicity of river water to fathead minnows showed a decreasing trend during the course of the study.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02488","usgsCitation":"Fey, D., Wirt, L., Besser, J., and Wright, W.G., 2002, Water quality and aquatic toxicity data of 2002 spring thaw conditions in the upper Animas River watershed, Silverton, Colorado: U.S. Geological Survey Open-File Report 2002-488, ii, 31 p., https://doi.org/10.3133/ofr02488.","productDescription":"ii, 31 p.","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":176229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4387,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-488","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Silverton","otherGeospatial":"Upper Animas River Watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.468017578125,\n              37.06394430056685\n            ],\n            [\n              -108.468017578125,\n              37.87485339352928\n            ],\n            [\n              -107.105712890625,\n              37.87485339352928\n            ],\n            [\n              -107.105712890625,\n              37.06394430056685\n            ],\n            [\n              -108.468017578125,\n              37.06394430056685\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9bb7","contributors":{"authors":[{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":241892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wirt, L.","contributorId":80342,"corporation":false,"usgs":true,"family":"Wirt","given":"L.","email":"","affiliations":[],"preferred":false,"id":241893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Besser, J.M.","contributorId":91569,"corporation":false,"usgs":true,"family":"Besser","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":241894,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wright, W. G.","contributorId":19582,"corporation":false,"usgs":true,"family":"Wright","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":241891,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44668,"text":"pp1658 - 2002 - Crustal structure of the coastal and marine San Francisco Bay region, California","interactions":[],"lastModifiedDate":"2023-09-26T20:23:41.314696","indexId":"pp1658","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1658","title":"Crustal structure of the coastal and marine San Francisco Bay region, California","docAbstract":"<p>As of the time of this writing, the San Francisco Bay region is home to about 6.8 million people, ranking fifth among population centers in the United States. Most of these people live on the coastal lands along San Francisco Bay, the Sacramento River delta, and the Pacific coast. The region straddles the tectonic boundary between the Pacific and North American Plates and is crossed by several strands of the San Andreas Fault system. These faults, which are stressed by about 4 cm of relative plate motion each year, pose an obvious seismic hazard.</p><p>We have many ways to study earthquake faults. Where faults break the land surface, we may learn valuable information needed for hazard assessment, such as cumulative offset, slip rate, and earthquake history. However, many of the major faults in the region are partly submerged beneath San Francisco and Monterey Bays. Although this situation poses problems in gathering observational data for hazard assessment, bay-region waterways provide an opportunity to study faultzone structure by using marine subsurface-imaging techniques, which are easier and cheaper than equivalent studies on land. In 1993, the U.S. Geological Survey (USGS) launched a 5-year project aimed at unearthing the basic science of the submerged San Andreas strike-slip fault system in the San Francisco Bay region with its many interacting strands. Primary project goals were structural, such as to discover how the San Andreas and Hayward Faults are connected or related at depth, to learn how the complex of faults in the San Andreas stepover zone on the Golden Gate platform functions, and to locate previously unknown faults. This volume thus contains mostly structural information about the San Francisco Bay region, much of it gathered through exploratory geophysical experiments.</p><p>The volume is organized “top down,” from studies in the shallowest crust to the base of the crust. The first three chapters are linked through their use of novel geophysical techniques to study earthquake effects, coseismic slip, and shallow stratigraphy. Kayen and others examine crustal structure at very high resolution and demonstrate the use of ground-penetrating-radar tomography to measure the liquefaction potential of coastal sedimentary deposits. McGann and others use microfossils from drill cores along the San Francisco-Oakland Bay Bridge to determine a more detailed late Pleistocene stratigraphy of San Francisco Bay than was previously available. Geist and Zoback use the historical record of a small local tsunami generated by the great 1906 San Francisco earthquake to model the rupture process of that earthquake.