{"pageNumber":"2677","pageRowStart":"66900","pageSize":"25","recordCount":184582,"records":[{"id":53854,"text":"sir20045036 - 2004 - Chemical Data for Detailed Studies of Irrigation Drainage in the Salton Sea Area, California, 1995?2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:43","indexId":"sir20045036","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5036","title":"Chemical Data for Detailed Studies of Irrigation Drainage in the Salton Sea Area, California, 1995?2001","docAbstract":"The primary purpose of this report is to present all chemical data from the Salton Sea area collected by the U.S. Geological Survey between 1995 and 2001. The data were collected primarily for the Department of the Interior's National Irrigation Water Quality Program (NIWQP). The report also contains a brief summary and citation to investigations done for the NIWQP between 1992 and 1995. The NIWQP began studies in the Salton Sea area in 1986 to evaluate effects on the environment from potential toxins, especially selenium, in irrigation-induced drainage. This data report is a companion to several reports published from the earlier studies and to interpretive publications that make use of historical and recent data from this area.\r\n\r\n    Data reported herein are from five collection studies. Water, bottom material, and suspended sediment collected in 1995-96 from the New River, the lower Colorado River, and the All-American Canal were analyzed for elements, semi-volatile (extractable) organic compounds, and organochlorine compounds. Sufficient suspended sediment for chemical analyses was obtained by tangential-flow filtration.\r\n    A grab sample of surficial bottom sediment collected from near the deepest part of the Salton Sea in 1996 was analyzed for 44 elements and organic and inorganic carbon. High selenium concentration confirmed the effective transfer (sequestration) of selenium into the bottom sediment. Similar grab samples were collected 2 years later (1998) from 11 locations in the Salton Sea and analyzed for elements, as before, and also for nutrients, organochlorine compounds, and polycyclic aromatic hydrocarbons. Nutrients were measured in bottom water, and water-column profiles were obtained for pH, conductance, temperature, and dissolved oxygen. Element and nutrient concentrations were obtained in 1999 from cores at 2 of the above 11 sites, in the north subbasin of the Salton Sea. The most-recent study reported herein was done in 2001 and contains element data on suspended material isolated by continuous-flow centrifugation on samples collected in transects extending out from the Whitewater, the Alamo, and the New Rivers into the Salton Sea. \r\n\r\n    Chemical data on suspended sediment and bottom material from tributory rivers and the Salton Sea itself show that many insoluble constituents, including selenium and DDE, are concentrated in the fine-grained, organic- and carbonate-rich bottom sediment from deep areas near the center of the Salton Sea. Data also show that selenium and arsenic are markedly enriched in seston (plankton, partially-degraded algal detritus, and mineral matter that compose suspended particulates in the lake) collected just below the water surface in the Salton Sea. This result indicates that bio-concentration in primary producers in the water column provides an important pathway whereby high selenium residues accumulate in fish and fish-eating birds at the Salton Sea.","language":"ENGLISH","doi":"10.3133/sir20045036","usgsCitation":"Schroeder, R.A., 2004, Chemical Data for Detailed Studies of Irrigation Drainage in the Salton Sea Area, California, 1995?2001: U.S. Geological Survey Scientific Investigations Report 2004-5036, 54 p., https://doi.org/10.3133/sir20045036.","productDescription":"54 p.","costCenters":[],"links":[{"id":4688,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5036/","linkFileType":{"id":5,"text":"html"}},{"id":177760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bdd","contributors":{"authors":[{"text":"Schroeder, Roy A. raschroe@usgs.gov","contributorId":1523,"corporation":false,"usgs":true,"family":"Schroeder","given":"Roy","email":"raschroe@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":248500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54029,"text":"wri034047 - 2004 - Development and Application of Watershed Regressions for Pesticides (WARP) for Estimating Atrazine Concentration Distributions in Streams","interactions":[],"lastModifiedDate":"2012-02-02T00:11:55","indexId":"wri034047","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","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":"2003-4047","title":"Development and Application of Watershed Regressions for Pesticides (WARP) for Estimating Atrazine Concentration Distributions in Streams","docAbstract":"Regression models were developed for predicting atrazine concentration distributions in rivers and streams, using the Watershed Regressions for Pesticides (WARP) methodology. Separate regression equations were derived for each of nine percentiles of the annual distribution of atrazine concentrations and for the annual time-weighted mean atrazine concentration. In addition, seasonal models were developed for two specific periods of the year--the high season, when the highest atrazine concentrations are expected in streams, and the low season, when concentrations are expected to be low or undetectable. Various nationally available watershed parameters were used as explanatory variables, including atrazine use intensity, soil characteristics, hydrologic parameters, climate and weather variables, land use, and agricultural management practices. Concentration data from 112 river and stream stations sampled as part of the U.S. Geological Survey's National Water-Quality Assessment and National Stream Quality Accounting Network Programs were used for computing the concentration percentiles and mean concentrations used as the response variables in regression models. Tobit regression methods, using maximum likelihood estimation, were used for developing the models because some of the concentration values used for the response variables were censored (reported as less than a detection threshold). Data from 26 stations not used for model development were used for model validation.