{"pageNumber":"1061","pageRowStart":"26500","pageSize":"25","recordCount":46734,"records":[{"id":52657,"text":"wri034246 - 2003 - Precipitation-Runoff Simulations of Current and Natural Streamflow Conditions in the Methow River Basin, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:11:26","indexId":"wri034246","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-4246","title":"Precipitation-Runoff Simulations of Current and Natural Streamflow Conditions in the Methow River Basin, Washington","docAbstract":"Management of the water resources of the Methow River Basin is changing in response to the listing of three species of fish under the Endangered Species Act and the Washington State-legislated watershed-planning process. This report describes the construction and calibration of an enhanced precipitation-runoff model for the Methow River Basin and evaluates the model as a predictive tool for assessing the current and natural streamflow conditions.\r\n\r\nThis study builds upon a previous precipitation-runoff model for the Methow River Basin and validates the current model using a new, more extensive streamflow data network. The major enhancement was the simulation of current flow conditions with the addition of irrigation diversions, returns, and application. The Geographic Information System Weasel characterized the physical properties of the basin and the Modular Modeling System, using the Precipitation-Runoff Modeling System, simulated the hydrologic flow.\r\n\r\nStreamflow was simulated for water years 1992-2001 to calibrate the model to measured streamflows. A sensitivity analysis was completed using nonlinear regression to determine hydrologic parameters pertinent to the modeling results. Simulated and measured streamflow generally showed close agreement, especially during spring runoff from snowmelt. Low-flow or baseflow periods, most restrictive to fish habitation, were simulated reasonably well yet possessed the most uncertainty. Simulations of annual mean streamflow as a percentage of measured annual mean streamflow for the 10-year calibration period at six of the seven streamflow-gaging stations ranged from -35.2 to +26.2 percent, with 65 percent of the simulated values within 15 percent. One station was intentionally calibrated to over-simulate discharge (simulated discharge greater than measured discharge) in order to compensate for observed channel losses not simulated by the model. Simulation of water years 1960-2001 demonstrated great variability in monthly streamflow statistics. The simulated mean monthly flows for 11 streamflow-gaging stations were an average of 2.5 percent higher for water years 1992-2001 than for the entire simulation period. If water year 2001, an extreme drought year, is omitted, simulated mean monthly flows for the 11 streamflow-gaging stations were an average of 9.0 percent higher than for the entire simulation period. The calibrated model also examined the effects of irrigation-canal seepage on streamflow. Irrigation-canal seepage contributed to streamflow throughout the year, with the greatest effect during the irrigation season.\r\n\r\n\r\nManagement of the water resources of the Methow River Basin is changing in response to the listing of three species of fish under the Endangered Species Act and the Washington State-legislated watershed-planning process. This report describes the construction and calibration of an enhanced precipitation-runoff model for the Methow River Basin and evaluates the model as a predictive tool for assessing the current and natural streamflow conditions.\r\n\r\nThis study builds upon a previous precipitation-runoff model for the Methow River Basin and validates the current model using a new, more extensive streamflow data network. The major enhancement was the simulation of current flow conditions with the addition of irrigation diversions, returns, and application. The Geographic Information System Weasel characterized the physical properties of the basin and the Modular Modeling System, using the Precipitation-Runoff Modeling System, simulated the hydrologic flow.\r\n\r\nStreamflow was simulated for water years 1992-2001 to calibrate the model to measured streamflows. A sensitivity analysis was completed using nonlinear regression to determine hydrologic parameters pertinent to the modeling results. Simulated and measured streamflow generally showed close agreement, especially during spring runoff from snowmelt. Low-flow or baseflow periods, most restrictive to fish habitation","language":"ENGLISH","doi":"10.3133/wri034246","usgsCitation":"Ely, D.M., 2003, Precipitation-Runoff Simulations of Current and Natural Streamflow Conditions in the Methow River Basin, Washington: U.S. Geological Survey Water-Resources Investigations Report 2003-4246, 35 p., https://doi.org/10.3133/wri034246.","productDescription":"35 p.","costCenters":[],"links":[{"id":5110,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034246/","linkFileType":{"id":5,"text":"html"}},{"id":178954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf5e","contributors":{"authors":[{"text":"Ely, D. Matthew","contributorId":100052,"corporation":false,"usgs":true,"family":"Ely","given":"D.","email":"","middleInitial":"Matthew","affiliations":[],"preferred":false,"id":245712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51327,"text":"ofr2003331 - 2003 - Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2002 to June 30, 2003","interactions":[],"lastModifiedDate":"2012-03-08T17:16:16","indexId":"ofr2003331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-331","title":"Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2002 to June 30, 2003","docAbstract":"Storm runoff water-quality samples were collected as part of the State of Hawaii Department of Transportation Stormwater Monitoring Program. This program is designed to assess the effects of highway runoff and urban runoff on Halawa Stream. For this program, rainfall data was collected at two sites, continuous streamflow data at three sites, and water-quality data at five sites, which include the three streamflow sites. This report summarizes rainfall, streamflow, and water-quality data collected between July 1, 2002 to June 30, 2003. \r\n\r\n \r\n\r\nA total of 28 samples were collected over five storms during July 1, 2002 to June 30, 2003. For two of the five storms, five grab samples and three flow-weighted timecomposite samples were collected. Grab samples were collected nearly simultaneously at all five sites, and flow-weighted timecomposite samples were collected at the three sites equipped with automatic samplers. The other three storms were partially sampled, where only flow-weighted time-composite samples were collected and/or not all stations were sampled. Samples were analyzed for total suspended solids, total dissolved solids, nutrients, chemical oxygen demand, and selected trace metals (cadmium, copper, lead, and zinc). Grab samples were additionally analyzed for oil and grease, total petroleum hydrocarbons, fecal coliform, and biological oxygen demand. Quality-assurance/qualitycontrol samples, collected during storms and during routine maintenance, were also collected to verify analytical procedures and insure proper cleaning of equipment.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr2003331","collaboration":"Prepared in cooperation with the State of Hawaii Department of Transportation","usgsCitation":"Young, S.T., and Ball, M.T., 2003, Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2002 to June 30, 2003: U.S. Geological Survey Open-File Report 2003-331, v, 30 p., https://doi.org/10.3133/ofr2003331.","productDescription":"v, 30 p.","additionalOnlineFiles":"Y","temporalStart":"2002-07-01","temporalEnd":"2003-06-30","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":176238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4658,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr03-331/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -157.96666666666667,21.333333333333332 ], [ -157.96666666666667,21.466666666666665 ], [ -157.8,21.466666666666665 ], [ -157.8,21.333333333333332 ], [ -157.96666666666667,21.333333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496ec","contributors":{"authors":[{"text":"Young, Stacie T. M.","contributorId":63432,"corporation":false,"usgs":true,"family":"Young","given":"Stacie","email":"","middleInitial":"T. M.","affiliations":[],"preferred":false,"id":243332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ball, Marcael T.J.","contributorId":16904,"corporation":false,"usgs":true,"family":"Ball","given":"Marcael","email":"","middleInitial":"T.J.","affiliations":[],"preferred":false,"id":243331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50669,"text":"ofr02279 - 2003 - Geophysical characterization of fractured bedrock at Site 8, former Pease Air Force Base, Newington, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:10:25","indexId":"ofr02279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2002-279","title":"Geophysical characterization of fractured bedrock at Site 8, former Pease Air Force Base, Newington, New Hampshire","docAbstract":"Borehole-geophysical logs collected from eight wells and direct-current resistivity data from three survey lines were analyzed to characterize the fractured bedrock and identify transmissive fractures beneath the former Pease Air Force Base, Newington, N.H. The following logs were used: caliper, fluid temperature and conductivity, natural gamma radiation, electromagnetic conductivity, optical and acoustic televiewer, and heat-pulse flowmeter. The logs indicate several foliation and fracture trends in the bedrock. Two fracture-correlated lineaments trending 28? and 29?, identified with low-altitude aerial photography, are coincident with the dominant structural trend. The eight boreholes logged at Site 8 generally have few fractures and have yields ranging from 0 to 40 gallons per minute. The fractures that probably resulted in high well yields (20?40 gallons per minute) strike northeast-southwest or by the right hand rule, have an orientation of 215?, 47?, and 51?. \r\n\r\nTwo-dimensional direct-current resistivity methods were used to collect detailed subsurface information about the overburden, bedrock-fracture zone depths, and apparent-dip directions. Analysis of data inversions from data collected with dipole-dipole and Schlumberger arrays indicated electrically conductive zones in the bedrock that are probably caused by fractured rock. These zones are coincident with extensions of fracture-correlated lineaments. The fracture-correlated lineaments and geophysical-survey results indicate a possible northeast-southwest anisotropy to the fractured rock.","language":"ENGLISH","doi":"10.3133/ofr02279","usgsCitation":"Mack, T.J., and Degnan, J.R., 2003, Geophysical characterization of fractured bedrock at Site 8, former Pease Air Force Base, Newington, New Hampshire: U.S. Geological Survey Open-File Report 2002-279, 27 p., https://doi.org/10.3133/ofr02279.","productDescription":"27 p.","costCenters":[],"links":[{"id":170467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4152,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr02-279/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c323","contributors":{"authors":[{"text":"Mack, Thomas J. 0000-0002-0496-3918 tjmack@usgs.gov","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":1677,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"tjmack@usgs.gov","middleInitial":"J.