{"pageNumber":"2906","pageRowStart":"72625","pageSize":"25","recordCount":184606,"records":[{"id":53584,"text":"fs09603 - 2003 - Earthquakes-Rattling the Earth's Plumbing System","interactions":[],"lastModifiedDate":"2019-09-06T16:21:33","indexId":"fs09603","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"096-03","title":"Earthquakes-Rattling the Earth's Plumbing System","docAbstract":"

Hydrogeologic responses to earthquakes have been known for decades, and have occurred both close to, and thousands of miles from earthquake epicenters. Water wells have become turbid, dry or begun flowing, discharge of springs and ground water to streams has increased and new springs have formed, and well and surface-water quality have become degraded as a result of earthquakes. Earthquakes affect our Earth’s intricate plumbing system—whether you live near the notoriously active San Andreas Fault in California, or far from active faults in Florida, an earthquake near or far can affect you and the water resources you depend on.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs09603","usgsCitation":"Sneed, M., Galloway, D.L., and Cunningham, W.L., 2003, Earthquakes-Rattling the Earth's Plumbing System: U.S. Geological Survey Fact Sheet 096-03, 5 p., https://doi.org/10.3133/fs09603.","productDescription":"5 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":494,"text":"Office of Groundwater","active":false,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":120620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_096_03.jpg"},{"id":350553,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/fs-096-03/pdf/fs-096-03.pdf","text":"Report","size":"1.2 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":4805,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/fs-096-03/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6290f6","contributors":{"authors":[{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":247854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cunningham, William L. wcunning@usgs.gov","contributorId":1198,"corporation":false,"usgs":true,"family":"Cunningham","given":"William","email":"wcunning@usgs.gov","middleInitial":"L.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":247855,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53162,"text":"fs09003 - 2003 - Native plants for effective coastal wetland restoration","interactions":[],"lastModifiedDate":"2024-10-09T14:33:46.413791","indexId":"fs09003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"090-03","title":"Native plants for effective coastal wetland restoration","docAbstract":"

Plant communities, along with soils and appropriate water regimes, are essential components of healthy wetland systems. In Louisiana, the loss of wetland habitat continues to be an issue of major concern. Wetland loss is caused by several interacting factors, both natural and human-induced (e.g., erosion and saltwater intrusion from the construction of canals and levees). Recent estimates of annual coastal land loss rates of about 62 km2 (24 mi2 ) over the past decade emphasize the magnitude of this problem. In an attempt to slow the rate of loss and perhaps halt the overall trend, resource managers in Louisiana apply various techniques to restore damaged or degraded habitats to functioning wetland systems.

Researchers at the U.S. Geological Survey’s National Wetlands Research Center (NWRC) have cooperated with the Louisiana Department of Natural Resources in studies that address effective restoration strategies for coastal wetlands. The studies have identified differences in growth that naturally exist in native Louisiana wetland plant species and genetic varieties (i.e., clones) within species. Clones of a species have a distinctive genetic identity, and some clones may also have distinctive growth responses under various environmental conditions (i.e., preferences). Indeed, large areas of coastal marsh are typically populated by several clones of a plant species, each growing in a microenvironment suited to its preferences.

These studies will provide information that will assist resource managers in selecting plant species and clones of species with known growth characteristics that can be matched to environmental conditions at potential restoration sites.

Before the studies began, a collection of several clones from four plant species native to coastal Louisiana was established. The species collected included saltgrass (Distichlis spicata), common reed (Phragmites australis), giant bulrush (Schoenoplectus californicus), and saltmarsh bulrush (Schoenoplectus robustus). Plants connected by roots were collected from public lands across the coastal zone, and then allowed to grow several months and produce new stems and plants from underground stems called “rhizomes.” These procedures maintained the genetic identity of the clones and allowed the plants to adjust to greenhouse conditions before experimental treatments began.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs09003","usgsCitation":"Howard, R.J., 2003, Native plants for effective coastal wetland restoration: U.S. Geological Survey Fact Sheet 090-03, 2 p., https://doi.org/10.3133/fs09003.","productDescription":"2 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":125713,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2003/090/coverthb.jpg"},{"id":4743,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2003/090/fs09003.pdf","text":"Report","size":"467 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 090-03"}],"contact":"

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606361","contributors":{"authors":[{"text":"Howard, Rebecca J. 0000-0001-7264-4364 howardr@usgs.gov","orcid":"https://orcid.org/0000-0001-7264-4364","contributorId":2429,"corporation":false,"usgs":true,"family":"Howard","given":"Rebecca","email":"howardr@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":246804,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53271,"text":"ofr03283 - 2003 - Hurricane Mitch: mapping coastal habitats","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"ofr03283","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":"2003-283","title":"Hurricane Mitch: mapping coastal habitats","language":"ENGLISH","doi":"10.3133/ofr03283","usgsCitation":"Handley, L.R., Thibodeaux, J.L., Dugas, J.L., Mouton, K., and Haviland, B., 2003, Hurricane Mitch: mapping coastal habitats: U.S. Geological Survey Open-File Report 2003-283, 86 p., https://doi.org/10.3133/ofr03283.","productDescription":"86 p.","costCenters":[],"links":[{"id":177922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4977,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.nwrc.usgs.gov/hurricane/mitch/Mitch_Report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a3a8","contributors":{"authors":[{"text":"Handley, Lawrence R. handleyl@usgs.gov","contributorId":3459,"corporation":false,"usgs":true,"family":"Handley","given":"Lawrence","email":"handleyl@usgs.gov","middleInitial":"R.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":247135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thibodeaux, Jesse L. II","contributorId":79548,"corporation":false,"usgs":true,"family":"Thibodeaux","given":"Jesse","suffix":"II","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":247136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dugas, Jason L. 0000-0001-6094-7560","orcid":"https://orcid.org/0000-0001-6094-7560","contributorId":86419,"corporation":false,"usgs":true,"family":"Dugas","given":"Jason","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":247137,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mouton, Kelly 0000-0002-7692-8206 moutonk@usgs.gov","orcid":"https://orcid.org/0000-0002-7692-8206","contributorId":2998,"corporation":false,"usgs":true,"family":"Mouton","given":"Kelly","email":"moutonk@usgs.gov","affiliations":[],"preferred":true,"id":247134,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haviland, Bryan","contributorId":97980,"corporation":false,"usgs":true,"family":"Haviland","given":"Bryan","email":"","affiliations":[],"preferred":false,"id":247138,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":57224,"text":"wdrOK021 - 2003 - Water resources data, Oklahoma, water year 2002; Volume 1. Arkansas River basin","interactions":[],"lastModifiedDate":"2020-09-15T20:29:21.057528","indexId":"wdrOK021","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":"OK-02-1","title":"Water resources data, Oklahoma, water year 2002; Volume 1. Arkansas River basin","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOK021","usgsCitation":"Blazs, R., Walters, D., Coffey, T., Boyle, D., and Wellman, J., 2003, Water resources data, Oklahoma, water year 2002; Volume 1. 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D.L.","contributorId":55505,"corporation":false,"usgs":true,"family":"Boyle","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":256384,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wellman, J.J.","contributorId":81972,"corporation":false,"usgs":true,"family":"Wellman","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":256385,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53944,"text":"itr030006 - 2003 - A Framework for Long-term Ecological Monitoring in Olympic National Park: Prototype for the Coniferous Forest Biome","interactions":[],"lastModifiedDate":"2017-11-22T16:07:31","indexId":"itr030006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":37,"text":"Information and Technology Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"2003-0006","title":"A Framework for Long-term Ecological Monitoring in Olympic National Park: Prototype for the Coniferous Forest Biome","docAbstract":"