\r\n\r\n     The annual models accounted for 62 to 77 percent of the variability in concentrations among the 112 model development stations. Atrazine use intensity (the amount of atrazine used in the watershed divided by watershed area) was the most important explanatory variable in all models, but additional watershed parameters significantly increased the amount of variability explained by the models. Predicted concentrations from all 10 models were within a factor of 10 of the observed concentrations at most model development and model validation stations. Results for the two sets of seasonal models were similar. Concentration distributions derived from the seasonal-model predictions provided additional information compared to distributions derived from the annual models.","language":"ENGLISH","doi":"10.3133/wri034047","usgsCitation":"Larson, S., Crawford, C.G., and Gilliom, R.J., 2004, Development and Application of Watershed Regressions for Pesticides (WARP) for Estimating Atrazine Concentration Distributions in Streams: U.S. Geological Survey Water-Resources Investigations Report 2003-4047, 81 p., https://doi.org/10.3133/wri034047.","productDescription":"81 p.","costCenters":[],"links":[{"id":174400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5472,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034047/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672d8","contributors":{"authors":[{"text":"Larson, Steven J.","contributorId":29845,"corporation":false,"usgs":true,"family":"Larson","given":"Steven J.","affiliations":[],"preferred":false,"id":248969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":248967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57784,"text":"sir20045031 - 2004 - Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin","interactions":[],"lastModifiedDate":"2015-11-16T12:14:24","indexId":"sir20045031","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5031","title":"Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin","docAbstract":"<p>Numerical models were constructed for simulation of ground-water flow in the Menomonee Valley Brownfield, in Milwaukee, Wisconsin. An understanding of ground-water flow is necessary to develop an efficient program to sample ground water for contaminants. Models were constructed in a stepwise fashion, beginning with a regional, single-layer, analytic-element model (GFLOW code) that provided boundary conditions for a local, eight layer, finite-difference model (MODFLOW code) centered on the Menomonee Valley Brownfield. The primary source of ground water to the models is recharge over the model domains; primary sinks for ground water within the models are surface-water features and the Milwaukee Metropolitan Sewerage District Inline Storage System (ISS). Calibration targets were hydraulic heads, surface-water fluxes, vertical gradients, and ground-water infiltration to the ISS. Simulation of ground-water flow by use of the MODFLOW model indicates that about 73 percent of recharge within the MODFLOW domain circulates to the ISS and 27 percent discharges to gaining surface-water bodies. In addition, infiltration to the ISS comes from the following sources: 36 percent from recharge within the model domain, 45 percent from lateral flow into the domain, 15 percent from Lake Michigan, and 4 percent from other surface-water bodies. Particle tracking reveals that the median traveltime from the recharge point to surface-water features is 8 years; the median time to the ISS is 255 years. The traveltimes to the ISS are least over the northern part of the valley, where dolomite is near the land surface. The distribution of traveltimes in the MODFLOW simulation is greatly influenced by the effective porosity values assigned to the various lithologies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045031","collaboration":"In cooperation with the U.S. Environmental Protection Agency, Region 5, and City of Milwaukee, Wisconsin","usgsCitation":"Dunning, C.P., Feinstein, D.T., Hunt, R.J., and Krohelski, J.T., 2004, Simulation of ground-water flow, surface-water flow, and a deep sewer tunnel system in the Menomonee Valley, Milwaukee, Wisconsin: U.S. Geological Survey Scientific Investigations Report 2004-5031, vi, 40 p., https://doi.org/10.3133/sir20045031.","productDescription":"vi, 40 p.","numberOfPages":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":182239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5742,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5031/","linkFileType":{"id":5,"text":"html"}},{"id":311359,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2004/5031/pdf/2004-5031_Menomonee.pdf"}],"scale":"48","country":"United States","state":"Wisconsin","city":"Milwaukee","otherGeospatial":"Menominee Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.97697067260742,\n              42.995607893370135\n            ],\n            [\n              -87.97697067260742,\n              43.059857997098916\n            ],\n            [\n              -87.87895202636719,\n              43.059857997098916\n            ],\n            [\n              -87.87895202636719,\n              42.995607893370135\n            ],\n            [\n              -87.97697067260742,\n              42.995607893370135\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f246f","contributors":{"authors":[{"text":"Dunning, C. P.","contributorId":35792,"corporation":false,"usgs":true,"family":"Dunning","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":257777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feinstein, D. T.","contributorId":47328,"corporation":false,"usgs":true,"family":"Feinstein","given":"D.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":257779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunt, R. J.","contributorId":40164,"corporation":false,"usgs":true,"family":"Hunt","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":257778,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krohelski, J. T.","contributorId":59046,"corporation":false,"usgs":true,"family":"Krohelski","given":"J.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":257780,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":57805,"text":"sir20045067 - 2004 - Ground-water quality of coastal aquifer systems in the West Coast Basin, Los Angeles County, California, 1999-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"sir20045067","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5067","title":"Ground-water quality of coastal aquifer systems in the West Coast Basin, Los Angeles County, California, 1999-2002","docAbstract":"The extensive use of ground water throughout the Central and West Coast Basins of Los Angeles County during the first half of the 20th century resulted in declining water levels, widespread seawater intrusion, and deterioration of water quality along most reaches of the coast. In order to control seawater intrusion in the West Coast Basin, freshwater is injected into a series of wells at two seawater barrier projects. In order to better understand the processes of seawater intrusion and the efficiency of current barrier operation, data were collected from multiple-well monitoring sites installed by the U.S. Geological Survey, from local observation wells, and from production wells. The occurrence and areal extent of native, saline, and recently injected ground water near the coast were defined through the collection and analysis of inorganic and isotopic water-quality data and geophysical logs. \r\n\r\n     Most water in the West Coast Basin with a dissolved-solids concentration less than 500 milligrams per liter generally has a sodium-bicarbonate to sodium/calcium-bicarbonate character. Water with a dissolved-solids