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Degnan, James R. 0000-0002-5665-9010 jrdegnan@usgs.gov","orcid":"https://orcid.org/0000-0002-5665-9010","contributorId":498,"corporation":false,"usgs":true,"family":"Degnan","given":"James","email":"jrdegnan@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57161,"text":"ds101 - 2003 - Comparison of 2002 Water Year and Historical Water-Quality Data, Upper Gunnison River Basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:12:08","indexId":"ds101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"101","title":"Comparison of 2002 Water Year and Historical Water-Quality Data, Upper Gunnison River Basin, Colorado","docAbstract":"Introduction:   \r\nPopulation growth and changes in land-use practices have the potential to affect water quality and quantity in the upper Gunnison River basin. In 1995, the U.S. Geological Survey (USGS), in cooperation with local sponsors, City of Gunnison, Colorado River Water Conservation District, Crested Butte South Metropolitan District, Gunnison County, Mount Crested Butte Water and Sanitation District, National Park Service, Town of Crested Butte, and Upper Gunnison River Water Conservancy District, established a water-quality monitoring program in the upper Gunnison River basin to characterize current water-quality conditions and to assess the effects of increased urban development and other land-use changes on water quality. The monitoring network has evolved into two groups of stations, stations that are considered as long term and stations that are rotational. The long-term stations are monitored to assist in defining temporal changes in water quality (how conditions have changed over time). The rotational stations are monitored to assist in the spatial definition of water-quality conditions (how conditions differ throughout the basin) and to address local and short term concerns. Another group of stations (rotational group 2) will be chosen and sampled beginning in water year 2004. Annual summaries of the water-quality data from the monitoring network provide a point of reference for discussions regarding water-quality sampling in the upper Gunnison River basin. \r\n\r\nThis summary includes data collected during water year 2002. The introduction provides a map of the sampling locations, definitions of terms, and a one-page summary of selected water-quality conditions at the network stations. The remainder of the summary is organized around the data collected at individual stations. Data collected during water year 2002 are compared to historical data (data collected for this network since 1995), state water-quality standards, and federal water-quality guidelines. Data were collected during water year 2002 following USGS protocols (U.S. Geological Survey, variously dated).\r\n\r\n","language":"ENGLISH","doi":"10.3133/ds101","usgsCitation":"Spahr, N., 2003, Comparison of 2002 Water Year and Historical Water-Quality Data, Upper Gunnison River Basin, Colorado: U.S. Geological Survey Data Series 101, 70 p., https://doi.org/10.3133/ds101.","productDescription":"70 p.","costCenters":[],"links":[{"id":5639,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ds101/","linkFileType":{"id":5,"text":"html"}},{"id":180689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4c4","contributors":{"authors":[{"text":"Spahr, N.E.","contributorId":79476,"corporation":false,"usgs":true,"family":"Spahr","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":256299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56954,"text":"wri20034259 - 2003 - Review of Selected References and Data sets on Ambient Ground- and Surface-Water Quality in the Metedeconk River, Toms River, and Kettle Creek Basins, New Jersey, 1980-2001","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"wri20034259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-4259","title":"Review of Selected References and Data sets on Ambient Ground- and Surface-Water Quality in the Metedeconk River, Toms River, and Kettle Creek Basins, New Jersey, 1980-2001","docAbstract":"Surface water and ground water from unconfined aquifers are the primary sources of drinking water for much of the population, about 391,000, in the Metedeconk River, Toms River, and Kettle Creek watersheds in the New Jersey Coastal Plain. The quality of these sources of drinking water is a concern because they are vulnerable to contamination. Indications of the occurrence, distribution, and likely sources and transport mechanisms of certain contaminants were obtained from 48 selected reports and 2 selected data sets on water quality in or near the watersheds (1980-2001). These indications are described and briefly summarized in this report.\r\n\r\nThe findings of studies on ground-water quality indicate that shallow ground water within the study area generally meets primary drinking-water standards, with notable exceptions. Volatile organic compounds, mercury, arsenic, radionuclides, nitrate, and coliform bacteria have been detected in shallow ground water in some areas at levels that exceed Federal and State drinking-water standards. For example, results of analyses of untreated samples collected from more than 13,000 private wells during 1983-99 indicated that concentrations of volatile organic compounds in samples from 7.3 percent of the wells exceeded at least 1 of 11 drinking-water standards, according to records maintained by the Ocean County Health Department. In cases of exceedances, however, water treatment, well replacement, and (or) retesting assured that applicable drinking-water standards were being met at the tap. Reported concentrations of the pesticide chlordane in some areas exceeded the drinking-water standard; few data are available on the occurrence of other pesticides. Studies of nearby areas, however, indicate that pesticide concentrations generally could be expected to be below drinking-water standards. The combination of low pH and low dissolved solids in many areas results in shallow ground water that is highly corrosive and, if untreated, able to leach trace elements and release asbestos fibers from plumbing materials. \r\n\r\nReported concentrations of nitrate, volatile organic compounds, trace elements, and pesticides in samples from the monitored mainstem and tributary streams within the study area generally are below maximum contaminant levels for drinking water or below detection limits. Results of studies in other areas indicate that pesticide concentrations in surface water could be considerably higher during high flows soon after the application of pesticides to crops than during low flows. Fecal coliform bacteria counts in streams vary considerably. Concentrations or counts of these classes of surface-water-quality constituents likely are functions of the intensity and type of upstream development. Results of limited monitoring for radionuclide concentrations reported by the Brick Township Municipal Utilities Authority of the Metedeconk River indicate that radionuclide concentrations or activities do not exceed maximum contaminant levels for drinking water. As a consequence of organic matter in surface water, the formati ultraviolet absorbance in samples from the Metedeconk River and the Toms River exceeded the alternative compliance criteria for source water (2.0 milligrams per liter for total organic carbon and 0.02 absorbance units-liters per milligram-centimeter for specific ultraviolet absorbance) with respect to treatment requirements for preventing elevated concentrations of disinfection by-products in treated water.\r\n\r\nWater-quality and treatment issues associated with use of ground and surface water for potable supply in the study area are related to human activities and naturally occurring factors. Additional monitoring and analysis of ground and surface water would be needed to determine conclusively the occurrence and distribution of some contaminants and the relative importance of various potential contaminant sources, transport and attenuation mechanisms, and transport pathways.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri20034259","collaboration":"Prepared in cooperation with the New Jersey Department of Environmental Protection","usgsCitation":"Nicholson, R.S., Hunchak-Kariouk, K., and Cauller, S.J., 2003, Review of Selected References and Data sets on Ambient Ground- and Surface-Water Quality in the Metedeconk River, Toms River, and Kettle Creek Basins, New Jersey, 1980-2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4259, v, 37 p., https://doi.org/10.3133/wri20034259.","productDescription":"v, 37 p.","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":185336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12148,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri03-4259/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.58333333333333,39.833333333333336 ], [ -74.58333333333333,40.25 ], [ -74,40.25 ], [ -74,39.833333333333336 ], [ -74.58333333333333,39.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6041ac","contributors":{"authors":[{"text":"Nicholson, Robert S. rnichol@usgs.gov","contributorId":2283,"corporation":false,"usgs":true,"family":"Nicholson","given":"Robert","email":"rnichol@usgs.gov","middleInitial":"S.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":255977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunchak-Kariouk, Kathryn","contributorId":41448,"corporation":false,"usgs":true,"family":"Hunchak-Kariouk","given":"Kathryn","email":"","affiliations":[],"preferred":false,"id":255979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cauller, Stephen J. 0000-0002-1823-8813 sjcaulle@usgs.gov","orcid":"https://orcid.org/0000-0002-1823-8813","contributorId":3641,"corporation":false,"usgs":true,"family":"Cauller","given":"Stephen","email":"sjcaulle@usgs.gov","middleInitial":"J.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":false,"id":255978,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51456,"text":"ofr03104 - 2003 - Estimates of deep percolation beneath native vegetation, irrigated fields, and the Amargosa-River Channel, Amargosa Desert, Nye County, Nevada","interactions":[],"lastModifiedDate":"2020-02-10T06:39:14","indexId":"ofr03104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-104","title":"Estimates of deep percolation beneath native vegetation, irrigated fields, and the Amargosa-River Channel, Amargosa Desert, Nye County, Nevada","docAbstract":"<p>The presence and approximate rates of deep percolation beneath areas of native vegetation, irrigated fields, and the Amargosa-River channel in the Amargosa Desert of southern Nevada were evaluated using the chloride mass-balance method and inferred downward velocities of chloride and nitrate peaks. Estimates of deep-percolation rates in the Amargosa Desert are needed for the analysis of regional ground-water flow and transport. An understanding of regional flow patterns is important because ground water originating on the Nevada Test Site may pass through the area before discharging from springs at lower elevations in the Amargosa Desert and in Death Valley. Nine boreholes 10 to 16 meters deep were cored nearly continuously using a hollow-stem auger designed for gravelly sediments. Two boreholes were drilled in each of three irrigated fields in the Amargosa-Farms area, two in the Amargosa-River channel, and one in an undisturbed area of native vegetation. Data from previously cored boreholes beneath undisturbed, native vegetation were compared with the new data to further assess deep percolation under current climatic conditions and provide information on spatial variability.