</p><p>The last four chapters are dedicated to studies of fault related structure of the seismogenic crust in and around the San Andreas Fault system in the San Francisco Bay region. Jachens and others compile an aeromagnetic anomaly map from new high-resolution flights across the bay region. Some of these anomalies mark the positions of offshore faults, and others are offset by faults, providing constraints on cumulative slip. Hart and others concisely summarize the marine seismic data recorded in and around San Francisco Bay, map the coverage, and provide archival information for those interested in acquiring data.</p><p>The last two chapters present the results of the seismic data that have been analyzed. Bruns and others present their analysis of high-quality intermediate-resolution (~5-km penetration) seismic-reflection data gathered over the complex San Andreas-San Gregorio Fault junction. This junction, which is thought to be where the 1906 San Francisco earthquake originated (see Geist and Zoback, this volume), contains an apparent extensional right stepover in the San Andreas Fault. Finally, Parsons and others review and summarize the results of deep-crustal seismic-reflection experiments and local-earthquake tomographic studies, including previously unpublished data, and provide additional support and discussion for already-published studies.</p><p>In summary, these studies were carried out in an environment where background information on faults in the San Francisco Bay region was sought. Much of the structural information presented here comes from experiments of a style unlikely to be conducted by the USGS in the near future. Together, the chapters in this volume provide a structural framework for a major part of a complex strike-slip fault system.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1658","usgsCitation":"2002, Crustal structure of the coastal and marine San Francisco Bay region, California: U.S. Geological Survey Professional Paper 1658, Report: iii, 145 p.; 2 Plates: 36.00 x 60.00 inches, https://doi.org/10.3133/pp1658.","productDescription":"Report: iii, 145 p.; 2 Plates: 36.00 x 60.00 inches","numberOfPages":"149","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":285114,"rank":9,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch8.pdf","text":"Chapter 8","linkFileType":{"id":1,"text":"pdf"}},{"id":81969,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1658/pdf/plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81968,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1658/pdf/plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81970,"rank":11,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1658/pdf/pp1658.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":3766,"rank":10,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/1658/","linkFileType":{"id":5,"text":"html"}},{"id":421211,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52283.htm","linkFileType":{"id":5,"text":"html"}},{"id":110442,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pp1658.txt","text":"Introduction","linkFileType":{"id":5,"text":"html"},"description":"58863"},{"id":285109,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch3.pdf","text":"Chapter 3","linkFileType":{"id":1,"text":"pdf"}},{"id":285108,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch2.pdf","text":"Chapter 2","linkFileType":{"id":1,"text":"pdf"}},{"id":285113,"rank":8,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch7.pdf","text":"Chapter 7","linkFileType":{"id":1,"text":"pdf"}},{"id":285112,"rank":7,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch6.pdf","text":"Chapter 6","linkFileType":{"id":1,"text":"pdf"}},{"id":285111,"rank":6,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch5.pdf","text":"Chapter 5","linkFileType":{"id":1,"text":"pdf"}},{"id":285110,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1658/pdf/ch4.pdf","text":"Chapter 4","linkFileType":{"id":1,"text":"pdf"}},{"id":126489,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1658/report-thumb.jpg"}],"scale":"150000","projection":"Transverse Mercator projection","datum":"North American Datum of 1927","country":"United States","state":"California","otherGeospatial":"San Francisco Bay Region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,37.25 ], [ -122.75,38.25 ], [ -122.0,38.25 ], [ -122.0,37.25 ], [ -122.75,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f420","contributors":{"editors":[{"text":"Parsons, Thomas E. 0000-0002-0582-4338 tparsons@usgs.gov","orcid":"https://orcid.org/0000-0002-0582-4338","contributorId":2314,"corporation":false,"usgs":true,"family":"Parsons","given":"Thomas","email":"tparsons@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":749309,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":50584,"text":"ofr02492 - 2002 - Publications of the Volcano Hazards Program 2001","interactions":[],"lastModifiedDate":"2014-03-13T10:29:21","indexId":"ofr02492","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-492","title":"Publications of the Volcano Hazards Program 2001","docAbstract":"<p>The Volcano Hazards Program of the U.S. Geological Survey (USGS) is part of the Geologic Hazards Assessments subactivity as funded by Congressional appropriation. Investigations are carried out in the Geology and Hydrology Disciplines of the USGS and with cooperators at the Alaska Division of Geological and Geophysical Surveys, University of Alaska Fairbanks Geophysical Institute, University of Hawaii Hilo, University of Utah, and University of Washington Geophysics Program. This report lists publications from all these institutions.</p>\n<br/>\n<p>This report contains only published papers and maps; numerous abstracts produced for presentations at scientific meetings have not been included. Publications are included based on date of publication with no attempt to assign them to Fiscal Year.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02492","usgsCitation":"Nathenson, M., 2002, Publications of the Volcano Hazards Program 2001: U.S. Geological Survey Open-File Report 2002-492, Report: PDF, 9 p.; Report: TXT, https://doi.org/10.3133/ofr02492.","productDescription":"Report: PDF, 9 p.; Report: TXT","numberOfPages":"9","additionalOnlineFiles":"Y","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":176319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02492.jpg"},{"id":4389,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0492/","linkFileType":{"id":5,"text":"html"}},{"id":283919,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0492/pdf/of02-492.pdf"},{"id":283920,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0492/of02-492.txt"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655e9f","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":241896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50892,"text":"ofr02151 - 2002 - User's manual for computer program BASEPLOT","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr02151","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-151","title":"User's manual for computer program BASEPLOT","docAbstract":"The checking and reviewing of daily records of streamflow within the U.S. Geological Survey is traditionally accomplished by hand-plotting and mentally collating tables of data. The process is time consuming, difficult to standardize, and subject to errors in computation, data entry, and logic. In addition, the presentation of flow data on the internet requires more timely and accurate computation of daily flow records.\r\n\r\n \r\n\r\nBASEPLOT was developed for checking and review of primary streamflow records within the U.S. Geological Survey. Use of BASEPLOT enables users to (1) provide efficiencies during the record checking and review process, (2) improve quality control, (3) achieve uniformity of checking and review techniques of simple stage-discharge relations, and (4) provide a tool for teaching streamflow computation techniques.\r\n\r\nThe BASEPLOT program produces tables of quality control checks and produces plots of rating curves and discharge measurements; variable shift (V-shift) diagrams; and V-shifts converted to stage-discharge plots, using data stored in the U.S. Geological Survey Automatic Data Processing System database. In addition, the program plots unit-value hydrographs that show unit-value stages, shifts, and datum corrections; input shifts, datum corrections, and effective dates; discharge measurements; effective dates for rating tables; and numeric quality control checks. Checklist/tutorial forms are provided for reviewers to ensure completeness of review and standardize the review process. The program was written for the U.S. Geological Survey SUN computer using the Statistical Analysis System (SAS) software produced by SAS Institute, Incorporated.","language":"ENGLISH","doi":"10.3133/ofr02151","usgsCitation":"Sanders, C.L., 2002, User's manual for computer program BASEPLOT: U.S. Geological Survey Open-File Report 2002-151, p. 66, illus. incl. 2 tables, 5 refs; 28 cm., https://doi.org/10.3133/ofr02151.","productDescription":"p. 66, illus. incl. 2 tables, 5 refs; 28 cm.","costCenters":[],"links":[{"id":4656,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr02151/","linkFileType":{"id":5,"text":"html"}},{"id":175695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a030","contributors":{"authors":[{"text":"Sanders, Curtis L. Jr.","contributorId":76391,"corporation":false,"usgs":true,"family":"Sanders","given":"Curtis","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":242564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44670,"text":"pp1662 - 2002 - Studies by the U.S. Geological Survey in Alaska, 2000","interactions":[],"lastModifiedDate":"2023-09-22T21:13:12.247675","indexId":"pp1662","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1662","title":"Studies by the U.S. Geological Survey in Alaska, 2000","docAbstract":"The collection of eight papers that follow continue the series of U.S. Geological Survey (USGS) investigative reports in Alaska under the broad umbrella of the geologic sciences. The series presents new and sometimes-preliminary findings that are of interest to earth scientists in academia, government, and industry; to land and resource managers; and to the general public. Reports presented in Studies by the U.S. Geological Survey in Alaska cover a broad spectrum of topics from various parts of the State (fig. 1), serving to emphasize the diversity of USGS efforts to meet the Nation's needs for earth-science information in Alaska.\r\n\r\nThe papers in this volume are organized under the topics Geologic Framework, Resources, and Environment and Climate. This organization is intended to reflect the scope and objectives of current USGS geologic programs in Alaska. 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,{"id":47513,"text":"ofr2002300 - 2002 - Water-Resources Investigations in Wisconsin, 2002","interactions":[],"lastModifiedDate":"2015-10-15T13:53:40","indexId":"ofr2002300","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-300","title":"Water-Resources Investigations in Wisconsin, 2002","docAbstract":"<p>The statewide average precipitation of 34.83 inches for the 2001 water year was 3.15 inches greater than the normal annual precipitation of 31.68 inches for water years 1961&ndash;90. Average precipitation values affecting streamflow conditions ranged from 92 percent in northeast Wisconsin to 122 percent in southwest Wisconsin with a statewide average of 110 percent (summary tables provided by Lyle Anderson and Ed Hopkins, State Climatology Office, University of Wisconsin, Madison, written commun., 2002).</p>\n<p>The year started out very dry with all regions of the state below 50% of the long-term October average. November precipitation, which was approximately normal, was followed by a December which had record-setting snowfall in most of southern Wisconsin and heavier than normal snowfall the rest of the state. This snowfall total was boosted by the colder than normal temperatures that increased the snowfall depth for water content. The state had the first emergency snow declaration since 1979 with 14 counties receiving aid for December snow clean-up (Wisconsin State Journal, Dec. 15, 2001). Statewide precipitation in January was close to normal. February precipitation was above normal in northwest, north central and all of southern Wisconsin. Elsewhere in the state precipitation was close to normal. In March all regions of the state were very dry with total precipitation below 50% of the long-term March average. In April, the northwest corner of the state had precipitation over three times normal, north central had more than double normal and west central also had precipitation significantly above normal. The rest of the state was also above normal. In May, precipitation in the southern and central parts of the state was about 160 percent of normal. From mid June to mid July there was a statewide dry spell, with most of the state receiving less than 1 inch of rain. August precipitation was close to normal for most of the state with some localized very heavy rains of over 11 inches in southwest and south central Wisconsin. In September, the southern part of the state was above normal, the northwest part of the state was below normal and the rest of the state was about normal.</p>\n<p>Runoff for rivers in the state ranged from 67 percent of the average annual runoff (1964&ndash;2001) at the Kewaunee River site in the northeast part of the state to 160 percent of the average annual runoff (1944&ndash;2001) at the Eau Galle River at Spring Valley site in the west central part of the state. Departures of runoff in the 2001 water year as a percent of long-term average runoff in the state (determined using stations with drainage areas greater than 150 square miles and at least 20 years of record) are shown in figure 4.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2002300","usgsCitation":"Hueschen, K.A., Jones, S., and Fuller, J.A., 2002, Water-Resources Investigations in Wisconsin, 2002 (Version 1.0): U.S. Geological Survey Open-File Report 2002-300, xii, 184 p., https://doi.org/10.3133/ofr2002300.","productDescription":"xii, 184 p.","numberOfPages":"198","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":168725,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12071,"rank":3,"type":{"id":15,"text":"Index 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