concentration greater than 1,000 milligrams per liter also contains variable amounts of calcium and sodium, but chloride is predominant. Most of these high-dissolved-solids wells are perforated in the Upper aquifer systems; several have dissolved-chloride values near that of seawater. Elevated chloride concentrations were measured at many wells in both the Upper and Lower aquifer systems inland from the barrier projects. Although water levels have increased in many wells over the last 30 years, some of the wells do not show a corresponding decrease in dissolved chloride. \r\n\r\n     A detailed assessment of saline ground water was provided by examining the ratios of chloride to bromide, iodide, and boron. Seawater-freshwater mixing lines were constructed using all three ratios. These ion ratios also identify water affected by mixing with injected imported water and oil-field brine water. \r\n\r\n     Isotopic data -oxygen-18, deuterium, strontium-87, boron-11, tritium, and carbon-14-also were collected. The stable isotopes oxygen-18 and deuterium were used to distinguish between isotopically heavier water that originated in the Los Angeles Forebay, isotopically lighter water that originated in the Montebello Forebay, local recharge, and water containing a mixture of seawater and imported water. Tritium data were used to identify recent water (less than 50 years old) present in the Upper and Lower aquifer systems inland from the seawater barrier projects, and present locally near the Dominguez Gap. Carbon-14 data indicate that water with uncorrected ages ranging from about 4,000 years to more than 20,000 years before present occurs in the Lower aquifer systems and in the Pico unit. \r\n\r\n     Borehole electromagnetic conductivity logs, combined with gamma-ray logs, were used to identify potential saline zones throughout the entire well depth; this provides an indicator of intrusion in zones that are not being monitored by a piezometer. Temperature logging was used to track the thermal effects of the cooler water used for injection. Specific-conductance logs provided a screening-level indicator of poor-quality water in monitoring wells.","language":"ENGLISH","doi":"10.3133/sir20045067","usgsCitation":"Land, M., Reichard, E.G., Crawford, S.M., Everett, R., Newhouse, M.W., and Williams, C.F., 2004, Ground-water quality of coastal aquifer systems in the West Coast Basin, Los Angeles County, California, 1999-2002: U.S. Geological Survey Scientific Investigations Report 2004-5067, 88 p., https://doi.org/10.3133/sir20045067.","productDescription":"88 p.","costCenters":[],"links":[{"id":5765,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5067/","linkFileType":{"id":5,"text":"html"}},{"id":184120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae1f","contributors":{"authors":[{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":257844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reichard, Eric G. 0000-0002-7310-3866 egreich@usgs.gov","orcid":"https://orcid.org/0000-0002-7310-3866","contributorId":1207,"corporation":false,"usgs":true,"family":"Reichard","given":"Eric","email":"egreich@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":257842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crawford, Steven M.","contributorId":80714,"corporation":false,"usgs":true,"family":"Crawford","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257845,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Everett, Rhett R. 0000-0001-7983-6270 reverett@usgs.gov","orcid":"https://orcid.org/0000-0001-7983-6270","contributorId":843,"corporation":false,"usgs":true,"family":"Everett","given":"Rhett R.","email":"reverett@usgs.gov","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":false,"id":257841,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newhouse, Mark W.","contributorId":36181,"corporation":false,"usgs":true,"family":"Newhouse","given":"Mark","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":257843,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Williams, Colin F. 0000-0003-2196-5496 colin@usgs.gov","orcid":"https://orcid.org/0000-0003-2196-5496","contributorId":274,"corporation":false,"usgs":true,"family":"Williams","given":"Colin","email":"colin@usgs.gov","middleInitial":"F.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":257840,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":57802,"text":"sir20045116 - 2004 - Microbial and Dissolved Organic Carbon Characterization of Stormflow in the Santa Ana River at Imperial Highway, Southern California, 1999-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"sir20045116","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5116","title":"Microbial and Dissolved Organic Carbon Characterization of Stormflow in the Santa Ana River at Imperial Highway, Southern California, 1999-2002","docAbstract":"The Santa Ana River drains about 2,670 square miles of densely populated coastal southern California, near Los Angeles. Almost all the flow in the river, more than 200,000 acre-feet annually, is diverted to ponds where it infiltrates and recharges underlying aquifers pumped to supply water for more than 2 million people. Base flow in the river is almost entirely treated municipal wastewater discharged from upstream treatment plants and, in the past, stormflow was considered a source of high-quality water suitable for use as a source of ground-water recharge that would dilute poorer quality water recharged during base flow. \r\n\r\n     Stormflow in the Santa Ana River at the Imperial Highway diversion contains total coliform bacteria concentrations as high as 3,400,000 colonies per 100 mL (milliliters). Fecal indicator bacteria concentrations, including fecal coliforms, Escherichia coli, and enterococci, were as high as 310,000, 84,000, and 102,000 colonies per 100 mL, respectively. Although concentrations were high owing to urban runoff during the first stormflow of the rainy season, the highest concentrations occurred during the recessional flows of the first stormflow of the rainy season after streamflow returned to pre-storm conditions. Molecular indicators of microbiological organisms in stormflow, including phospholipid fatty acid (PLFA) and genetic data, show that the diversity of the total microbial population decreases during stormflow while fecal indicator bacteria concentrations increase. This suggests that the source of the bacteria must be poorly diverse and dominated by only a few types of bacteria. Although direct runoff of fecal indicator bacteria from urban areas occurs, this process cannot explain the very high concentrations of fecal indicator bacteria in runoff from upstream parts of the basin characterized by urban, agricultural (including more than 300,000 head of dairy cattle), and other land uses. Although other explanations are possible, fecal indicator bacteria concentrations and molecular microbiological data indicate accumulation and extended survival of bacteria in streambed sediments, and subsequent mobilization of