</p><p>The profiles beneath native vegetation were characterized by large amounts of accumulated chloride just below the root zone with almost no further accumulation at greater depths. This pattern is typical of profiles beneath interfluvial areas in arid alluvial basins of the southwestern United States, where salts have been accumulating since the end of the Pleistocene. The profiles beneath irrigated fields and the Amargosa-River channel contained more than twice the volume of water compared to profiles beneath native vegetation, consistent with active deep percolation beneath these sites. Chloride profiles beneath two older fields (cultivated since the 1960’s) as well as the upstream Amargosa-River site were indicative of long-term, quasi-steady deep percolation. Chloride profiles beneath the newest field (cultivated since 1993), the downstream Amargosa-River site, and the edge of an older field were indicative of recently active deep percolation moving previously accumulated salts from the upper profile to greater depths.</p><p>Results clearly indicate that deep percolation and ground-water recharge occur not only beneath areas of irrigation but also beneath ephemeral stream channels, despite the arid climate and infrequency of runoff. Rates of deep percolation beneath irrigated fields ranged from 0.1 to 0.5 m/yr. Estimated rates of deep percolation beneath the Amargosa-River channel ranged from 0.02 to 0.15 m/yr. Only a few decades are needed for excess irrigation water to move through the unsaturated zone and recharge ground water. Assuming vertical, one-dimensional flow, the estimated time for irrigation-return flow to reach the water table beneath the irrigated fields ranged from about 10 to 70 years. In contrast, infiltration from present-day runoff takes centuries to move through the unsaturated zone and reach the water table. The estimated time for water to reach the water table beneath the channel ranged from 140 to 1000 years. These values represent minimum times, as they do not take lateral flow into account. The estimated fraction of irrigation water becoming deep percolation averaged 8 to 16 percent. Similar fractions of infiltration from ephemeral flow events were estimated to become deep percolation beneath the normally dry Amargosa-River channel. In areas where flood-induced channel migration occurs at sub-centennial frequencies, residence times in the unsaturated zone beneath the Amargosa channel could be longer. Estimates of deep percolation presented herein provide a basis for evaluating the importance of recharge from irrigation and channel infiltration in models of ground-water flow from the Nevada Test Site.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr03104","collaboration":"Prepared in cooperation with the Nevada Operations Office, U.S. Department of Energy, under Interagency Agreement DE - AI08 - 96NV11967 ","usgsCitation":"Stonestrom, D.A., Prudic, D.E., Laczniak, R.J., Akstin, K.C., Boyd, R., and Henkelman, K.K., 2003, Estimates of deep percolation beneath native vegetation, irrigated fields, and the Amargosa-River Channel, Amargosa Desert, Nye County, Nevada: U.S. Geological Survey Open-File Report 2003-104, 88 p., https://doi.org/10.3133/ofr03104.","productDescription":"88 p.","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":179304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4464,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-104/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Amargosa Desert","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcb37","contributors":{"authors":[{"text":"Stonestrom, David A. 0000-0001-7883-3385 dastones@usgs.gov","orcid":"https://orcid.org/0000-0001-7883-3385","contributorId":2280,"corporation":false,"usgs":true,"family":"Stonestrom","given":"David","email":"dastones@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":243632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":243633,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laczniak, Randell J.","contributorId":90687,"corporation":false,"usgs":true,"family":"Laczniak","given":"Randell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":243637,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Akstin, Katherine C.","contributorId":88023,"corporation":false,"usgs":true,"family":"Akstin","given":"Katherine","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243636,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boyd, Robert A.","contributorId":16491,"corporation":false,"usgs":true,"family":"Boyd","given":"Robert A.","affiliations":[],"preferred":false,"id":243634,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Henkelman, Katherine K.","contributorId":26751,"corporation":false,"usgs":true,"family":"Henkelman","given":"Katherine","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":243635,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":51528,"text":"ofr03264 - 2003 - Saturation overland flow estimated from TOPMODEL for the conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr03264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-264","title":"Saturation overland flow estimated from TOPMODEL for the conterminous United States","docAbstract":"This 5-kilometer resolution raster (grid) dataset for the conterminous United States represents the average percentage of saturation overland flow in total streamflow estimated by the watershed model TOPMODEL. Saturation overland flow is simulated in TOPMODEL as precipitation that falls on saturated land-surface areas and enters the stream channel.\r\n\r\nTOPMODEL was applied to 5- by 5-kilometer areas across the conterminous United States using national climate, soils, and terrain GIS datasets. The model was run for 1,000 days for each 5- by 5-kilometer area. The average percentage of saturation overland flow in total streamflow was computed for the 1,000-day simulation in each grid cell.","language":"ENGLISH","doi":"10.3133/ofr03264","usgsCitation":"Wolock, D.M., 2003, Saturation overland flow estimated from TOPMODEL for the conterminous United States: U.S. Geological Survey Open-File Report 2003-264, raster digital data, https://doi.org/10.3133/ofr03264.","productDescription":"raster digital data","costCenters":[],"links":[{"id":4548,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/lookup/getspatial?satof48","linkFileType":{"id":5,"text":"html"}},{"id":176328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdba9","contributors":{"authors":[{"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":353,"text":"Kansas Water Science Center","active":false,"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":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":243853,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44647,"text":"wri034007 - 2003 - Explosive-residue compounds resulting from snow avalanche control in the Wasatch Mountains of Utah","interactions":[],"lastModifiedDate":"2017-02-07T15:51:16","indexId":"wri034007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-4007","title":"Explosive-residue compounds resulting from snow avalanche control in the Wasatch Mountains of Utah","docAbstract":"<p>A snow avalanche is a powerful force of nature that can play a significant role in developing mountain landscapes (Perla and Martinelli, 1975). More importantly, loss of life can occur when people are caught in the path of snow avalanches (Grossman, 1999). Increasing winter recreation, including skiing, snowboarding, snowmobiling, snowshoeing, and climbing in mountainous areas, has increased the likelihood of people encountering snow avalanches (fig. 1). Explosives are used by most ski areas and State highway departments throughout the Western United States to control the release of snow avalanches, thus minimizing the loss of human life during winter recreation and highway travel (fig. 2).</p><p>Common explosives used for snow avalanche control include trinitrotoluene (TNT), pentaerythritoltetranitrate (PETN), cyclotrimethylenetrinitramine (RDX), tetrytol, ammonium nitrate, and nitroglycerin (Perla and Martinelli, 1975). During and after snowfall or wind loading of potential avalanche slopes, ski patrollers and Utah Department of Transportation personnel deliver explosive charges onto predetermined targets to artificially release snow avalanches, thereby rendering the slope safer for winter activities. Explosives can be thrown by hand onto target zones or shot from cannons for more remote delivery of explosive charges. Hand-delivered charges typically contain about 2 pounds of TNT or its equivalent (Perla and Martinelli, 1975).</p><p>Depending on the size of the ski area, acreage of potential avalanche terrain, and weather conditions, the annual quantity of explosives used during a season of snow avalanche control can be substantial. For example, the three ski areas of Alta, Snowbird, and Brighton, plus the Utah Department of Transportation, may use as many as 11,200 hand charges per year (Wasatch Powderbird Guides, unpub. data, 1999) for snow avalanche control in Big and Little Cottonwood Canyons (fig. 3). If each charge is assumed to weigh 2 pounds, this equates to about 22,400 pounds of explosive hand charges per year. In addition, 2,240 to 3,160 Avalauncher rounds and 626 to 958 military artillery rounds (explosive mass not specified) are used each year by the three ski areas and the Utah Department of Transportation for snow avalanche control in Big and Little Cottonwood Canyons (Wasatch Powderbird Guides, unpub. data, 1999). The other ski area in Big Cottonwood Canyon, Brighton, uses about 2,000 pounds of explosives per year for snow avalanche control (Michele Weidner, Cirrus Ecological Solutions consultant, written commun., 2001).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri034007","usgsCitation":"Naftz, D.L., Kanagy, L.K., Susong, D.D., Wydoski, D.S., and Kanagy, C.J., 2003, Explosive-residue compounds resulting from snow avalanche control in the Wasatch Mountains of Utah: U.S. Geological Survey Water-Resources Investigations Report 2003-4007, 41 p., https://doi.org/10.3133/wri034007.","productDescription":"41 p.","numberOfPages":"41","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":168928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3755,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034007/","linkFileType":{"id":5,"text":"html"}},{"id":334641,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wrir03-4007/resources/WRIR-03-4007.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8be5","contributors":{"authors":[{"text":"Naftz, David L. 0000-0003-1130-6892 dlnaftz@usgs.gov","orcid":"https://orcid.org/0000-0003-1130-6892","contributorId":1041,"corporation":false,"usgs":true,"family":"Naftz","given":"David","email":"dlnaftz@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kanagy, Leslie K. 0000-0001-5073-8538 lkkanagy@usgs.gov","orcid":"https://orcid.org/0000-0001-5073-8538","contributorId":4543,"corporation":false,"usgs":true,"family":"Kanagy","given":"Leslie","email":"lkkanagy@usgs.gov","middleInitial":"K.