This report is the result of a five-year collaboration between scientists of the U.S. Geological Survey Forest and Rangeland Ecosystem Science Center, Olympic Field Station, and the natural resources staff of Olympic National Park to develop a comprehensive strategy for monitoring natural resources of Olympic National Park. Olympic National Park is the National Park Serviceʼs prototype monitoring park, representing parks in the coniferous forest biome. Under the umbrella of the National Park Serviceʼs prototype parks program, U.S. Geological Survey and Olympic National Park staffs are obligated to:

Olympic National Park is part of the North Coast and Cascades Network, a network of seven Pacific Northwestern park units created recently by the National Park Serviceʼs Inventory and Monitoring Program to extend the monitoring of ʻvital signsʼ of park health to all National Park Service units. It is our intent and hope that the monitoring strategies and conceptual models described here will meet the overall purpose of the prototype parks monitoring program in proving useful not only to Olympic National Park, but also to parks within the North Coast and Cascades Network and elsewhere.

Part I contains the conceptual design and sampling framework for the prototype long-term monitoring program in Olympic National Park. In this section, we explore key elements of monitoring design that help to ensure the spatial, ecological, and temporal integration of monitoring program elements and discuss approaches used to design an ecosystem-based monitoring program. Basic monitoring components include ecosystem drivers, (e.g., climate, atmospheric inputs, human pressures), indicators of ecosystem integrity (e.g., biogeochemical indicators), known threats (e.g., impacts of introduced mountain goats), and focal or ʻkeyʼ species (e.g., rare or listed species, Roosevelt elk). Monitoring system drivers and key indicators of ecosystem integrity provide the long-term baseline needed to judge what constitutes ʻunnaturalʼ variation in park resources and provide the earliest possible warning of unacceptable change. Monitoring effects of known threats and the status of focal species will provide information useful to park managers for dealing with current park issues.

In Part I we describe the process of identifying potential indicators of ecological condition and present conceptual models of park ecosystems. In addition we report results from several workshops held in conjunction with Olympic National Park aimed at identifying potential indicators of change in the parkʼs ecosystem. First, we describe the responses of Olympic National Park staff to the generic question, “What is the most important resource to monitor in Olympic National Park and why?” followed by the responses from resource and land managers from areas adjoining the park. We also catalogue the responses of various expert groups that we asked to help identify the most appropriate system drivers and indicators of change in the Olympic National Park ecosystems. Results of the workshops provided the justification for selecting basic indicators of ecosystem integrity, effects of current threats to park resources, and focal resources of parks to detect both the currently evident and unforeseeable changes in park resources.

We conclude Part I by exploring several generic statistical issues relevant to monitoring natural resources in Olympic National Park. Specifically we discuss trade-offs associated with sampling extensively versus sampling intensively in smaller geographic regions and describe a conceptual framework to guide development of a generic sampling frame for monitoring. We recommend partitioning Olympic National Park into three zones of decreasing accessibility to maximize monitoring efficiency. We present examples of how the generic sampling frame could be used to help ensure spatial integration of individual monitoring projects.

Part II of the report is a record of the potential monitoring questions and indicators identified to date in our workshops. The presentation is organized according to the major system drivers, components, and processes identified in the intermediate-level working model of the Olympic National Park ecosystem. For each component of the park system, we develop the need and justification for monitoring, articulate park management issues, and describe key resources and ecosystem functions. We also present a pictorial conceptual model of each ecological subsystem, identify monitoring questions, and list potential indicators for each monitoring question. We conclude each section by identifying linkages of indicators to other ecological subsystems in our general ecosystem model, spatial and temporal contexts for monitoring (where and how often to monitor), and research and development needs. Part II represents the most current detailed listing of potential indicators—the material for subsequent discussions of monitoring priorities and selection of indicators for protocol development.