those sediments and associated bacteria during stormflow. Both PLFA and genetic data indicate that water from dairy-waste storage ponds was not present during sampled stormflows. This is consistent with the relatively dry conditions and the absence of large stormflows during the study. \r\n\r\n     Dissolved organic carbon (DOC) concentrations in stormflow ranged from 3 to 15.3 mg/L. In general, concentrations increased during stormflow and were distributed across the stormflow hydrograph in a manner similar to that of fecal indicator bacteria. DOC concentrations typically remained high for several days after flow returned to pre-storm conditions. Ultraviolet absorbance, excitation emission spectroscopy, and sequential fractionation of DOC using XAD-8 and XAD-4 resins showed that the composition of DOC changed rapidly during stormflow. Hydrophobic and hydrophilic acids were the largest fraction of DOC composing between 27 and 45 percent and between 24 and 37 percent of the DOC, respectively. \r\n\r\n     The fraction of DOC composed of hydrophobic acids decreased due to urban runoff and increased during the recession of the first stormflow of the rainy season; the hydrophilic-acid fraction generally decreased throughout the stormflow hydrograph; the transhydrophilic-acid fraction did not vary greatly during stormflow; and the hydrophobic-neutral fraction increased from low values in base flow to almost 30 percent of the DOC after more soluble and more mobile hydrophobic and hydrophilic acids were washed from urban areas. Comparison of ultraviolet absorbance data with data collected during previous studies shows that the optical properties and, presumably, the composition of the DOC were different in this study than DOC collected during wetter periods. \r\n\r\n     Samples of shallow ground water collec","language":"ENGLISH","doi":"10.3133/sir20045116","usgsCitation":"Izbicki, J., Pimentel, M.I., Leddy, M., and Bergamaschi, B., 2004, Microbial and Dissolved Organic Carbon Characterization of Stormflow in the Santa Ana River at Imperial Highway, Southern California, 1999-2002 (Online Only): U.S. Geological Survey Scientific Investigations Report 2004-5116, 80 p., https://doi.org/10.3133/sir20045116.","productDescription":"80 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":184035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5762,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5116/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62dec4","contributors":{"authors":[{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":257828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pimentel, M. Isabel","contributorId":54257,"corporation":false,"usgs":true,"family":"Pimentel","given":"M.","email":"","middleInitial":"Isabel","affiliations":[],"preferred":false,"id":257831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leddy, Menu","contributorId":11697,"corporation":false,"usgs":true,"family":"Leddy","given":"Menu","email":"","affiliations":[],"preferred":false,"id":257830,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bergamaschi, Brian A. 0000-0002-9610-5581 bbergama@usgs.gov","orcid":"https://orcid.org/0000-0002-9610-5581","contributorId":1448,"corporation":false,"usgs":true,"family":"Bergamaschi","given":"Brian A.","email":"bbergama@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":257829,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":57807,"text":"ofr20041273 - 2004 - Selected presentations on coal-bed gas in the eastern United States","interactions":[],"lastModifiedDate":"2022-06-29T18:18:31.74269","indexId":"ofr20041273","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","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":"2004-1273","title":"Selected presentations on coal-bed gas in the eastern United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041273","usgsCitation":"Warwick, P.D., 2004, Selected presentations on coal-bed gas in the eastern United States (Version 1.0): U.S. Geological Survey Open-File Report 2004-1273, 96 p., https://doi.org/10.3133/ofr20041273.","productDescription":"96 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":184932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5767,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1273/","linkFileType":{"id":5,"text":"html"}},{"id":402702,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68862.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.681640625,\n              28.65203063036226\n            ],\n            [\n              -71.71875,\n              28.65203063036226\n            ],\n            [\n              -71.71875,\n              43.26120612479979\n            ],\n            [\n              -88.681640625,\n              43.26120612479979\n            ],\n            [\n              -88.681640625,\n              28.65203063036226\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6981b8","contributors":{"authors":[{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":257851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57806,"text":"ofr20041256 - 2004 - Surficial geology and analysis of post impoundment sediment of Lake Mohave; interpretation of sidescan sonar and seismic-reflection data","interactions":[],"lastModifiedDate":"2022-12-01T19:36:13.721816","indexId":"ofr20041256","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","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":"2004-1256","title":"Surficial geology and analysis of post impoundment sediment of Lake Mohave; interpretation of sidescan sonar and seismic-reflection data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041256","usgsCitation":"Foster, D.S., Capone, M.K., Parolski, K.F., Twichell, D.C., and Rudin, M.J., 2004, Surficial geology and analysis of post impoundment sediment of Lake Mohave; interpretation of sidescan sonar and seismic-reflection data: U.S. Geological Survey Open-File Report 2004-1256, HTML Document, https://doi.org/10.3133/ofr20041256.","productDescription":"HTML Document","costCenters":[],"links":[{"id":184931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":409934,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68861.htm","linkFileType":{"id":5,"text":"html"}},{"id":5766,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1256/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, Nevada","otherGeospatial":"Lake Mohave","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.78761935621542,\n              36.00512225424448\n            ],\n            [\n              -114.78761935621542,\n              35.2045559699329\n            ],\n            [\n              -114.53089279149953,\n              35.2045559699329\n            ],\n            [\n              -114.53089279149953,\n              36.00512225424448\n            ],\n            [\n              -114.78761935621542,\n              36.00512225424448\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bfa","contributors":{"authors":[{"text":"Foster, David S. 0000-0003-1205-0884 