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":230191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Susong, David D. ddsusong@usgs.gov","contributorId":1040,"corporation":false,"usgs":true,"family":"Susong","given":"David","email":"ddsusong@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wydoski, Duane S. dwydoski@usgs.gov","contributorId":3734,"corporation":false,"usgs":true,"family":"Wydoski","given":"Duane","email":"dwydoski@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":230190,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kanagy, Christopher J. ckanagy@usgs.gov","contributorId":1201,"corporation":false,"usgs":true,"family":"Kanagy","given":"Christopher","email":"ckanagy@usgs.gov","middleInitial":"J.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":230189,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":51551,"text":"ofr03170 - 2003 - Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr03170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-170","title":"Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2001","docAbstract":"River-channel topographic surveys were conducted and bed-material samples were collected along transects across the Platte River during water year 2001 (October 1, 2000 to September 30, 2001). A total of 57 transect lines or cross sections were established within three study reaches located along the middle channel of the Platte River in a 2,650-acre parcel of land owned by the Nebraska Public Power District (NPPD), hereinafter referred to as the Cottonwood Ranch Property. Five additional cross sections were established downstream of the Cottonwood Ranch Property across the entire width of the Platte River as a component of a proposed future general monitoring program. A development and enhancement plan is proposed by NPPD on the Cottonwood Ranch Property to satisfy their Federal Energy Regulatory Commission (FERC) relicensing guidelines. The goal of the plan is to improve habitat along this reach for endangered species. The United States Geological Survey (USGS) designed a monitoring and research program to study and detect what effects, if any, these channel management actions have on channel morphology and sediment transport within and adjacent to the Cottonwood Ranch Property. This report presents the data-collection methods and summarizes the geomorphic data collected in support of the monitoring program for water year 2001.","language":"ENGLISH","doi":"10.3133/ofr03170","usgsCitation":"Kinzel, P., Parker, R., Nelson, J., Burman, R., and Heckman, A., 2003, Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2001: U.S. Geological Survey Open-File Report 2003-170, 19 p., https://doi.org/10.3133/ofr03170.","productDescription":"19 p.","costCenters":[],"links":[{"id":4585,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_Env_Fluid/downloads.html","linkFileType":{"id":5,"text":"html"}},{"id":179474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c538","contributors":{"authors":[{"text":"Kinzel, Paul","contributorId":100940,"corporation":false,"usgs":true,"family":"Kinzel","given":"Paul","affiliations":[],"preferred":false,"id":243929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Randolph","contributorId":40278,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","affiliations":[],"preferred":false,"id":243925,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Johnathan","contributorId":45384,"corporation":false,"usgs":true,"family":"Nelson","given":"Johnathan","email":"","affiliations":[],"preferred":false,"id":243926,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burman, R.","contributorId":79172,"corporation":false,"usgs":true,"family":"Burman","given":"R.","email":"","affiliations":[],"preferred":false,"id":243927,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Heckman, Aashley","contributorId":81557,"corporation":false,"usgs":true,"family":"Heckman","given":"Aashley","email":"","affiliations":[],"preferred":false,"id":243928,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":51550,"text":"ofr03171 - 2003 - Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr03171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-171","title":"Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2002","docAbstract":"River-channel topographic surveys were conducted and bed-material samples were collected along transects across the Platte River during water year 2002 (October 1, 2001 to September 30, 2002). A total of 57 transect lines or cross sections were established within three study reaches located along the middle channel of the Platte River in a 2,650-acre parcel of land owned by the Nebraska Public Power District (NPPD), hereinafter referred to as the Cottonwood Ranch Property. Five additional cross sections were established downstream of the Cottonwood Ranch Property across the entire width of the Platte River as a component of a proposed future general monitoring program. A development and enhancement plan is proposed by NPPD on the Cottonwood Ranch Property to satisfy their Federal Energy Regulatory Commission (FERC) relicensing guidelines. The goal of the plan is to improve habitat along this reach for endangered species. The United States Geological Survey (USGS) designed a monitoring and research program to study and detect what effects, if any, these channel management actions have on channel morphology and sediment transport within and adjacent to the Cottonwood Ranch Property. This report presents the data-collection methods and summarizes the geomorphic data collected in support of the monitoring program for water year 2002.","language":"ENGLISH","doi":"10.3133/ofr03171","usgsCitation":"Kinzel, P., Parker, R., Nelson, J., Gyetvai, S., Burman, A., and Heckman, A., 2003, Geomorphic data collected within and adjacent to Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2002: U.S. Geological Survey Open-File Report 2003-171, 19 p. + additional files (download is 97.4 MB)(CD available), https://doi.org/10.3133/ofr03171.","productDescription":"19 p. + additional files (download is 97.4 MB)(CD available)","costCenters":[],"links":[{"id":4584,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_Env_Fluid/downloads.html","linkFileType":{"id":5,"text":"html"}},{"id":179473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c552","contributors":{"authors":[{"text":"Kinzel, Paul","contributorId":100940,"corporation":false,"usgs":true,"family":"Kinzel","given":"Paul","affiliations":[],"preferred":false,"id":243923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Randolph","contributorId":40278,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","affiliations":[],"preferred":false,"id":243921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Jonathan","contributorId":100471,"corporation":false,"usgs":true,"family":"Nelson","given":"Jonathan","affiliations":[],"preferred":false,"id":243922,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gyetvai, Steven","contributorId":12561,"corporation":false,"usgs":true,"family":"Gyetvai","given":"Steven","affiliations":[],"preferred":false,"id":243919,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burman, Aaron","contributorId":27546,"corporation":false,"usgs":true,"family":"Burman","given":"Aaron","affiliations":[],"preferred":false,"id":243920,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Heckman, Ashley","contributorId":102138,"corporation":false,"usgs":true,"family":"Heckman","given":"Ashley","affiliations":[],"preferred":false,"id":243924,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":51538,"text":"ofr03195 - 2003 - Quality-Assurance Plan for Water-Quality Activities of the U.S. Geological Survey in Miami, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr03195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-195","title":"Quality-Assurance Plan for Water-Quality Activities of the U.S. Geological Survey in Miami, Florida","docAbstract":"In accordance with guidelines set forth by the Office of Water Quality in the Water Resources Discipline of the U.S. Geological Survey, a quality-assurance plan has been created for use by the U.S. Geological Survey (USGS) in Miami to conduct water-quality activities. This quality-assurance plan documents the standards, policies, and procedures used by the Miami USGS for activities related to the collection, processing, storage, analysis, and publication of water-quality data. The policies and procedures that are documented in this quality-assurance plan for water-quality activities are meant to complement the Miami USGS quality-assurance plans for surface-water and ground-water activities.","language":"ENGLISH","doi":"10.3133/ofr03195","usgsCitation":"Lietz, A.C., 2003, Quality-Assurance Plan for Water-Quality Activities of the U.S. Geological Survey in Miami, Florida: U.S. Geological Survey Open-File Report 2003-195, 72 p., https://doi.org/10.3133/ofr03195.","productDescription":"72 p.","costCenters":[],"links":[{"id":4555,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-195/","linkFileType":{"id":5,"text":"html"}},{"id":178023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651521","contributors":{"authors":[{"text":"Lietz, A. C. (compiler)","contributorId":43847,"corporation":false,"usgs":true,"family":"Lietz","given":"A.","suffix":"(compiler)","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51553,"text":"ofr03146 - 2003 - Flow characteristics at U.S. Geological Survey streamgages in the conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:11:31","indexId":"ofr03146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-146","title":"Flow characteristics at U.S. Geological Survey streamgages in the conterminous United States","docAbstract":"This dataset represents point locations and flow characteristics for current (as of November 20, 2001) and historical U.S. Geological Survey (USGS) streamgages in the conterminous United States. The flow characteristics were computed from the daily streamflow data recorded at each streamgage for the period of record.\r\n\r\nThe attributes associated with each streamgage include:\r\n\r\nStation number\r\nStation name\r\nStation latitude (decimal degrees in North American Datum of 1983, NAD 83)\r\nStation longitude (decimal degrees in NAD 83)\r\nFirst date (year, month, day) of streamflow data\r\nLast date (year, month, day) of streamflow data\r\nNumber of days of streamflow data\r\nMinimum and maximum daily flow for the period of record (cubic feet per second)\r\nPercentiles (1, 5, 10, 20, 25, 50, 75, 80, 90, 95, 99) of daily flow for the period of record (cubic feet per second)\r\nAverage and standard deviation of daily flow for the period of record (cubic feet per second)\r\nMean annual base-flow index (BFI: see supplemental information) computed for the period of record (fraction, ranging from 0 to 1)\r\nYear-to-year standard deviation of the annual base-flow index computed for the period of record (fraction)\r\nNumber of years of data used to compute the base-flow index (years)\r\nReported drainage area (square miles)\r\nReported contributing drainage area (square miles)\r\nNational Water Information System (NWIS)-Web page URL for streamgage\r\nHydrologic Unit Code (HUC, 8 digit)\r\nHydrologic landscape region (HLR)\r\nRiver Reach File 1 (RF1) segment identification number (E2RF1##)\r\n\r\nStation numbers, names, locations, and drainage areas were acquired through the National Water Information System (NWIS)-Web (http://water.usgs.gov/nwis) on November 20, 2001. The streamflow data used to compute flow characteristics were copied from the Water server (water.usgs.gov:/www/htdocs/nwisweb/data1/discharge/) on November 2, 2001.