Collectively, the sections of this report contain a comprehensive list of the important monitoring questions and potential indicators as well as recommendations for designing an integrated monitoring program. In Part I, Chapter 6 we provide recommendations on how to proceed with the important next steps in the design process: establishing priorities among the many possible monitoring questions and indicators, and beginning to research and design effective long-term monitoring protocols.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared in Cooperation with Olympic National Park","usgsCitation":"Jenkins, K., Woodward, A., and Schreiner, E., 2003, A Framework for Long-term Ecological Monitoring in Olympic National Park: Prototype for the Coniferous Forest Biome: Information and Technology Report 2003-0006, x, 150 p.","productDescription":"x, 150 p.","numberOfPages":"162","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":174607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/itr/2003/0006/coverthb.jpg"},{"id":4858,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/itr/2003/0006/itr030006.pdf","text":"Report","size":"5.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"ITR "}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4955e4b0b290850ef105","contributors":{"authors":[{"text":"Jenkins, Kurt","contributorId":30681,"corporation":false,"usgs":true,"family":"Jenkins","given":"Kurt","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":248748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodward, Andrea 0000-0003-0604-9115 awoodward@usgs.gov","orcid":"https://orcid.org/0000-0003-0604-9115","contributorId":3028,"corporation":false,"usgs":true,"family":"Woodward","given":"Andrea","email":"awoodward@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":248747,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schreiner, Ed","contributorId":97555,"corporation":false,"usgs":true,"family":"Schreiner","given":"Ed","email":"","affiliations":[],"preferred":false,"id":248749,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":57225,"text":"wdrOK022 - 2003 - Water resources data, Oklahoma, water year 2002; Volume 2. Red River basin","interactions":[],"lastModifiedDate":"2020-09-25T16:31:06.8045","indexId":"wdrOK022","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":"OK-02-2","title":"Water resources data, Oklahoma, water year 2002; Volume 2. Red River basin","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOK022","usgsCitation":"Blazs, R., Walters, D., Coffey, T., Boyle, D., and Wellman, J., 2003, Water resources data, Oklahoma, water year 2002; Volume 2. 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D.L.","contributorId":55505,"corporation":false,"usgs":true,"family":"Boyle","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":256389,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wellman, J.J.","contributorId":81972,"corporation":false,"usgs":true,"family":"Wellman","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":256390,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":47851,"text":"fs04403 - 2003 - Geohydrology of Recharge and Seawater Intrusion in the Pajaro Valley, Santa Cruz and Monterey Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:44","indexId":"fs04403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"044-03","title":"Geohydrology of Recharge and Seawater Intrusion in the Pajaro Valley, Santa Cruz and Monterey Counties, California","docAbstract":"The U.S. Geological Survey (USGS) in cooperation with the Pajaro Valley Water Management Agency (PVWMA), has completed the collection and analyses of geologic, hydrologic, geophysical,\r\nand geochemical data in the coastal aquifer systems of the Pajaro Valley (fig. 1). These data were collected to delineate the geohydrologic framework of seawater intrusion, as well as, the source, age, and movement of ground water in the coastal aquifer systems (Hanson, 2003).","language":"ENGLISH","doi":"10.3133/fs04403","usgsCitation":"Hanson, R.T., 2003, Geohydrology of Recharge and Seawater Intrusion in the Pajaro Valley, Santa Cruz and Monterey Counties, California: U.S. Geological Survey Fact Sheet 044-03, 4 p., https://doi.org/10.3133/fs04403.","productDescription":"4 p.","costCenters":[],"links":[{"id":122294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_044_03.jpg"},{"id":4054,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-044-03/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8aae","contributors":{"authors":[{"text":"Hanson, Randall T. 0000-0002-9819-7141 rthanson@usgs.gov","orcid":"https://orcid.org/0000-0002-9819-7141","contributorId":801,"corporation":false,"usgs":true,"family":"Hanson","given":"Randall","email":"rthanson@usgs.gov","middleInitial":"T.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":236387,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53954,"text":"ofr0326 - 2003 - Tree islands of the Florida Everglades - A disappearing resource","interactions":[],"lastModifiedDate":"2025-04-18T15:31:13.141547","indexId":"ofr0326","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":"2003-26","title":"Tree islands of the Florida Everglades - A disappearing resource","docAbstract":"Until recently, the timing and cause of tree island formation have been poorly understood, with estimates of initial tree-island development as early as thousands of years ago to as recently as the last few decades. To increase our knowledge about the origins of these features, sediment cores were collected on and around tree islands. These cores were dated using radioisotopic techniques, including carbon-14 dating, which provides reliable dates from ~40,000 to ~300 years ago, and lead-210 dating, which provides age models for the last century. These age models were paired with vegetational reconstruction based on pollen analysis from cores to identify the timing of tree-island formation and assess past tree-island response to hydrologic changes in the 20th century.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0326","usgsCitation":"Tree Islands of the Florida Everglades - A Disappearing Resource; 2003; OFR; 2003-26; Geological Survey (U.S.)","productDescription":"2 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":173857,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2003/0026/coverthb.jpg"},{"id":4867,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0026/ofr03-26.pdf","text":"Report","size":"14.4 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2003-0026"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.21989956095884,\n 26.52881121594524\n ],\n [\n -81.18597868368488,\n 26.52881121594524\n ],\n [\n -81.18597868368488,\n 25.150575418214927\n ],\n [\n -80.21989956095884,\n 25.150575418214927\n ],\n [\n -80.21989956095884,\n 26.52881121594524\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","publishedDate":"2003-01-03","noUsgsAuthors":false,"publicationDate":"2003-01-03","publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e94c8","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47749,"text":"wri024247 - 2003 - Ground-water-quality assessment of shallow aquifers in the Front Range Urban Corridor, Colorado, 1954-98","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"wri024247","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":"2002-4247","title":"Ground-water-quality assessment of shallow aquifers in the Front Range Urban Corridor, Colorado, 1954-98","docAbstract":"Historical (1954-98) water-quality data for major ions, trace elements, major plant nutrients, and organic constituents collected in 3,870 sampling events at 2,138 shallow wells represent ground-water quality in shallow aquifers that underlie the Front Range Urban Corridor in Colorado. Nonparametric summary statistics and maps of concentrations across the study area indicate that ground water in the study area included fresh to saline water. Sulfate concentrations were elevated in the north and northeast parts of the study area, possibly due to Pierre Shale and Laramie Formation shale outcrops in those areas. Apart from isolated areas of known contamination, chloride concentrations were generally less than 100 milligrams per liter across the study area. Wells with elevated nitrate concentrations usually were located near rivers and streams downgradient from metropolitan areas. Elevated nitrate concentrations in wells that were not along the South Platte River were possibly from individual sewage disposal system usage or from fertilizer application to land. Spatial distribution for organic compounds for which more than 40 percent of the data were above the detection limit (atrazine, methyl-tert-butylether, and prometon) is not widespread across the study area, but this may reflect limitations of data availability. \r\n\r\nSummary statistics calculated or estimated by decade are influenced by the temporal variability of data across the study area. The median values of specific conductance, chloride, and nitrate from the 1970?s are less than values from the 1980?s and 1990?s, which, because most samples from the l970?s were collected in the western part of the study area, indicates that water quality in the western part of the study area is generally different than the rest of the study area. Chloride may be introduced to ground water from runoff of road deicers or chlorinated organics in transportation/transitional areas, where the median concentration is the greatest (85.0 milligrams per liter). Nitrate median concentrations are several times greater where the land is cultivated or used for agricultural business, which may reflect use of nitrogen fertilizers and the presence of animal feeding operations. \r\n\r\nMost inorganic and organic constituents exceeded drinking-water standards in only a small percentage of samples. Exceptions to this include sulfate; nitrate; trace elements aluminum, cadmium, iron, and manganese; and organic compounds 1,1-dichloroethylene, tetrachloroethylene, trichloroethylene, benzene, and dichloromethane.","language":"ENGLISH","doi":"10.3133/wri024247","usgsCitation":"Flynn, J.L., 2003, Ground-water-quality assessment of shallow aquifers in the Front Range Urban Corridor, Colorado, 1954-98: U.S. Geological Survey Water-Resources Investigations Report 2002-4247, 32 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/wri024247.","productDescription":"32 p. :col. ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":4078,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024247/","linkFileType":{"id":5,"text":"html"}},{"id":169770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a17e","contributors":{"authors":[{"text":"Flynn, Jennifer L.","contributorId":66298,"corporation":false,"usgs":true,"family":"Flynn","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":236151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44894,"text":"wri024196 - 2003 - Investigation of water quality in the Great Sand Dunes National Monument and Preserve, Saguache County, Colorado, February 1999 through September 2000: Qualifying for outstanding waters designation","interactions":[],"lastModifiedDate":"2012-02-02T00:10:13","indexId":"wri024196","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":"2002-4196","title":"Investigation of water quality in the Great Sand Dunes National Monument and Preserve, Saguache County, Colorado, February 1999 through September 2000: Qualifying for outstanding waters designation","docAbstract":"Great Sand Dunes National Monument and Preserve is located on the eastern side of the San Luis Valley in south-central Colorado. The monument covers 60.4 square miles in Saguache and Alamosa Counties and lies at the base of the Sangre de Cristo Mountains, where a unique combination of climate, topography, and hydrology has created and maintained the Nation?s tallest inland sand dunes. The Sangre de Cristo Mountains, which rise to more than 14,000 feet to the north and east of the dunes, are the source of several streams that flow around the dunes and eventually recharge the aquifer beneath the valley. Sand Creek and Medano Creeks are the largest of the streams in the monument that originate in the Sangre de Cristo Mountains; several ephemeral streams flow into Sand Creek and Medano Creek. Maintaining the high surface-water quality in the Great Sand Dunes National Monument and Preserve is identified as a critical issue by the National Park Service. Additionally, the National Park Service has indicated a desire to pursue an Outstanding Waters Designation, which offers the highest level of water-quality protection available under the Clean Water Act and Colorado regulations. This designation is designed to prevent any degradation from existing conditions (Chatman and others, 1997). Assessment is needed to evaluate whether the water quality of the streams in the monument meets the requirements for an Outstanding Waters Designation. Historically, prospecting and mining activities have occurred in the watersheds of Sand and Medano Creeks; currently, however, there is no mining activity in those watersheds. In addition, the camping and recreation that occur upstream from the monument on national preserve lands and water activities that occur in Medano Creek during the summer are a potential source of human-waste contamination. Figure 1. Location of study area, sampling sites, and indication of sites that meet or exceed instream standards. The U.S. Geological Survey (USGS), in cooperation with the National Park Service, investigated the water quality at 15 sites (fig. 1) from February 1999 through September 2000 to identify baseline water-quality conditions and to determine if the water met standards to qualify for the Outstanding Waters Designation. This report describes current water-quality conditions in streams in the monument and compares the water-quality data to Colorado instream standards to assist the State of Colorado Water Quality Control Commission in the determination of qualification for Outstanding Waters Designation.","language":"ENGLISH","doi":"10.3133/wri024196","usgsCitation":"Ferguson, S.A., 2003, Investigation of water quality in the Great Sand Dunes National Monument and Preserve, Saguache County, Colorado, February 1999 through September 2000: Qualifying for outstanding waters designation: U.S. Geological Survey Water-Resources Investigations Report 2002-4196, 8 p. : ill., map ; 28 cm., https://doi.org/10.3133/wri024196.","productDescription":"8 p. : ill., map ; 28 cm.","costCenters":[],"links":[{"id":169966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3787,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024196","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4783e4b07f02db483888","contributors":{"authors":[{"text":"Ferguson, Sheryl A.","contributorId":78698,"corporation":false,"usgs":true,"family":"Ferguson","given":"Sheryl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":230631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51953,"text":"ofr0368 - 2003 - Hydrostratigraphy of tree island cores from Water Conservation Area 3","interactions":[],"lastModifiedDate":"2025-04-18T15:28:41.121028","indexId":"ofr0368","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":"2003-68","title":"Hydrostratigraphy of tree island cores from Water Conservation Area 3","docAbstract":"Cores and borehole-geophysical logs collected on and around two tree islands in Water Conservation Area 3 have been examined to develop a stratigraphic framework for these ecosystems. Especially important is the potential for the exchange of ground water and surface water within these features. The hydrostratigraphic results from this study document the lithologic nature of the foundation of the tree islands, the distribution of porous intervals, the potential for paleotopographic influence on their formation, and the importance of low-permeability, subaerial-exposure horizons on the vertical exchange of ground water and surface water. \r\n\r\n\r\n \r\nFigure 1. Location of Tree Islands 3AS3 and 3BS1. [larger image] \r\nResults from this hydrostratigraphic study indicate that subtle differences occur in lithofacies and topography between the on-island and off-island subsurface geologic records. Specifics are described herein. Firstly, at both tree-island sites, the top of the limestone bedrock is slightly elevated beneath the head of the tree islands relative to the off-island core sites and the tail of the tree islands, which suggests that bedrock 'highs' acted as 'seeds' for the development of the tree islands of this study and possibly many others. Secondly, examination of the recovered core and the caliper logs tentatively suggest that the elevated limestone beneath the tree islands may have a preferentially more porous framework relative to limestone beneath the adjacent areas, possibly providing a ground-water-to-surface-water connection that sustains the tree island system. Finally, because the elevation of the top of the limestone bedrock at the head of Tree Island 3AS3 is slightly higher than the surrounding upper surface of the peat, and because the wetland peats have a lower hydraulic conductivity than the limestone bedrock (Miami Limestone and Fort Thompson Formation), it is possible that there is a head difference between surface water of the wetlands and the ground water in underlying limestone bedrock.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0368","usgsCitation":"Hydrostratigraphy of Tree Island Cores from Water Conservation Area 3; 2003; OFR; 2003-68; McNeill, Donald F.; Cunningham, Kevin J.","productDescription":"130 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":179088,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2003/0068/coverthb.jpg"},{"id":4502,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0068/ofr03-68.pdf","text":"Report","size":"8.29 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 03-68"}],"country":"United States","state":"Florida","otherGeospatial":"Water Conservation Area 3","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.87148626491134,\n 25.85968346269803\n ],\n [\n -80.87148626491133,\n 25.70\n ],\n [\n -80.48039655724416,\n 25.70\n ],\n [\n -80.48382716871531,\n 25.86277066079785\n ],\n [\n -80.87148626491134,\n 25.85968346269803\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","publishedDate":"2003-10-01","noUsgsAuthors":false,"publicationDate":"2003-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc6d0","contributors":{"authors":[{"text":"McNeill, Donald F.","contributorId":56511,"corporation":false,"usgs":true,"family":"McNeill","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":244526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, Kevin J. 0000-0002-2179-8686 kcunning@usgs.gov","orcid":"https://orcid.org/0000-0002-2179-8686","contributorId":1689,"corporation":false,"usgs":true,"family":"Cunningham","given":"Kevin","email":"kcunning@usgs.gov","middleInitial":"J.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":244525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":56825,"text":"wri034198 - 2003 - Sedimentation History of Lago Guayabal, Puerto Rico, 1913-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:49","indexId":"wri034198","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":"2003-4198","title":"Sedimentation History of Lago Guayabal, Puerto Rico, 1913-2001","docAbstract":"The Lago Guayabal dam, located in the municipality of Villalba in southern Puerto Rico, was constructed in 1913 for irrigation of croplands in the southern coastal plains and is owned and operated by the Puerto Rico Electric Power Authority. The reservoir had an original storage capacity of 11.82 million cubic meters and a drainage area upstream of the dam of 112 square kilometers. Sedimentation has reduced the storage capacity to 6.12 million cubic meters in 2001, which represents a storage loss of about 48 percent. However, the actual sediment accumulation in the reservoir during the 88 years is greater, because some sediment removal was conducted between 1940 and 1948 by dredging and sluicing. This report summarizes the historical data from a 1913 land survey and eight bathymetric surveys conducted between 1914 and 2001, and the relation of high sedimentation to agricultural land practices within the Lago Guayabal basin and six major hurricanes which made landfall on the island. \r\n\r\nThe reservoir had an area-normalized sedimentation rate of about 1,863 cubic meters per square kilometer per year between 1913 and 1936 from a 112 square kilometer basin. In 1972, a new dam upstream along the Rio Toa Vaca impounded runoff from 57.5 square kilometers, and sediment transport to Lago Guayabal was reduced. A comparison of bathymetric survey results between 1972 and 2001 indicates an area-normalized sedimentation rate of 1,120 cubic meters per square kilometer per year or about 60 percent of the rate between 1913 and 1936. The significant reduction (almost half) of the sedimentation rate after the Toa Vaca dam was built may indicate that erosion susceptibility of the Rio Toa Vaca watershed is about twice that of the Rio Jacaguas watershed impounded by Lago Guayabal.","language":"ENGLISH","doi":"10.3133/wri034198","usgsCitation":"Soler-Lopez, L.R., 2003, Sedimentation History of Lago Guayabal, Puerto Rico, 1913-2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4198, 28 p., 2 pls., https://doi.org/10.3133/wri034198.","productDescription":"28 p., 2 pls.","costCenters":[],"links":[{"id":175114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5671,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034198/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbd44","contributors":{"authors":[{"text":"Soler-Lopez, Luis