dfoster@usgs.gov","orcid":"https://orcid.org/0000-0003-1205-0884","contributorId":1320,"corporation":false,"usgs":true,"family":"Foster","given":"David","email":"dfoster@usgs.gov","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":257846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capone, Mark K.","contributorId":16903,"corporation":false,"usgs":true,"family":"Capone","given":"Mark","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":257848,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parolski, Kenneth F.","contributorId":6452,"corporation":false,"usgs":true,"family":"Parolski","given":"Kenneth","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":257847,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":257849,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rudin, Mark J.","contributorId":45345,"corporation":false,"usgs":true,"family":"Rudin","given":"Mark","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":257850,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57816,"text":"sir20045077 - 2004 - Simulated effects of impoundment of lake seminole on ground-water flow in the upper Floridan Aquifer in southwestern Georgia and adjacent parts of Alabama and Florida","interactions":[],"lastModifiedDate":"2017-01-31T08:41:43","indexId":"sir20045077","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5077","title":"Simulated effects of impoundment of lake seminole on ground-water flow in the upper Floridan Aquifer in southwestern Georgia and adjacent parts of Alabama and Florida","docAbstract":"Hydrologic implications of the impoundment of Lake Seminole in southwest Georgia and its effect on components of the surface- and ground-water flow systems of the lower Apalachicola?Chattahoochee?Flint (ACF) River Basin were investigated using a ground-water model. Comparison of simulation results of postimpoundment drought conditions (October 1986) with results of hypothetical preimpoundment conditions (a similar drought prior to 1955) provides a qualitative measure of the changes in hydraulic head and ground-water flow to and from streams and Lake Seminole, and across State lines caused by the impoundment.\r\n\r\nBased on the simulation results, the impoundment of Lake Seminole changed ground-water flow directions within about 20?30 miles of the lake, reducing the amount of ground water flowing from Florida to Georgia southeast of the lake. Ground-water storage was increased by the impoundment, as indicated by a simulated increase of as much as 26 feet in the water level in the Upper Floridan aquifer. The impoundment of Lake Seminole caused changes to simulated components of the ground-water budget, including reduced discharge from the Upper Floridan aquifer to streams (315 million gallons per day); reduced recharge from or increased discharge to regional ground-water flow at external model boundaries (totaling 183 million gallons per day); and reduced recharge from or increased discharge to the undifferentiated overburden (totaling 129 million gallons per day).","language":"ENGLISH","doi":"10.3133/sir20045077","usgsCitation":"Jones, L.E., and Torak, L.J., 2004, Simulated effects of impoundment of lake seminole on ground-water flow in the upper Floridan Aquifer in southwestern Georgia and adjacent parts of Alabama and Florida: U.S. Geological Survey Scientific Investigations Report 2004-5077, 18 p., https://doi.org/10.3133/sir20045077.","productDescription":"18 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":184913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5794,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5077/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama, Florida, Georgia","otherGeospatial":"Upper Floridan Aquifer ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.385498046875,\n              29.017748018496047\n            ],\n            [\n              -86.385498046875,\n              33.4955977448657\n            ],\n            [\n              -82.72705078125,\n              33.4955977448657\n            ],\n            [\n              -82.72705078125,\n              29.017748018496047\n            ],\n            [\n              -86.385498046875,\n              29.017748018496047\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984d6","contributors":{"authors":[{"text":"Jones, L. Elliott 0000-0002-7394-2053 lejones@usgs.gov","orcid":"https://orcid.org/0000-0002-7394-2053","contributorId":44569,"corporation":false,"usgs":true,"family":"Jones","given":"L.","email":"lejones@usgs.gov","middleInitial":"Elliott","affiliations":[],"preferred":false,"id":257881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Torak, Lynn J. ljtorak@usgs.gov","contributorId":401,"corporation":false,"usgs":true,"family":"Torak","given":"Lynn","email":"ljtorak@usgs.gov","middleInitial":"J.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":257880,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57872,"text":"fs20043073 - 2004 - PNSN, Pacific Northwest Seismograph Network","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"fs20043073","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-3073","title":"PNSN, Pacific Northwest Seismograph Network","language":"ENGLISH","doi":"10.3133/fs20043073","usgsCitation":"Ludwin, R., 2004, PNSN, Pacific Northwest Seismograph Network: U.S. Geological Survey Fact Sheet 2004-3073, 1 sheet ([2] p.) : col. ill., col. map ; 28 x 18 cm., https://doi.org/10.3133/fs20043073.","productDescription":"1 sheet ([2] p.) : col. ill., col. map ; 28 x 18 cm.","costCenters":[],"links":[{"id":120641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3073.bmp"},{"id":5809,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2004/3073/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689e0e","contributors":{"authors":[{"text":"Ludwin, R.S.","contributorId":55459,"corporation":false,"usgs":true,"family":"Ludwin","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":257915,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57799,"text":"sir20045089 - 2004 - Water, ice, and meteorological measurements at South Cascade Glacier, Washington, balance year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"sir20045089","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5089","title":"Water, ice, and meteorological measurements at South Cascade Glacier, Washington, balance year 2002","docAbstract":"Winter snow accumulation and summer snow and ice ablation were measured at South Cascade Glacier, Washington, to estimate glacier mass balance quantities for balance year 2002. The 2002 glacier-average maximum winter snow balance was 4.02 meters, the second largest since 1959. The 2002 glacier summer, net, and annual (water year) balances were -3.47, 0.55, and 0.54 meters, respectively. The area of the glacier near the end of the balance year was 1.92 square kilometers, and the equilibrium-line altitude and the accumulation area ratio were 1,820 meters and 0.84, respectively. During September 20, 2001 to September 13, 2002, the terminus