\r\n\r\nThe missing value indicator for all attributes is -99. Some streamflow characteristics are missing for: (1) streamgages measuring flow subject to tidal effects, which cause flow to reverse directions, (2) streamgages with site information but no streamflow data at the time the data were retrieved, and (3) streamgages with record length too short to compute the base-flow index.","language":"ENGLISH","doi":"10.3133/ofr03146","usgsCitation":"Wolock, D., 2003, Flow characteristics at U.S. Geological Survey streamgages in the conterminous United States: U.S. Geological Survey Open-File Report 2003-146, vector digital data, https://doi.org/10.3133/ofr03146.","productDescription":"vector digital data","costCenters":[],"links":[{"id":4587,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/lookup/getspatial?qsitesdd","linkFileType":{"id":5,"text":"html"}},{"id":179481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606794","contributors":{"authors":[{"text":"Wolock, David","contributorId":61528,"corporation":false,"usgs":true,"family":"Wolock","given":"David","affiliations":[],"preferred":false,"id":243935,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51962,"text":"ofr03126 - 2003 - Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases","interactions":[{"subject":{"id":51132,"text":"ofr02475 - 2002 - Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases","indexId":"ofr02475","publicationYear":"2002","noYear":false,"title":"Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases"},"predicate":"SUPERSEDED_BY","object":{"id":51962,"text":"ofr03126 - 2003 - Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases","indexId":"ofr03126","publicationYear":"2003","noYear":false,"title":"Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases"},"id":1}],"lastModifiedDate":"2017-07-14T10:02:23","indexId":"ofr03126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-126","title":"Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases","docAbstract":"<p>High incidences of neurodegenerative diseases, mainly dementia, parkinsonism, and amyotrophic lateral sclerosis, occur on the island of Guam (Koerner, 1952; Kurland and Mulder, 1954). The occurrence and description of the diseases and a summary of the investigations can be found in Perl (1997). The diseases have been more prevalent along the southern coast, particularly the small villages of Umatac, Merizo, and Inarajan (Reed and Brody, 1975; Roman, 1996; and Perl, 1997) (fig. 1), and referred to as the southern villages in this report. Tertiary volcanic rocks underlie most of the southern part of the island, including these villages. The northern part of Guam, with lower incidences of the diseases, consists of carbonate rocks. Epidemiological studies beginning in the early 1950’s failed to show the cause to be genetic etiology (Plato and others, 1986; Zhang and others, 1990). In recent studies, the search for pathogenic mechanisms has shifted to environmental factors. Excesses or deficiencies of various elements from dietary sources including drinking water can have an effect on human health. These deficiencies or excesses can usually be attributed to the geochemical composition of the rocks and derived soils that underlie the area. An example is the high concentration of Se in soil associated with the occurrence of selenosis in adults (Mills, 1996). Yase (1972) suggested that the neurodegenerative diseases on Guam may be related to accumulation of trace elements such as manganese and aluminum, both of which may cause neurodegeneration. It has been suggested that a deficiency in calcium and magnesium in the soil and water along with readily available aluminum could be connected to the occurrence of the diseases (Gajdusek, 1982; Yanagihara and others, 1984; Garruto and others, 1989). Some of the studies investigated metal exposure, particularly aluminum and manganese, and deficiencies in calcium and magnesium (Garruto and others, 1984). Aluminum has been shown to have neurotoxic effects (MacDonald and Martin, 1988), and aluminum has been implicated in the pathogenesis of Alzheimer’s disease and similar dementia by Perl and others (1982). Studies of soils developed on volcanic rocks on Guam and other islands by McLachlan and others (1989) found that soils on Guam averaged 42-fold higher yield of elutable aluminum than soils developed on volcanic rocks on Jamaica or Palau. They did not detect unusually high dietary aluminum or low dietary calcium, but concluded that the soils and possibly the dusts of Guam might be a major source of aluminum entering the body of the inhabitants. </p><p>This study was conducted to investigate the geochemistry of the soils and rocks of the volcanic southern part of the island of Guam, particularly in the vicinity of the three southern villages (Umatac, Merizo, and Inarajan) with high incidences of the diseases. In addition to total chemical analyses of the soils and rocks, various extractions of soils were carried out. Both excesses and deficiencies of various elements were looked for. Because soluble aluminum in the soil was shown by McLachlan and others (1989) to be unusually high, water-soluble extractions as well as sequential extractions of the soils were carried out. In addition, elements such as aluminum found in dust can traverse the nose-brain barrier in experimental animals (Sunderman, 2000) and respiratory epithelium is known to contain the highest concentration of aluminum in the human body (Tipton and others, 1957). The availability of elements, particularly aluminum from human inhalation of dust, derived from soil, was investigated. The available elements were determined by extractions of soils using a simulated lung-fluid extraction.</p><p>In order to compare the results of the chemical data of rocks and soils from Guam to other rocks and soils elsewhere, samples of similar rocks and soils were collected in the western United States and similar analyses to those for the Guam samples carried out. </p><p>The complete chemical analyses of the soils, rocks, and streambed sediments as well as descriptions of the methods used can be found in Miller and others (2002). </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03126","usgsCitation":"Miller, W.R., and Sanzolone, R.F., 2003, Investigation of the possible connection of rock and soil geochemistry to the occurrence of high rates of neurodegenerative diseases on Guam and a hypothesis for the cause of the diseases (Version 1.0; Supersedes Open-File Report 02-475 ): U.S. Geological Survey Open-File Report 2003-126, 44 p., https://doi.org/10.3133/ofr03126.","productDescription":"44 p.","costCenters":[{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"links":[{"id":343848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4508,"rank":99,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-126","linkFileType":{"id":5,"text":"html"}}],"country":"Guam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              144.8554229736328,\n              13.657997240451978\n            ],\n            [\n              144.84855651855466,\n              13.648655851178583\n            ],\n            [\n              144.84237670898438,\n              13.635977659944741\n            ],\n            [\n              144.8334503173828,\n              13.62730271586922\n            ],\n            [\n              144.83276367187497,\n              13.619294792550386\n            ],\n            [\n              144.8334503173828,\n              13.596604204326937\n            ],\n            [\n              144.83207702636716,\n              13.589930088097534\n            ],\n            [\n              144.82315063476562,\n              13.575246370955854\n            ],\n            [\n              144.81628417968747,\n              13.5638992398015\n            ],\n            [\n              144.80941772460938,\n              13.559894240510056\n            ],\n            [\n              144.80941772460938,\n              13.555221655998887\n            ],\n            [\n              144.80735778808594,\n              13.54654375532336\n            ],\n            [\n              144.7998046875,\n              13.535862827464362\n            ],\n            [\n              144.80049133300778,\n              13.527851816968928\n            ],\n            [\n              144.80255126953125,\n              13.521175769019486\n            ],\n            [\n              144.80392456054688,\n              13.514499534006687\n            ],\n            [\n              144.79705810546875,\n              13.510493703244114\n            ],\n            [\n              144.7881317138672,\n              13.509826058240764\n            ],\n            [\n              144.7771453857422,\n              13.507823112015922\n            ],\n            [\n              144.76890563964844,\n              13.503149505416228\n            ],\n            [\n              144.76890563964844,\n              13.496472765758952\n            ],\n            [\n              144.77096557617188,\n              13.490463540396036\n            ],\n            [\n              144.7675323486328,\n              13.486457306148576\n            ],\n            [\n              144.76341247558594,\n              13.481115555981754\n            ],\n            [\n              144.7455596923828,\n              13.480447828815223\n            ],\n            [\n              144.7332000732422,\n              13.481115555981754\n            ],\n            [\n              144.7126007080078,\n              13.479780099783271\n            ],\n            [\n              144.69955444335938,\n              13.47176720592802\n            ],\n            [\n              144.6906280517578,\n              13.465757359351146\n            ],\n            [\n              144.6851348876953,\n              13.47176720592802\n            ],\n            [\n              144.68101501464844,\n              13.46976394051145\n            ],\n            [\n              144.67483520507812,\n              13.466425127537216\n            ],\n            [\n              144.65560913085938,\n              13.466425127537216\n            ],\n            [\n              144.6398162841797,\n              13.46508958930154\n            ],\n            [\n              144.6247100830078,\n              13.459079575009808\n            ],\n            [\n              144.61578369140625,\n              13.451065987933186\n            ],\n            [\n              144.61578369140625,\n              13.44171646419877\n            ],\n            [\n              144.6240234375,\n              13.43303443707212\n            ],\n            [\n              144.63912963867188,\n              13.427023618820577\n            ],\n            [\n              144.63706970214844,\n              13.417673157887597\n            ],\n            [\n              144.64462280273435,\n              13.410326111752818\n            ],\n            [\n              