R.","contributorId":27501,"corporation":false,"usgs":true,"family":"Soler-Lopez","given":"Luis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":255812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56837,"text":"wri20034303 - 2003 - Effects of Aquifer Development and Changes in Irrigation Practices on Ground-Water Availability in the Santa Isabel Area, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:12:02","indexId":"wri20034303","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":"2003-4303","title":"Effects of Aquifer Development and Changes in Irrigation Practices on Ground-Water Availability in the Santa Isabel Area, Puerto Rico","docAbstract":"The alluvial aquifer in the area of Santa Isabel is located within the South Coastal Plain aquifer of Puerto Rico. Variations in precipitation, changes in irrigation practices, and increasing public-supply water demand have been the primary factors controlling water-level fluctuations within the aquifer. Until the late 1970s, much of the land in the study area was irrigated using inefficient furrow flooding methods that required large volumes of both surface and ground water. A gradual shift in irrigation practices from furrow systems to more efficient micro-drip irrigation systems occurred between the late 1970s and the late 1980s. Irrigation return flow from the furrow-irrigation systems was a major component of recharge to the aquifer. By the early 1990s, furrow-type systems had been replaced by the micro-drip irrigation systems. Water levels declined about 20 feet in the aquifer from 1985 until present (February 2003). \r\n\r\nThe main effect of the changes in agricultural practices is the reduction in recharge to the aquifer and total irrigation withdrawals. Increases in ground-water withdrawals for public supply offset the reduction in ground-water withdrawals for irrigation such that the total estimated pumping rate in 2003 was only 8 percent less than in 1987. Micro-drip irrigation resulted in the loss of irrigation return flow to the aquifer. These changes resulted in lowering the water table below sea level over most of the Santa Isabel area. By 2002, lowering of the water table reversed the natural discharge along the coast and resulted in the inland movement of seawater, which may result in increased salinity of the aquifer, as had occurred in other parts of the South Coastal Plain. \r\n\r\nManagement alternatives for the South Coastal Plain aquifer in the vicinity of Santa Isabel include limiting groundwater\r\nwithdrawals or implementing artificial recharge measures. Another alternative for the prevention of saltwater intrusion is to inject freshwater or treated sewage effluent into wells along the coast. A digital ground-water flow model was developed to provide information for water managers to evaluate some of these alternatives. After calibration of the ground-water model to historical data, four simulations of ground-water management strategies were performed: ground-water conservation, surface infiltration over existing agricultural fields, or infiltration along streams and canals, or injection wells along the coast. \r\n\r\nSimulations of four alternative water management strategies indicate that current condition of water levels below sea level near the coast can be reversed to raise water levels above sea level by either: (1) about a 27 percent reduction in 2003 ground-water withdrawal rates; (2) application of about 1,700 million gallons per year of artificial recharge over more than half of the current agricultural areas; (3) injection of about 3 million gallons per day (1,095 million gallons per year) of freshwater or treated wastewater in wells distributed along the coast; (4) injection of about 3.5 million gallons per day (1,280 million gallons per year) of freshwater or treated wastewater in wells distributed along canals and streams.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri20034303","usgsCitation":"Kuniansky, E.L., Gómez-Gómez, F., and Torres-Gonzalez, S., 2003, Effects of Aquifer Development and Changes in Irrigation Practices on Ground-Water Availability in the Santa Isabel Area, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 2003-4303, 65 p., https://doi.org/10.3133/wri20034303.","productDescription":"65 p.","costCenters":[],"links":[{"id":5685,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034303/","linkFileType":{"id":5,"text":"html"}},{"id":180923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db62521f","contributors":{"authors":[{"text":"Kuniansky, Eve L. 0000-0002-5581-0225 elkunian@usgs.gov","orcid":"https://orcid.org/0000-0002-5581-0225","contributorId":932,"corporation":false,"usgs":true,"family":"Kuniansky","given":"Eve","email":"elkunian@usgs.gov","middleInitial":"L.","affiliations":[{"id":5064,"text":"Southeast Regional Director's Office","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"preferred":true,"id":255840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gómez-Gómez, Fernando","contributorId":31366,"corporation":false,"usgs":true,"family":"Gómez-Gómez","given":"Fernando","affiliations":[],"preferred":false,"id":255842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Torres-Gonzalez, Sigfredo sttorres@usgs.gov","contributorId":3997,"corporation":false,"usgs":true,"family":"Torres-Gonzalez","given":"Sigfredo","email":"sttorres@usgs.gov","affiliations":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"preferred":true,"id":255841,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53134,"text":"wri034111 - 2003 - Occurrence and Transport of Diazinon in the Sacramento River and Selected Tributaries, California, during Two Winter Storms, January?February 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wri034111","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":"2003-4111","title":"Occurrence and Transport of Diazinon in the Sacramento River and Selected Tributaries, California, during Two Winter Storms, January?February 2001","docAbstract":"Diazinon, an organophosphate insecticide, is applied as an orchard dormant spray in the Sacramento Valley during the winter months when the area receives most of its annual rainfall. During winter rainstorms that frequently follow dormant spray applications, some of the applied pesticide is transported in storm runoff to the Sacramento River and its tributaries. Diazinon is also used to control insect pests on residential and commercial properties in urban areas and is frequently detected in urban storm runoff draining into the Sacramento River system.\r\n\r\n Between January 24 and February 14, 2001, diazinon concentrations and loads were measured in the Sacramento River and selected tributaries during two winter storms that occurred after dormant spray applications were made to orchards in the Sacramento Valley. Water samples were collected at 21 sites that represented agricultural and urban inputs on a variety of scales, from small tributaries and drains representing local land use to main-stem river sites representing regional effects.\r\n\r\n Concentrations of diazinon ranged from below laboratory reporting levels to 1,380 nanograms per liter (ng/L), with a median of 55 ng/L during the first monitored storm and 26 ng/L during the second. The highest concentrations were observed in small channels draining predominantly agricultural land.\r\n\r\nAbout 26,000 pounds of diazinon were reported applied to agricultural land in the study area just before and during the monitoring period. About 0.2 percent of the applied insecticide appeared to be transported to the lower Sacramento River during that period. The source of about one third of the total load measured in the lower Sacramento River appears to be in the portion of the drainage basin upstream of the city of Colusa. About 12 percent of the diazinon load in the lower Sacramento River was transported from the Feather River Basin, which drains much of the mountainous eastern portions of the Sacramento River Basin. \r\n\r\n Diazinon use in the study area during the 2000?2001 dormant spray season continued a declining trend observed since 1993. The maximum concentrations of diazinon observed during the last 2 years of monitoring were lower than concentrations observed in previous years when larger amounts of diazinon had been applied as dormant sprays.","language":"ENGLISH","doi":"10.3133/wri034111","usgsCitation":"Dileanis, P.D., Brown, D.L., Knifong, D.L., and Saleh, D., 2003, Occurrence and Transport of Diazinon in the Sacramento River and Selected Tributaries, California, during Two Winter Storms, January?February 2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4111, 85 p., https://doi.org/10.3133/wri034111.","productDescription":"85 p.","costCenters":[],"links":[{"id":4713,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034111/","linkFileType":{"id":5,"text":"html"}},{"id":177230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a569d","contributors":{"authors":[{"text":"Dileanis, Peter D. dileanis@usgs.gov","contributorId":71541,"corporation":false,"usgs":true,"family":"Dileanis","given":"Peter","email":"dileanis@usgs.gov","middleInitial":"D.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":246728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, David L.","contributorId":55425,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":246727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knifong, Donna L. dknifong@usgs.gov","contributorId":1517,"corporation":false,"usgs":true,"family":"Knifong","given":"Donna","email":"dknifong@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":246726,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saleh, Dina 0000-0002-1406-9303 dsaleh@usgs.gov","orcid":"https://orcid.org/0000-0002-1406-9303","contributorId":939,"corporation":false,"usgs":true,"family":"Saleh","given":"Dina","email":"dsaleh@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":246725,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":54180,"text":"wdrNC021B - 2003 - Water resources data, North Carolina, water year 2002. Volume 1B: Surface-water records","interactions":[],"lastModifiedDate":"2017-01-18T14:35:48","indexId":"wdrNC021B","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":"NC-02-1B","title":"Water resources data, North Carolina, water year 2002. Volume 1B: Surface-water records","docAbstract":"Water-resources data for the 2002 water year for North Carolina consist of records of stage, discharge, water quality for streams; stage and contents for lakes and reservoirs; precipitation; and ground-water levels and water quality of ground water. Volume 1 contains discharge records for 211 gaging stations; stage and contents for 62 lakes and reservoirs; stage for 20 gaging stations; water quality for 52 gaging stations and 7 miscellaneous sites, and continuous water quality for 30 sites; and continuous precipitation at 109 sites. Volume 2 contains ground-water-level data from 