retreated 4 meters, and computed average ice speeds in the ablation area ranged from 7.8 to 20.7 meters per year. Runoff from the subbasin containing the glacier and from an adjacent non-glacierized basin were measured during part of the 2002 water year. Air temperature, precipitation, atmospheric water-vapor pressure, wind speed and incoming solar radiation were measured at selected locations near the glacier.","language":"ENGLISH","doi":"10.3133/sir20045089","usgsCitation":"Bidlake, W.R., Josberger, E.G., and Savoca, M.E., 2004, Water, ice, and meteorological measurements at South Cascade Glacier, Washington, balance year 2002: U.S. Geological Survey Scientific Investigations Report 2004-5089, 50 p., https://doi.org/10.3133/sir20045089.","productDescription":"50 p.","costCenters":[],"links":[{"id":183947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5759,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045089/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697973","contributors":{"authors":[{"text":"Bidlake, William R. wbidlake@usgs.gov","contributorId":1712,"corporation":false,"usgs":true,"family":"Bidlake","given":"William","email":"wbidlake@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":257824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Josberger, Edward G. ejosberg@usgs.gov","contributorId":1710,"corporation":false,"usgs":true,"family":"Josberger","given":"Edward","email":"ejosberg@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":257823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savoca, Mark E. mesavoca@usgs.gov","contributorId":1961,"corporation":false,"usgs":true,"family":"Savoca","given":"Mark","email":"mesavoca@usgs.gov","middleInitial":"E.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":257825,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57797,"text":"ofr20041230 - 2004 - Data from channel-change monitoring at selected sites in Maricopa County, Arizona, 1997-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:12:20","indexId":"ofr20041230","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","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":"2004-1230","title":"Data from channel-change monitoring at selected sites in Maricopa County, Arizona, 1997-2002","docAbstract":"Stream channels in arid regions are subject to a wide range of hydrologic, hydraulic, and sedimentary conditions. These channels often are dry or have little streamflow most of the time, and the few flows that do occur can cause substantial changes to the channel and flood plain. Because floods in arid regions are often flashy, and many gaging stations are in remote areas, hydrographers must rely on indirect measurements of streamflow. Channel change is important because one major assumption necessary for indirect measurements of discharge is that the channel conditions after the flood represent the conditions during the peak discharge.\r\n\r\nThe U.S. Geological Survey, in cooperation with the Flood Control District of Maricopa County, is monitoring selected perennial and ephemeral streams within Maricopa County, Arizona, to track the amount and variability of channel change. This report contains basic data from surveys of monumented cross sections conducted from 1997 through 2002. The amount of change varied widely from channel to channel, and the largest geomorphic change occurred in conjunction with peak flows above the 10-year recurrence interval.","language":"ENGLISH","doi":"10.3133/ofr20041230","usgsCitation":"O’Day, C.M., 2004, Data from channel-change monitoring at selected sites in Maricopa County, Arizona, 1997-2002 (Online Only): U.S. Geological Survey Open-File Report 2004-1230, 61 p., https://doi.org/10.3133/ofr20041230.","productDescription":"61 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":183945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5757,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr20041230/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c895","contributors":{"authors":[{"text":"O’Day, Christine M.","contributorId":87625,"corporation":false,"usgs":true,"family":"O’Day","given":"Christine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57730,"text":"fs20043091 - 2004 - Linking selenium sources to ecosystems: San Francisco Bay-Delta Model","interactions":[],"lastModifiedDate":"2020-02-09T16:53:38","indexId":"fs20043091","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-3091","title":"Linking selenium sources to ecosystems: San Francisco Bay-Delta Model","docAbstract":"<p><span>Marine sedimentary rocks of the Coast Ranges contribute selenium to soil, surface water, and ground water in the western San Joaquin Valley, California. Irrigation funnels selenium into a network of subsurface drains and canals. Proposals to build a master drain (i.e., San Luis Drain) to discharge into the San Francisco Bay-Delta Estuary remain as controversial today as they were in the 1950s, when drainage outside the San Joaquin Valley was first considered. An existing 85-mile portion of the San Luis Drain was closed in 1986 after fish mortality and deformities in ducks, grebes and coots were discovered at Kesterson National Wildlife Refuge, the temporary terminus of the drain. A 28-mile portion of the drain now conveys drainage from 100,000 acres into the San Joaquin River and eventually into the Bay-Delta. If the San Luis Drain is extended directly to the Bay-Delta, as is now being proposed as an alternative to sustain agriculture, it could receive drainage from an estimated one-million acres of farmland affected by rising water tables and increasing salinity. In addition to agricultural sources, oil refineries also discharge selenium to the Bay-Delta, although those discharges have declined in recent years. To understand the effects of changing selenium inputs, scientists have developed the Bay-Delta Selenium Model.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20043091","usgsCitation":"Presser, T.S., and Luoma, S.N., 2004, Linking selenium sources to ecosystems: San Francisco Bay-Delta Model: U.S. Geological Survey Fact Sheet 2004-3091, 4 p., https://doi.org/10.3133/fs20043091.","productDescription":"4 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":5981,"rank":99,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2004-3091/","linkFileType":{"id":5,"text":"html"}},{"id":338509,"rank":3,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2004/3091/coverthb2.jpg"},{"id":338426,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2004/3091/pdf/FS2004-3091.pdf","text":"Report","size":"1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2004-3091"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.211669921875,\n              37.34395908944491\n            ],\n            [\n              -120.73974609374999,\n              37.34395908944491\n            ],\n            [\n              -120.73974609374999,\n              38.40194908237822\n            ],\n            [\n              -123.211669921875,\n              38.40194908237822\n            ],\n            [\n              -123.211669921875,\n              37.34395908944491\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a5082","contributors":{"authors":[{"text":"Presser, Theresa S. 0000-0001-5643-0147 tpresser@usgs.gov","orcid":"https://orcid.org/0000-0001-5643-0147","contributorId":2467,"corporation":false,"usgs":true,"family":"Presser","given":"Theresa","email":"tpresser@usgs.gov","middleInitial":"S.