144.65492248535156,\n              13.412329873889819\n            ],\n            [\n              144.65904235839844,\n              13.40498266437702\n            ],\n            [\n              144.65972900390625,\n              13.397635230317864\n            ],\n            [\n              144.656982421875,\n              13.390287571826326\n            ],\n            [\n              144.64942932128906,\n              13.383607687629086\n            ],\n            [\n              144.65011596679688,\n              13.371583429171958\n            ],\n            [\n              144.64393615722656,\n              13.356218226019239\n            ],\n            [\n              144.63775634765625,\n              13.347533113126199\n            ],\n            [\n              144.62951660156247,\n              13.345528811936576\n            ],\n            [\n              144.63363647460938,\n              13.338847687855717\n            ],\n            [\n              144.64393615722656,\n              13.330830095126228\n            ],\n            [\n              144.64805603027344,\n              13.322144069659341\n            ],\n            [\n              144.64942932128906,\n              13.307443931670674\n            ],\n            [\n              144.656982421875,\n              13.289401634020445\n            ],\n            [\n              144.656982421875,\n              13.27469951026642\n            ],\n            [\n              144.6631622314453,\n              13.264006497508065\n            ],\n            [\n              144.67483520507812,\n              13.254649725423508\n            ],\n            [\n              144.6837615966797,\n              13.24863446756652\n            ],\n            [\n              144.69406127929688,\n              13.246629348568725\n            ],\n            [\n              144.71054077148438,\n              13.243287446865004\n            ],\n            [\n              144.72976684570312,\n              13.241950673337922\n            ],\n            [\n              144.73388671875,\n              13.24930283689451\n            ],\n            [\n              144.74212646484375,\n              13.257991471072014\n            ],\n            [\n              144.75723266601562,\n              13.269353062714407\n            ],\n            [\n              144.7661590576172,\n              13.280714123074006\n            ],\n            [\n              144.77371215820312,\n              13.292074651728969\n            ],\n            [\n              144.77508544921875,\n              13.308112139122006\n            ],\n            [\n              144.77439880371094,\n              13.323480401570771\n            ],\n            [\n              144.77508544921875,\n              13.335507056537201\n            ],\n            [\n              144.77439880371094,\n              13.366239121719289\n            ],\n            [\n              144.7785186767578,\n              13.388283626028894\n            ],\n            [\n              144.7833251953125,\n              13.403646783973812\n            ],\n            [\n              144.79225158691406,\n              13.410326111752818\n            ],\n            [\n              144.79087829589844,\n              13.422348433874618\n            ],\n            [\n              144.7998046875,\n              13.419676858742317\n            ],\n            [\n              144.80941772460938,\n              13.426355740831927\n            ],\n            [\n              144.81353759765625,\n              13.435038009690745\n            ],\n            [\n              144.8279571533203,\n              13.439712947377316\n            ],\n            [\n              144.8389434814453,\n              13.449730364019857\n            ],\n            [\n              144.8499298095703,\n              13.457076203381147\n            ],\n            [\n              144.86846923828125,\n              13.47577368642247\n            ],\n            [\n              144.8815155029297,\n              13.486457306148576\n            ],\n            [\n              144.8931884765625,\n              13.490463540396036\n            ],\n            [\n              144.8938751220703,\n              13.498475807268505\n            ],\n            [\n              144.89593505859375,\n              13.505820148970754\n            ],\n            [\n              144.91035461425778,\n              13.511828987642952\n            ],\n            [\n              144.92820739746094,\n              13.519172918153423\n            ],\n            [\n              144.93438720703125,\n              13.529187004103694\n            ],\n            [\n              144.9371337890625,\n              13.541203351336101\n            ],\n            [\n              144.942626953125,\n              13.555889173697548\n            ],\n            [\n              144.94606018066406,\n              13.562564247541179\n            ],\n            [\n              144.9529266357422,\n              13.577248749550982\n            ],\n            [\n              144.95567321777344,\n              13.588595242295824\n            ],\n            [\n              144.9591064453125,\n              13.597939005012236\n            ],\n            [\n              144.9542999267578,\n              13.602610748172255\n            ],\n            [\n              144.94056701660156,\n              13.602610748172255\n            ],\n            [\n              144.931640625,\n              13.603945515004137\n            ],\n            [\n              144.9089813232422,\n              13.608617139653049\n            ],\n            [\n              144.90692138671875,\n              13.617960112295492\n            ],\n            [\n              144.898681640625,\n              13.62730271586922\n            ],\n            [\n              144.89181518554688,\n              13.636644950140424\n            ],\n            [\n              144.87808227539062,\n              13.648655851178583\n            ],\n            [\n              144.86915588378906,\n              13.655995545325037\n            ],\n            [\n              144.86228942871094,\n              13.659331694429515\n            ],\n            [\n              144.8554229736328,\n              13.657997240451978\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0; Supersedes Open-File Report 02-475 ","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a91","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":244553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanzolone, Richard F.","contributorId":88007,"corporation":false,"usgs":true,"family":"Sanzolone","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":244554,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51554,"text":"ofr03145 - 2003 - Hydrologic landscape regions of the United States","interactions":[],"lastModifiedDate":"2013-06-17T13:02:36","indexId":"ofr03145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-145","title":"Hydrologic landscape regions of the United States","docAbstract":"Hydrologic landscape regions (HLRs) in the United States were delineated by using geographic information system (GIS) tools and statistical methods including principal components and cluster analyses. The GIS and statistical analyses were applied to land-surface form, geologic texture (permeability of the soil and bedrock), and climate variables that describe the physical and climatic setting of 43,931 small (roughly 200 square kilometers) watersheds in the United States. The analyses then grouped the watersheds into 20 noncontiguous regions (the HLRs) on the basis of similarities in land-surface form, geologic texture, and climate characteristics. This hydrologic landscape regions dataset contains for each of the 49,931 watersheds the (1) watershed identification number, (2) land-surface form, geologic texture, and climate characteristics for each watershed, and (3) hydrologic landscape region number for each watershed.","language":"English","publisher":"U.S. Geological Service","publisherLocation":"Reston, VA","doi":"10.3133/ofr03145","usgsCitation":"Wolock, D.M., 2003, Hydrologic landscape regions of the United States: U.S. Geological Survey Open-File Report 2003-145, Dataset, https://doi.org/10.3133/ofr03145.","productDescription":"Dataset","costCenters":[],"links":[{"id":179566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4588,"rank":100,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/lookup/getspatial?hlrus","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -179.993809,4.582580 ], [ -179.993809,84.659265 ], [ 179.883210,84.659265 ], [ 179.883210,4.582580 ], [ -179.993809,4.582580 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60679b","contributors":{"authors":[{"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":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":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":243936,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53334,"text":"wdrFL022B - 2003 - Water Resources Data, Florida, Water Year 2002, Volume 2B. South Florida Ground Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wdrFL022B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-02-2B","title":"Water Resources Data, Florida, Water Year 2002, Volume 2B. South Florida Ground Water","docAbstract":"Water resources data for 2002 water year in Florida consists of continuous or daily discharge for 392 streams, periodic discharge for 15 streams, continuous or daily stage for 191 streams, periodic stage for 13 stream, peak discharge for 33 streams, and peak stage for 33 streams, continuous or daily elevations for 14 lakes, periodic elevations for 49 lakes, continuous ground-water levels for 418 wells, periodic ground-water levels for 1287 wells, quality of water data for 116 surface-water sites, and 291 wells. \r\n\r\nThe data for South Florida included continuous or daily discharge for 71 streams, continuous or daily stage for 49 streams, no peak stage discharge for streams, 1 continuous elevation for lake, continuous ground-water levels for 238 wells, periodic ground-water levels for 260 wells, water quality for 24 surface-water sites, and 159 wells. \r\n\r\nThese data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State, and Federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL022B","usgsCitation":"Prinos, S., Overton, K., and Byrne, M., 2003, Water Resources Data, Florida, Water Year 2002, Volume 2B. South Florida Ground Water: U.S. Geological Survey Water Data Report FL-02-2B, 620 p., https://doi.org/10.3133/wdrFL022B.","productDescription":"620 p.","costCenters":[],"links":[{"id":174417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5037,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl022A/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafff","contributors":{"authors":[{"text":"Prinos, S.","contributorId":61089,"corporation":false,"usgs":true,"family":"Prinos","given":"S.","affiliations":[],"preferred":false,"id":247299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Overton, K.","contributorId":53456,"corporation":false,"usgs":true,"family":"Overton","given":"K.","email":"","affiliations":[],"preferred":false,"id":247298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Byrne, M.","contributorId":50210,"corporation":false,"usgs":true,"family":"Byrne","given":"M.","email":"","affiliations":[],"preferred":false,"id":247297,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53278,"text":"wdrME021 - 2003 - Water resources data-Maine, water year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"wdrME021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ME-02-1","title":"Water resources data-Maine, water year 2002","docAbstract":"The Water Resources Division of the U.S. Geological Survey, in cooperation with State, Federal, and other local governmental agencies, obtains a large amount of data pertaining to the water resources of Maine each year. These data, accumulated during the many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State.