143 observation wells and ground-water-quality data from 72 wells. Additional water data were collected at 85 sites not involved in the systematic data-collection program, and are published as miscellaneous measurements in Volume 1. The collection of water-resources data in North Carolina is a part of the National Water-Data System operated by the U.S. Geological Survey in cooperation with State, municipal, and Federal agencies.","language":"ENGLISH","doi":"10.3133/wdrNC021B","usgsCitation":"Ragland, B., Barker, R., and Robinson, J.B., 2003, Water resources data, North Carolina, water year 2002. Volume 1B: Surface-water records: U.S. Geological Survey Water Data Report NC-02-1B, 663 p., https://doi.org/10.3133/wdrNC021B.","productDescription":"663 p.","temporalStart":"2001-10-01","temporalEnd":"2002-09-30","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":181577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5622,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/wdr-nc-02/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North 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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0d7f","contributors":{"authors":[{"text":"Ragland, B.C.","contributorId":27127,"corporation":false,"usgs":true,"family":"Ragland","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":249441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barker, R.G.","contributorId":93121,"corporation":false,"usgs":true,"family":"Barker","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":249443,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, J. B.","contributorId":32564,"corporation":false,"usgs":true,"family":"Robinson","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":249442,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54272,"text":"wdrNJ022 - 2003 - Water Resources Data, New Jersey, Water Year 2002--Volume 2. Ground-Water Data","interactions":[],"lastModifiedDate":"2012-02-02T00:11:36","indexId":"wdrNJ022","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":"NJ-02-2","title":"Water Resources Data, New Jersey, Water Year 2002--Volume 2. Ground-Water Data","docAbstract":"Water-resources data for the 2002 water year for New Jersey are presented in three volumes, and consists of records of stage, discharge, and quality of streams; stage and contents of lakes and reservoirs; and levels and quality of ground water. Volume 3 contains a summary of surface- and ground-water hydrologic conditions for the 2002 water year, a listing of current water-resources projects in New Jersey, a bibliography of water-related reports, articles, and fact sheets for New Jersey completed by the Geological Survey in recent years, water-quality records of chemical analyses from 118 continuing-record surface-water stations, 15 miscellaneous ground-water sites, and records of daily statistics of temperature and other physical measurements from 6 continuous-recording stations. Locations of water-quality stations are shown in figures 12-14. Locations of miscellaneous water-quality sites are shown in figures 40-41. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating federal, state, and local agencies in New Jersey.","language":"ENGLISH","doi":"10.3133/wdrNJ022","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2003, Water Resources Data, New Jersey, Water Year 2002--Volume 2. Ground-Water Data: U.S. Geological Survey Water Data Report NJ-02-2, 238 p., https://doi.org/10.3133/wdrNJ022.","productDescription":"238 p.","costCenters":[],"links":[{"id":5384,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrnj022/","linkFileType":{"id":5,"text":"html"}},{"id":178106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb26a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532224,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54277,"text":"wdrUT021 - 2003 - Water resources data, Utah, water year 2002","interactions":[],"lastModifiedDate":"2017-02-03T15:09:02","indexId":"wdrUT021","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":"UT-02-1","title":"Water resources data, Utah, water year 2002","docAbstract":"Water-resources data for the 2002 water year for Utah consist of records of stage, discharge, and water quality of\r\nstreams; stage and contents of lakes and reservoirs; and water levels and water quality of ground water. This report\r\ncontains discharge records for 163 gaging stations; stage and contents for 10 lakes and reservoirs; water quality for\r\n24 hydrologic stations, and 64 wells; water levels for 66 observation wells; and precipitation for 2 stations. Additional\r\nwater data were collected at various sites not involved in the systematic data-collection program and are published\r\nas miscellaneous measurements. These data represent that part of the National Water Data System collected\r\nby the U.S. Geological Survey and cooperating State and Federal agencies in Utah.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/wdrUT021","collaboration":"Prepared in cooperation with the State of Utah and other cooperators and agencies","usgsCitation":"Wilberg, D., Tibbetts, J., and Enright, M., 2003, Water resources data, Utah, water year 2002: U.S. Geological Survey Water Data Report UT-02-1, xlii, 391 p., https://doi.org/10.3133/wdrUT021.","productDescription":"xlii, 391 p.","numberOfPages":"437","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":182047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5391,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/WDRUT02","linkFileType":{"id":5,"text":"html"}},{"id":334742,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/WDRUT02/PDF/ADRUT02.pdf","size":"18 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa7c4","contributors":{"authors":[{"text":"Wilberg, Dale E.","contributorId":60215,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale E.","affiliations":[],"preferred":false,"id":249735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tibbetts, J.R.","contributorId":63470,"corporation":false,"usgs":true,"family":"Tibbetts","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":249736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Enright, Michael","contributorId":99979,"corporation":false,"usgs":true,"family":"Enright","given":"Michael","email":"","affiliations":[],"preferred":false,"id":249737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54279,"text":"wdrVA022 - 2003 - Water Resources Data, Virginia, Water Year 2002, Volume 2. Ground-Water Level and Ground-Water Quality Records","interactions":[],"lastModifiedDate":"2012-02-02T00:11:59","indexId":"wdrVA022","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":"VA-02-2","title":"Water Resources Data, Virginia, Water Year 2002, Volume 2. Ground-Water Level and Ground-Water Quality Records","docAbstract":"This report is Volume 2 in our 2002 series and includes records of water levels and water quality of ground-water wells. It contains records for water levels at 267 observation wells and water quality at 62 wells. Locations of these wells are shown on figures 4, 5, 6, and 7. The data in this report represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Virginia.","language":"ENGLISH","doi":"10.3133/wdrVA022","usgsCitation":"White, R.K., Powell, E.D., and Guyer, J.R., 2003, Water Resources Data, Virginia, Water Year 2002, Volume 2. Ground-Water Level and Ground-Water Quality Records: U.S. Geological Survey Water Data Report VA-02-2, 368 p., https://doi.org/10.3133/wdrVA022.","productDescription":"368 p.","costCenters":[],"links":[{"id":5393,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/WDRVA022","linkFileType":{"id":5,"text":"html"}},{"id":182128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f69a4","contributors":{"authors":[{"text":"White, Roger K.","contributorId":19624,"corporation":false,"usgs":true,"family":"White","given":"Roger","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":249742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, Eugene D.","contributorId":80309,"corporation":false,"usgs":true,"family":"Powell","given":"Eugene","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":249744,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guyer, Joel R.","contributorId":47446,"corporation":false,"usgs":true,"family":"Guyer","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":249743,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53681,"text":"ofr03348 - 2003 - Flow Velocity, Water Temperature, and Conductivity in Shark River Slough, Everglades National Park, Florida: August 2001-June 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"ofr03348","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":"2003-348","title":"Flow Velocity, Water Temperature, and Conductivity in Shark River Slough, Everglades National Park, Florida: August 2001-June 2002","docAbstract":"The data-collection effort described in this report is in support of the U.S. Geological Survey (USGS) Place-Based Studies project investigating 'Forcing Effects on Flow Structure in Vegetated Wetlands of the Everglades.' Data collected at four locations in Shark River Slough, Everglades National Park, during the 2001-2002 wet season are documented in the report and methods used to process the data are described. Daily mean flow velocities, water temperatures, and specific conductance values are presented in the appendices of the report. The quality-checked and edited data have been compiled and stored on the USGS South Florida Information Access (SOFIA) website http://sofia.usgs.gov.","language":"ENGLISH","doi":"10.3133/ofr03348","usgsCitation":"Riscassi, A.L., and Schaffranek, R.W., 2003, Flow Velocity, Water Temperature, and Conductivity in Shark River Slough, Everglades National Park, Florida: August 2001-June 2002: U.S. Geological Survey Open-File Report 2003-348, 45 p., https://doi.org/10.3133/ofr03348.","productDescription":"45 p.","costCenters":[],"links":[{"id":5000,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03348/","linkFileType":{"id":5,"text":"html"}},{"id":178755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df6b1","contributors":{"authors":[{"text":"Riscassi, Ami L.","contributorId":24399,"corporation":false,"usgs":true,"family":"Riscassi","given":"Ami","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":248073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaffranek, Raymond W.","contributorId":86314,"corporation":false,"usgs":true,"family":"Schaffranek","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":248074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47501,"text":"fs12902 - 2003 - Real-time ground-water-level monitoring in New Jersey, 2002","interactions":[],"lastModifiedDate":"2016-02-24T14:54:52","indexId":"fs12902","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"129-02","title":"Real-time ground-water-level monitoring in New Jersey, 2002","docAbstract":"