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":687765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":687766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57753,"text":"sir20045034 - 2004 - External quality-assurance results for the national atmospheric deposition program/national trends network, 2000-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:12:33","indexId":"sir20045034","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5034","title":"External quality-assurance results for the national atmospheric deposition program/national trends network, 2000-2001","docAbstract":"Five external quality-assurance programs were operated by the U.S. Geological Survey for the National Atmospheric Deposition Program/National Trends Network (NADP/NTN) from 2000 through 2001 (study period): the intersite-comparison program, the blind-audit program, the field-audit program, the interlaboratory-comparison program, and the collocated-sampler program. Each program is designed to measure specific components of the total error inherent in NADP/NTN wet-deposition measurements. \r\n\r\nThe intersite-comparison program assesses the variability and bias of pH and specific-conductance determinations made by NADP/NTN site operators with respect to accuracy goals. The accuracy goals are statistically based using the median of all of the measurements obtained for each of four intersite-comparison studies. The percentage of site operators responding on time that met the pH accuracy goals ranged from 84.2 to 90.5 percent. In these same four intersite-comparison studies, 88.9 to 99.0 percent of the site operators met the accuracy goals for specific conductance. \r\n\r\nThe blind-audit program evaluates the effects of routine sample handling, processing, and shipping on the chemistry of weekly precipitation samples. The blind-audit data for the study period indicate that sample handling introduced a small amount of sulfate contamination and slight changes to hydrogen-ion content of the precipitation samples. The magnitudes of the paired differences are not environmentally significant to NADP/NTN data users. \r\n\r\nThe field-audit program (also known as the 'field-blank program') was designed to measure the effects of field exposure, handling, and processing on the chemistry of NADP/NTN precipitation samples. The results indicate potential low-level contamination of NADP/NTN samples with calcium, ammonium, chloride, and nitrate. Less sodium contamination was detected by the field-audit data than in previous years. Statistical analysis of the paired differences shows that contaminant ions are entrained into the solutions from the field-exposed buckets, but the positive bias that results from the minor amount of contamination appears to affect the analytical results by less than 6 percent. \r\n\r\nAn interlaboratory-comparison program is used to estimate the analytical variability and bias of participating laboratories, especially the NADP Central Analytical Laboratory (CAL). Statistical comparison of the analytical results of participating laboratories implies that analytical data from the various monitoring networks can be compared. Bias was identified in the CAL data for ammonium, chloride, nitrate, sulfate, hydrogen-ion, and specific-conductance measurements, but the absolute value of the bias was less than analytical minimum reporting limits for all constituents except ammonium and sulfate. Control charts show brief time periods when the CAL's analytical precision for sodium, ammonium, and chloride was not within the control limits. Data for the analysis of ultrapure deionized-water samples indicated that the laboratories are maintaining good control of laboratory contamination. Estimated analytical precision among the laboratories indicates that the magnitudes of chemical-analysis errors are not environmentally significant to NADP data users. \r\n\r\nOverall precision of the precipitation-monitoring system used by the NADP/NTN was estimated by evaluation of samples from collocated monitoring sites at CA99, CO08, and NH02. Precision defined by the median of the absolute percent difference (MAE) was estimated to be approximately 10 percent or less for calcium, magnesium, sodium, chloride, nitrate, sulfate, specific conductance, and sample volume. The MAE values for ammonium and hydrogen-ion concentrations were estimated to be less than 10 percent for CA99 and NH02 but nearly 20 percent for ammonium concentration and about 17 percent for hydrogen-ion concentration for CO08. \r\n\r\nAs in past years, the variability in the collocated-site data for sam","language":"ENGLISH","doi":"10.3133/sir20045034","usgsCitation":"Wetherbee, G.A., Latysh, N.E., and Gordon, J.D., 2004, External quality-assurance results for the national atmospheric deposition program/national trends network, 2000-2001: U.S. Geological Survey Scientific Investigations Report 2004-5034, 68 p., https://doi.org/10.3133/sir20045034.","productDescription":"68 p.","costCenters":[],"links":[{"id":5996,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045034/","linkFileType":{"id":5,"text":"html"}},{"id":182575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a27","contributors":{"authors":[{"text":"Wetherbee, Gregory A. 0000-0002-6720-2294 wetherbe@usgs.gov","orcid":"https://orcid.org/0000-0002-6720-2294","contributorId":1044,"corporation":false,"usgs":true,"family":"Wetherbee","given":"Gregory","email":"wetherbe@usgs.gov","middleInitial":"A.","affiliations":[{"id":143,"text":"Branch of Quality Systems","active":true,"usgs":true}],"preferred":true,"id":257698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Latysh, Natalie E.","contributorId":39860,"corporation":false,"usgs":true,"family":"Latysh","given":"Natalie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":257699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, John D. 0000-0001-8396-8524 jgordon@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-8524","contributorId":347,"corporation":false,"usgs":true,"family":"Gordon","given":"John","email":"jgordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":257697,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56827,"text":"sir20045035 - 2004 - Sedimentation Survey of Lago Toa Vaca, Puerto Rico, June-July 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:49","indexId":"sir20045035","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5035","title":"Sedimentation Survey of Lago Toa Vaca, Puerto Rico, June-July 2002","docAbstract":"The Lago Toa Vaca dam is located in the municipality of Villalba