\r\n\r\n \r\n\r\nWater-resources data for the 2002 water year for Maine consists of records of stage, discharge, ground water levels,water quality of streams and ground-water wells, precipitation quantity, and snow quantity,. This report contains discharge records for: 5 gage-height stations, 61 discharge gaging stations, stream water-quality data for 2 stations, water levels for 19 ground-water wells, water-quality data for 2 ground-water well, precipitation quantity data for 12 stations, and snow quantity data for 82 stations. Additional water data were collected at other sites, not part of the systematic data-collection program, and are published as special study and miscellaneous record.","language":"ENGLISH","doi":"10.3133/wdrME021","usgsCitation":"Stewart, G., Caldwell, J.M., and Cloutier, A., 2003, Water resources data-Maine, water year 2002: U.S. Geological Survey Water Data Report ME-02-1, 250 p., https://doi.org/10.3133/wdrME021.","productDescription":"250 p.","costCenters":[],"links":[{"id":177215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4981,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/WDR-ME-02/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f09ab","contributors":{"authors":[{"text":"Stewart, G.J.","contributorId":62246,"corporation":false,"usgs":true,"family":"Stewart","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":247155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caldwell, J. M.","contributorId":93934,"corporation":false,"usgs":true,"family":"Caldwell","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":247156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cloutier, A.R.","contributorId":26356,"corporation":false,"usgs":true,"family":"Cloutier","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":247154,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52859,"text":"ofr03263 - 2003 - Base-Flow Index Grid for the Conterminous United States","interactions":[],"lastModifiedDate":"2013-05-28T08:49:50","indexId":"ofr03263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2003-263","title":"Base-Flow Index Grid for the Conterminous United States","docAbstract":"This 1-kilometer raster (grid) dataset for the conterminous United States was created by interpolating base-flow index (BFI) values estimated at U.S. Geological Survey (USGS) streamgages. Base flow is the component of streamflow that can be attributed to ground-water discharge into streams.","language":"ENGLISH","doi":"10.3133/ofr03263","usgsCitation":"Wolock, D.M., 2003, Base-Flow Index Grid for the Conterminous United States: U.S. Geological Survey Open-File Report 2003-263, digital data set, https://doi.org/10.3133/ofr03263.","productDescription":"digital data set","costCenters":[],"links":[{"id":4875,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03263/","linkFileType":{"id":5,"text":"html"}},{"id":177995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":272837,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/bfi48grd.xml"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6488ad","contributors":{"authors":[{"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":353,"text":"Kansas Water Science Center","active":false,"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}],"preferred":true,"id":246142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53279,"text":"wdrTN021 - 2003 - Water resources data, Tennessee, water year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"wdrTN021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"TN-02-1","title":"Water resources data, Tennessee, water year 2002","language":"ENGLISH","doi":"10.3133/wdrTN021","usgsCitation":"Flohr, D., Garrett, J., Hamilton, J., and Phillips, T., 2003, Water resources data, Tennessee, water year 2002: U.S. Geological Survey Water Data Report TN-02-1, 442 p., https://doi.org/10.3133/wdrTN021.","productDescription":"442 p.","costCenters":[],"links":[{"id":4982,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/WDR-TN-02/","linkFileType":{"id":5,"text":"html"}},{"id":177216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ebf1","contributors":{"authors":[{"text":"Flohr, D.F.","contributorId":52259,"corporation":false,"usgs":true,"family":"Flohr","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":247158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrett, J.W.","contributorId":87958,"corporation":false,"usgs":true,"family":"Garrett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":247159,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamilton, J.T.","contributorId":99215,"corporation":false,"usgs":true,"family":"Hamilton","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":247160,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phillips, T.D.","contributorId":43845,"corporation":false,"usgs":true,"family":"Phillips","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":247157,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53280,"text":"wdrIN021 - 2003 - U.S. Geological Survey Water Resources Data Indiana Water Year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"wdrIN021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-02-1","title":"U.S. Geological Survey Water Resources Data Indiana Water Year 2002","language":"ENGLISH","doi":"10.3133/wdrIN021","usgsCitation":"Stewart, J., Keeton, C.R., Hammil, L.E., Nguyen, H.T., and Majors, D.K., 2003, U.S. Geological Survey Water Resources Data Indiana Water Year 2002: U.S. Geological Survey Water Data Report IN-02-1, 668 p., https://doi.org/10.3133/wdrIN021.","productDescription":"668 p.","costCenters":[],"links":[{"id":4983,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrin02/","linkFileType":{"id":5,"text":"html"}},{"id":177217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db612f56","contributors":{"authors":[{"text":"Stewart, James A.","contributorId":49824,"corporation":false,"usgs":true,"family":"Stewart","given":"James A.","affiliations":[],"preferred":false,"id":247162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keeton, Charles R.","contributorId":71220,"corporation":false,"usgs":true,"family":"Keeton","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":247163,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hammil, Lowell E.","contributorId":19198,"corporation":false,"usgs":true,"family":"Hammil","given":"Lowell","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":247161,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nguyen, Hieu T.","contributorId":97179,"corporation":false,"usgs":true,"family":"Nguyen","given":"Hieu","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":247165,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Majors, Deborah K.","contributorId":91925,"corporation":false,"usgs":true,"family":"Majors","given":"Deborah","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":247164,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":53281,"text":"wdrMT021 - 2003 - Water Resources Data, Montana, 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"wdrMT021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MT-02-1","title":"Water Resources Data, Montana, 2002","docAbstract":"Water resources data for Montana for the 2002 water year consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels in wells. This report contains discharge records for 244 streamflow-gaging stations; stage or content records for 9 lakes and large reservoirs and content for 31 smaller reservoirs; water-quality records for 142 streamflow stations (42 ungaged), 9 ground-water wells, and 3 lakes; precipitation records for 2 atmospheric-deposition stations; and water-level records for 53 observation wells. Additional water year 2002 data collected at crest-stage gage and miscellaneous-measurement sites were collected but are not published in this report. These data are stored within the District office files in Helena and available on request. These data represent part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Montana.","language":"ENGLISH","doi":"10.3133/wdrMT021","usgsCitation":"Berkas, W.R., White, M.K., Ladd, P.B., Bailey, F.A., and Dodge, K.A., 2003, Water Resources Data, Montana, 2002: U.S. Geological Survey Water Data Report MT-02-1, 721 p., https://doi.org/10.3133/wdrMT021.","productDescription":"721 p.","costCenters":[],"links":[{"id":4984,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrmt02/","linkFileType":{"id":5,"text":"html"}},{"id":177297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb55c","contributors":{"authors":[{"text":"Berkas, Wayne R. wrberkas@usgs.gov","contributorId":425,"corporation":false,"usgs":true,"family":"Berkas","given":"Wayne","email":"wrberkas@usgs.gov","middleInitial":"R.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Melvin K. mwhite@usgs.gov","contributorId":1563,"corporation":false,"usgs":true,"family":"White","given":"Melvin","email":"mwhite@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":247169,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ladd, Patricia B.","contributorId":64321,"corporation":false,"usgs":true,"family":"Ladd","given":"Patricia","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":247170,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bailey, Fred A. fbailey@usgs.gov","contributorId":1561,"corporation":false,"usgs":true,"family":"Bailey","given":"Fred","email":"fbailey@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":247168,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dodge, Kent A. kdodge@usgs.gov","contributorId":1036,"corporation":false,"usgs":true,"family":"Dodge","given":"Kent","email":"kdodge@usgs.gov","middleInitial":"A.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247167,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":53287,"text":"wdrNY021 - 2003 - Water Resources Data New York Water Year 2002, Volume 1. Eastern New York Excluding Long Island","interactions":[],"lastModifiedDate":"2018-12-13T08:43:50","indexId":"wdrNY021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-02-1","title":"Water Resources Data New York Water Year 2002, Volume 1. Eastern New York Excluding Long Island","docAbstract":"Water resources data for the 2002 water year for New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and ground-water levels. This volume contains records for water discharge at 147 gaging stations; stage only at 8 gaging stations; stage and contents at 4 gaging stations, and 18 other lakes and reservoirs; water quality at 29 gaging stations; and water levels at 14 observation wells. Also included are data for 32 crest-stage partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data together with the data in volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Municipal, and Federal agencies in New York.","language":"ENGLISH","doi":"10.3133/wdrNY021","usgsCitation":"Butch, G., Murray, P., Hebert, G., and Weigel, J.F., 2003, Water Resources Data New York Water Year 2002, Volume 1. Eastern New York Excluding Long Island: U.S. Geological Survey Water Data Report NY-02-1, 525 p., https://doi.org/10.3133/wdrNY021.","productDescription":"525 p.","costCenters":[],"links":[{"id":177388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4990,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/wdr-ny-02-1/index.html","linkFileType":{"id":5,"text":"html"}},{"id":360234,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/wdr-ny-02-1/pdf/rept2002.all.