This network was created to provide data to indicate water-level trends in shallow ground-water systems within the State of New Jersey and to make the data available in the shortest time possible. The wells in this network are located throughout New Jersey (fig. 1) and were chosen because they are completed in shallow aquifers (table 1). The monitoring of shallow aquifers is important because these aquifers are relied on for water supply and irrigation. Additionally, the natural discharge from shallow aquifers provides base flow to streams. Water levels in these aquifers respond relatively quickly to precipitation and dry periods, so the rapid reporting of water-level data is necessary to follow trends. This network, for example, provides data that allow observation of the onset of drought conditions in ground water. Also, the data from this network can be used to estimate the most recent water-level trend in surficial-aquifer wells not outfitted with satellite telemetry.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs12902","usgsCitation":"Jones, W.D., Navoy, A.S., and Pope, D.A., 2003, Real-time ground-water-level monitoring in New Jersey, 2002: U.S. Geological Survey Fact Sheet 129-02, 4 p., https://doi.org/10.3133/fs12902.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":123120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_129_02.jpg"},{"id":3954,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New 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Cartographic services contract...for everything geographic","interactions":[{"subject":{"id":30707,"text":"fs07801 - 2001 - Cartographic Services Contract","indexId":"fs07801","publicationYear":"2001","noYear":false,"title":"Cartographic Services Contract"},"predicate":"SUPERSEDED_BY","object":{"id":53166,"text":"fs06603 - 2003 - Cartographic services contract...for everything geographic","indexId":"fs06603","publicationYear":"2003","noYear":false,"title":"Cartographic services contract...for everything geographic"},"id":1}],"lastModifiedDate":"2012-02-27T14:10:03","indexId":"fs06603","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"066-03","title":"Cartographic services contract...for everything geographic","docAbstract":"The U.S. Geological Survey's (USGS) Cartographic Services Contract (CSC) is used to award work for photogrammetric and mapping services under the umbrella of Architect-Engineer (A&E) contracting. The A&E contract is broad in scope and can accommodate any activity related to standard, nonstandard, graphic, and digital cartographic products. Services provided may include, but are not limited to, photogrammetric mapping and aerotriangulation; orthophotography; thematic mapping (for example, land characterization); analog and digital imagery applications; geographic information systems development; surveying and control acquisition, including ground-based and airborne Global Positioning System; analog and digital image manipulation, analysis, and interpretation; raster and vector map digitizing; data manipulations (for example, transformations, conversions, generalization, integration, and conflation); primary and ancillary data acquisition (for example, aerial photography, satellite imagery, multispectral, multitemporal, and hyperspectral data); image scanning and processing; metadata production, revision, and creation; and production or revision of standard USGS products defined by formal and informal specification and standards, such as those for digital line graphs, digital elevation models, digital orthophoto quadrangles, and digital raster graphics.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs06603","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2003, Cartographic services contract...for everything geographic (Supercedes FS 078-01): U.S. Geological Survey Fact Sheet 066-03, 2 p., https://doi.org/10.3133/fs06603.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":4752,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2003/0066/","linkFileType":{"id":5,"text":"html"}},{"id":174063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2003/0066/report-thumb.jpg"},{"id":87125,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2003/0066/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Supercedes FS 078-01","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efd01","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":246142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52909,"text":"pp1668AB - 2003 - Correlation, sedimentology, structural setting, chemical composition, and provenance of selected formations in Mesoproterozoic Lemhi Group, central Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"pp1668AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1668","chapter":"A-B","title":"Correlation, sedimentology, structural setting, chemical composition, and provenance of selected formations in Mesoproterozoic Lemhi Group, central Idaho","docAbstract":"A unit of the Mesoproterozoic Apple Creek Formation of the Lemhi Range previously\r\nwas correlated with part of the lower subunit of the Mesoproterozoic Yellowjacket\r\nFormation in the Salmon River Mountains. Strata currently assigned to the middle\r\nsubunit of the Yellowjacket Formation lie conformably above the Apple Creek unit in the\r\nSalmon River Mountains, and are here renamed the banded siltite unit and reassigned to\r\nthe Apple Creek Formation. Almost all of the banded siltite unit is preserved within the\r\nSalmon River Mountains, where it grades upward into clastic rocks that currently are\r\nassigned to the upper subunit of the Yellowjacket Formation and that here are reassigned\r\nto the Gunsight Formation.\r\nThe banded siltite unit of the Apple Creek Formation is composed of a turbidite\r\nsequence, as recognized by previous workers. Uppermost strata of the unit were\r\nreworked by currents, possibly storm generated, and adjusted to a high water content by\r\ndeveloping abundant soft-sediment deformation features. Basal strata of the overlying\r\nGunsight Formation in the Salmon River Mountains display abundant hummocky\r\ncrossbeds, storm-generated features deposited below fair-weather wave base, that are\r\nconformable above the storm-reworked deposits. The hummocky crossbedded strata\r\ngrade upward into marine shoreface strata deposited above fair-weather wave base, which\r\nin turn are succeeded by fluvial strata. Hummocky and shoreface strata are absent from\r\nthe Gunsight Formation in the Lemhi Range. The major thickness of the Gunsight\r\nFormation in both the Salmon River Mountains and the Lemhi Range is composed of\r\nfluvial rocks, transitional in the upper part into marine rocks of the Swauger Formation.\r\nThe fluvial strata are mainly characterized by stacked sheets of metasandstone and coarse\r\nsiltite; they are interpreted as deposits of braided rivers.\r\nThe Poison Creek thrust fault of the Lemhi Range extends northwestward through the\r\nstudy area in the east-central part of the Salmon River Mountains. The Apple Creek and\r\nGunsight Formations on the southwest side of the thrust fault were transported to the\r\nnortheast as part of the Poison Creek thrust sheet. A segment of the thrust fault within\r\nthe Gunsight Formation in the Salmon River Mountains subsequently underwent normal\r\ndisplacement. Along this segment, lower Gunsight strata on the southwest were\r\njuxtaposed against upper Gunsight and Swauger strata on the northeast.","language":"ENGLISH","doi":"10.3133/pp1668AB","isbn":"0607996803","usgsCitation":"Tysdal, R.G., Lindsey, D.A., and Taggart, J.E., 2003, Correlation, sedimentology, structural setting, chemical composition, and provenance of selected formations in Mesoproterozoic Lemhi Group, central Idaho (Version 1.0): U.S. Geological Survey Professional Paper 1668, vi., 40 p. : ill. (some col.), maps ; 28 cm., https://doi.org/10.3133/pp1668AB.","productDescription":"vi., 40 p. : ill. (some col.), maps ; 28 cm.","costCenters":[],"links":[{"id":4972,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/p1668/","linkFileType":{"id":5,"text":"html"}},{"id":124786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1668_a-b.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcbcb","contributors":{"authors":[{"text":"Tysdal, Russell G.","contributorId":1700,"corporation":false,"usgs":true,"family":"Tysdal","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":246209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindsey, David A. 0000-0002-9466-0899 dlindsey@usgs.gov","orcid":"https://orcid.org/0000-0002-9466-0899","contributorId":773,"corporation":false,"usgs":true,"family":"Lindsey","given":"David","email":"dlindsey@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taggart, Joseph E. Jr.","contributorId":66317,"corporation":false,"usgs":true,"family":"Taggart","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":246210,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53943,"text":"itr030005 - 2003 - Geographic Information System Tools for Conservation Planning: User's Manual","interactions":[],"lastModifiedDate":"2012-02-02T00:11:45","indexId":"itr030005","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":37,"text":"Information and Technology Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"2003-0005","title":"Geographic Information System Tools for Conservation Planning: User's Manual","docAbstract":"Public and private land managers desire better ways to incorporate landscape, species, and habitat relations into their conservation planning processes. We present three tools, developed for the Environmental Systems Research Institute?s ArcView 3.x platform, applicable to many types of wildlife conservation management and planning efforts. These tools provide managers and planners with the ability to rapidly assess landscape attributes and link these attributes with species-habitat information. To use the tools, the user provides a detailed land cover spatial database and develops a matrix to identify species-habitat relations for the landscape of interest. The tools are applicable to any taxa or suite of taxa for which the required data are available. The user also has the ability to interactively make polygon-specific changes to the landscape and re-examine species-habitat relations. The development of these tools has given resource managers the means to evaluate the merits of proposed landscape management scenarios and to choose the scenario that best fits the goals of the managed area.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Fox, T.J., Rohweder, J., Kenow, K., Korschgen, C.E., and DeHaan, H., 2003, Geographic Information System Tools for Conservation Planning: User's Manual: Information and Technology Report 2003-0005, 4 p. + Appendixes A-B + CD-ROM; Data and GIS tools information online.","productDescription":"4 p. + Appendixes A-B + CD-ROM; Data and GIS tools information online","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":4857,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.umesc.usgs.gov/management/dss/gis_tools_for_conservation_planning.html","linkFileType":{"id":5,"text":"html"}},{"id":174606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9ab8","contributors":{"authors":[{"text":"Fox, Timothy J. 0000-0002-6167-3001 tfox@usgs.gov","orcid":"https://orcid.org/0000-0002-6167-3001","contributorId":1701,"corporation":false,"usgs":true,"family":"Fox","given":"Timothy","email":"tfox@usgs.gov","middleInitial":"J.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":248742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rohweder, Jason J.","contributorId":25629,"corporation":false,"usgs":true,"family":"Rohweder","given":"Jason J.","affiliations":[],"preferred":false,"id":248745,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kenow, K.P.","contributorId":18302,"corporation":false,"usgs":true,"family":"Kenow","given":"K.P.","affiliations":[],"preferred":false,"id":248744,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Korschgen, C. E.","contributorId":9197,"corporation":false,"usgs":true,"family":"Korschgen","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":248743,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeHaan, H.C.","contributorId":36618,"corporation":false,"usgs":true,"family":"DeHaan","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":248746,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53259,"text":"ofr03385 - 2003 - MODFLOW-2000, the U.S. Geological Survey modular ground-water model -- Documentation of MOD-PREDICT for predictions, prediction sensitivity analysis, and evaluation of uncertainty","interactions":[],"lastModifiedDate":"2017-07-13T13:00:30","indexId":"ofr03385","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":"2003-385","title":"MODFLOW-2000, the U.S. Geological Survey modular ground-water model -- Documentation of MOD-PREDICT for predictions, prediction sensitivity analysis, and evaluation of uncertainty","docAbstract":"

This document describes the MOD-PREDICT program, which helps evaluate userdefined sets of observations, prior information, and predictions, using the ground-water model MODFLOW-2000. MOD-PREDICT takes advantage of the existing Observation and Sensitivity Processes (Hill and others, 2000) by initiating runs of MODFLOW-2000 and using the output files produced. The names and formats of the MODFLOW-2000 input files are unchanged, such that full backward compatibility is maintained. A new name file and input files are required for MOD-PREDICT.

The performance of MOD-PREDICT has been tested in a variety of applications. Future applications, however, might reveal errors that were not detected in the test simulations. Users are requested to notify the U.S. Geological Survey of any errors found in this document or the computer program using the email address available at the web address below. Updates might occasionally be made to this document, to the MOD-PREDICT program, and to MODFLOW- 2000. Users can check for updates on the Internet at URL http://water.usgs.gov/software/ground water.html/.

","language":"English","publisher":"U.S. Geological Society","publisherLocation":"Denver, CO","doi":"10.3133/ofr03385","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Tonkin, M., Hill, M.C., and Doherty, J., 2003, MODFLOW-2000, the U.S. Geological Survey modular ground-water model -- Documentation of MOD-PREDICT for predictions, prediction sensitivity analysis, and evaluation of uncertainty: U.S. Geological Survey Open-File Report 2003-385, Reporrt: viii, 69 p., https://doi.org/10.3133/ofr03385.","productDescription":"Reporrt: viii, 69 p.","startPage":"1","endPage":"69","numberOfPages":"80","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":4936,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/nrp/gwsoftware/modpredict/modpredict.html","linkFileType":{"id":5,"text":"html"}},{"id":174302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2003/0385/report-thumb.jpg"},{"id":87134,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0385/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648cde","contributors":{"authors":[{"text":"Tonkin, M.J.","contributorId":34989,"corporation":false,"usgs":true,"family":"Tonkin","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":247085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, Mary C. mchill@usgs.gov","contributorId":974,"corporation":false,"usgs":true,"family":"Hill","given":"Mary","email":"mchill@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":247084,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doherty, John","contributorId":43843,"corporation":false,"usgs":true,"family":"Doherty","given":"John","affiliations":[],"preferred":false,"id":247086,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}