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd242","contributors":{"authors":[{"text":"Butch, G.K.","contributorId":63849,"corporation":false,"usgs":true,"family":"Butch","given":"G.K.","affiliations":[],"preferred":false,"id":247183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murray, P.M.","contributorId":33358,"corporation":false,"usgs":true,"family":"Murray","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":247182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hebert, G.J.","contributorId":18445,"corporation":false,"usgs":true,"family":"Hebert","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":247181,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weigel, J. F.","contributorId":74394,"corporation":false,"usgs":true,"family":"Weigel","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":247184,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53333,"text":"wdrFL022A - 2003 - Water Resources Data, Florida, Water Year 2002, Volume 2A. South Florida Surface Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wdrFL022A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-02-2A","title":"Water Resources Data, Florida, Water Year 2002, Volume 2A. South Florida Surface Water","docAbstract":"Water resources data for 2002 water year in Florida consists of continuous or daily discharge for 392 streams, periodic discharge for 15 streams, continuous or daily stage for 191 streams, periodic stage for 13 stream, peak discharge for 33 streams, and peak stage for 33 streams, continuous or daily elevations for 14 lakes, periodic elevations for 49 lakes, continuous ground-water levels for 418 wells, periodic ground-water levels for 1287 wells, quality of water data for 116 surface-water sites, and 291 wells. \r\n\r\nThe data for South Florida included continuous or daily discharge for 71 streams, continuous or daily stage for 49 streams, no peak stage discharge for streams, 1 continuous elevation for lake, continuous ground-water levels for 238 wells, periodic ground-water levels for 260 wells, water quality for 24 surface-water sites, and 159 wells. \r\n\r\nThe data represent the National Water Data System records collected by the U.S. Geological Survey and cooperation with local, state, and federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL022A","usgsCitation":"Price, C., Woolverton, J., and Overton, K., 2003, Water Resources Data, Florida, Water Year 2002, Volume 2A. South Florida Surface Water: U.S. Geological Survey Water Data Report FL-02-2A, 342 p., https://doi.org/10.3133/wdrFL022A.","productDescription":"342 p.","costCenters":[],"links":[{"id":5036,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl022A/","linkFileType":{"id":5,"text":"html"}},{"id":174416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6995d6","contributors":{"authors":[{"text":"Price, C.","contributorId":12910,"corporation":false,"usgs":true,"family":"Price","given":"C.","affiliations":[],"preferred":false,"id":247294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woolverton, J.","contributorId":86415,"corporation":false,"usgs":true,"family":"Woolverton","given":"J.","email":"","affiliations":[],"preferred":false,"id":247296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Overton, K.","contributorId":53456,"corporation":false,"usgs":true,"family":"Overton","given":"K.","email":"","affiliations":[],"preferred":false,"id":247295,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53335,"text":"wdrFL023A - 2003 - Water Resources Data, Florida, Water Year 2002, Volume 3A. Southwest Florida Surface Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wdrFL023A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-02-3A","title":"Water Resources Data, Florida, Water Year 2002, Volume 3A. Southwest Florida Surface Water","docAbstract":"Water resources data for the 2002 water year in Florida consist of continuous or daily discharges for 392 streams, periodic discharge for 15 streams, continuous daily stage for 191 streams, periodic stage for 13 streams, peak stage for 33 streams and peak discharge for 33 streams, continuous or daily elevations for 14 lakes, periodic elevations for 49 lakes; continuous ground-water levels for 418 wells, periodic ground-water levels for 1,287 wells, and quality-of-water data for 116 surface-water sites and 291 wells. \r\n\r\nThe data for Southwest Florida include records of stage, discharge, and water quality of streams; stage, contents, water quality of lakes and reservoirs, and water levels and water quality of ground-water wells. Volume 3A contains continuous or daily discharge for 99 streams, periodic discharge for 11 streams, continuous or daily stage for 63 streams, peak stage and discharge for 7 streams, continuous or daily elevations for 2 lakes, periodic elevations for 26 lakes, and quality-of-water data for 59 surface-water sites. \r\n\r\nThese data represent the national Water Data System records collected by the U.S. Geological Survey and cooperating local, state, and federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL023A","usgsCitation":"Kane, R., and Fletcher, W., 2003, Water Resources Data, Florida, Water Year 2002, Volume 3A. Southwest Florida Surface Water: U.S. Geological Survey Water Data Report FL-02-3A, 552 p., https://doi.org/10.3133/wdrFL023A.","productDescription":"552 p.","costCenters":[],"links":[{"id":5038,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl023A/","linkFileType":{"id":5,"text":"html"}},{"id":174503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba95","contributors":{"authors":[{"text":"Kane, R.L.","contributorId":29873,"corporation":false,"usgs":true,"family":"Kane","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":247300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":247301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53336,"text":"wdrFL023B - 2003 - Water Resources Data, Florida, Water Year 2002, Volume 3B. Southwest Florida Ground Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wdrFL023B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-02-3B","title":"Water Resources Data, Florida, Water Year 2002, Volume 3B. Southwest Florida Ground Water","docAbstract":"Water resources data for the 2002 water year in Florida consist of continuous or daily discharges for 392 streams, periodic discharge for 15 streams, continuous daily stage for 191 streams, periodic stage for 13 streams, peak stage for 33 streams and peak discharge for 33 streams, continuous or daily elevations for 14 lakes, periodic elevations for 49 lakes; continuous ground-water levels for 418 wells, periodic ground-water levels for 1,287 wells, and quality-of-water data for 116 surface-water sites and 291 wells. \r\n\r\nThe data for Southwest Florida include records of stage, discharge, and water quality of streams; stage, contents, water quality of lakes and reservoirs, and water levels and water quality of ground-water wells. Volume 3B contains records for continuous ground-water elevations for 125 wells; periodic ground-water elevations at 31 wells; miscellaneous ground-water elevations at 377 wells; and water quality at 46 ground-water sites. \r\n\r\nThese data represent the national Water Data System records collected by the U.S. Geological Survey and cooperating local, state, and federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL023B","usgsCitation":"Kane, R., and Fletcher, W., 2003, Water Resources Data, Florida, Water Year 2002, Volume 3B. Southwest Florida Ground Water: U.S. Geological Survey Water Data Report FL-02-3B, 276 p., https://doi.org/10.3133/wdrFL023B.","productDescription":"276 p.","costCenters":[],"links":[{"id":5039,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl023B/","linkFileType":{"id":5,"text":"html"}},{"id":174504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbaa9","contributors":{"authors":[{"text":"Kane, R.L.","contributorId":29873,"corporation":false,"usgs":true,"family":"Kane","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":247302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":247303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53427,"text":"wri024296 - 2003 - The Great Lakes Water Balance:  Data availability and annotated bibliography of selected references","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"wri024296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","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":"2002-4296","title":"The Great Lakes Water Balance:  Data availability and annotated bibliography of selected references","docAbstract":"Water balance calculations for the Great Lakes have been made for several decades and are a key component of Great Lakes water management. Despite the importance of the water balance, little has been done to inventory and describe the data available for use in water balance calculations. This report provides a catalog and brief description of major datasets that are used to calculate the Great Lakes water balance. Several additional datasets are identified that could be used to calculate parts of the water balance but currently are not being used. Individual offices and web pages that are useful for attaining these datasets are included. Four specific data gaps are also identified. An annotated bibliography of important publications dealing with the Great Lakes water balance is included. The findings of this investigation permit resource managers and scientists to access data more easily, assess shortcomings of current datasets, and identify which data are not currently being utilized in water balance calculations.","language":"ENGLISH","doi":"10.3133/wri024296","usgsCitation":"Neff, B., and Killian, J.R., 2003, The Great Lakes Water Balance:  Data availability and annotated bibliography of selected references: U.S. Geological Survey Water-Resources Investigations Report 2002-4296, 37 p., https://doi.org/10.3133/wri024296.","productDescription":"37 p.","costCenters":[],"links":[{"id":5210,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glc.org/wateruse/wrmdss/finalreport/pdf/ABpaperFINALPUBLISHED.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c454","contributors":{"authors":[{"text":"Neff, Brian P.","contributorId":27548,"corporation":false,"usgs":true,"family":"Neff","given":"Brian P.","affiliations":[],"preferred":false,"id":247568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Killian, Jason R.","contributorId":94740,"corporation":false,"usgs":true,"family":"Killian","given":"Jason","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":247569,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}