in southern Puerto Rico, and is owned and operated by the Puerto Rico Aqueduct and Sewer Authority. Construction was completed in 1972 as the first phase of a multi-purpose project that contemplated four possible diversions from other basins to mitigate the rapid storage capacity loss of Lago Guayabal, located immediately downstream of the Toa Vaca dam. The latter phases of the intra-basin diversions were cancelled, and currently, the reservoir receives runoff from only 56.8 square kilometers of its drainage area. \r\n\r\nLago Toa Vaca reservoir when constructed was to be used for irrigation of croplands in the southern coastal plain. The reservoir had an original storage capacity of 68.94 million cubic meters. Sedimentation has reduced the storage capacity by only 7 percent between 1972 and 2002 to 64.08 million cubic meters. This represents a long-term sedimentation rate of about 162,000 cubic meters per year. \r\n\r\nBased on the 2002 sedimentation survey, Lago Toa Vaca has a sediment trapping efficiency of about 98 percent and a drainage area-normalized sedimentation rate of about 3,086 cubic meters per square kilometer per year between 1972 and 2002. At the current long-term sedimentation rate the reservoir would lose its storage capacity by the year 2400.","language":"ENGLISH","doi":"10.3133/sir20045035","usgsCitation":"Soler-Lopez, L.R., 2004, Sedimentation Survey of Lago Toa Vaca, Puerto Rico, June-July 2002: U.S. Geological Survey Scientific Investigations Report 2004-5035, 32 p., https://doi.org/10.3133/sir20045035.","productDescription":"32 p.","costCenters":[],"links":[{"id":5672,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045035/","linkFileType":{"id":5,"text":"html"}},{"id":175116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f48ff","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":255814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56324,"text":"ofr20041219 - 2004 - Summary of Suspended-Sediment Concentration Data, San Francisco Bay, California, Water Year 2002","interactions":[],"lastModifiedDate":"2016-07-26T16:31:10","indexId":"ofr20041219","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","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":"2004-1219","title":"Summary of Suspended-Sediment Concentration Data, San Francisco Bay, California, Water Year 2002","docAbstract":"<p>Suspended-sediment concentration data were collected in San Francisco Bay during water year 2002 (October 1, 2001-September 30, 2002). Optical backscatterance sensors and water samples were used to monitor suspended sediment at two sites in Suisun Bay, three sites in San Pablo Bay, two sites in Central San Francisco Bay, and three sites in South San Francisco Bay. Sensors were positioned at two depths at most sites. Water samples were collected periodically and were analyzed for concentrations of suspended sediment. The results of the analyses were used to calibrate the electrical output of the optical backscatterance sensors so that a record of suspended-sediment concentrations could be derived. This report presents the data-collection methods used and summarizes the suspended-sediment concentration data collected from October 2001 through September 2002. Calibration curves and plots of edited data for each sensor also are presented.</p>","language":"ENGLISH","doi":"10.3133/ofr20041219","usgsCitation":"Buchanan, P.A., and Ganju, N., 2004, Summary of Suspended-Sediment Concentration Data, San Francisco Bay, California, Water Year 2002: U.S. Geological Survey Open-File Report 2004-1219, 54 p., https://doi.org/10.3133/ofr20041219.","productDescription":"54 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":184840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5700,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1219/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699486","contributors":{"authors":[{"text":"Buchanan, Paul A. 0000-0002-4796-4734 buchanan@usgs.gov","orcid":"https://orcid.org/0000-0002-4796-4734","contributorId":1018,"corporation":false,"usgs":true,"family":"Buchanan","given":"Paul","email":"buchanan@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":255232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ganju, Neil K. 0000-0002-1096-0465","orcid":"https://orcid.org/0000-0002-1096-0465","contributorId":93543,"corporation":false,"usgs":true,"family":"Ganju","given":"Neil K.","affiliations":[],"preferred":false,"id":255233,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56328,"text":"fs20043062 - 2004 - Climatic fluctuations, drought, and flow of the Colorado River","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"fs20043062","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-3062","title":"Climatic fluctuations, drought, and flow of the Colorado River","language":"ENGLISH","doi":"10.3133/fs20043062","usgsCitation":"Webb, R., McCabe, G., Hereford, R., and Wilkowske, C.D., 2004, Climatic fluctuations, drought, and flow of the Colorado River (Version 2 - Aug 2004): U.S. Geological Survey Fact Sheet 2004-3062, 4 p., https://doi.org/10.3133/fs20043062.","productDescription":"4 p.","costCenters":[],"links":[{"id":120645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3062.jpg"},{"id":5701,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2004-3062/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 2 - Aug 2004","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de130","contributors":{"authors":[{"text":"Webb, Robert H. rhwebb@usgs.gov","contributorId":1573,"corporation":false,"usgs":false,"family":"Webb","given":"Robert H.","email":"rhwebb@usgs.gov","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":255242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCabe, Gregory J. 0000-0002-9258-2997 gmccabe@usgs.gov","orcid":"https://orcid.org/0000-0002-9258-2997","contributorId":1453,"corporation":false,"usgs":true,"family":"McCabe","given":"Gregory J.","email":"gmccabe@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":255241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hereford, Richard 0000-0002-0892-7367 rhereford@usgs.gov","orcid":"https://orcid.org/0000-0002-0892-7367","contributorId":3620,"corporation":false,"usgs":true,"family":"Hereford","given":"Richard","email":"rhereford@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":255243,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilkowske, Christopher D. wilkowsk@usgs.gov","contributorId":1144,"corporation":false,"usgs":true,"family":"Wilkowske","given":"Christopher","email":"wilkowsk@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":false,"id":255240,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70239788,"text":"70239788 - 2004 - Tidal triggering caught in the act","interactions":[],"lastModifiedDate":"2023-01-19T23:03:11.001149","indexId":"70239788","displayToPublicDate":"2004-08-27T16:54:39","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tidal triggering caught in the act","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.1100726","usgsCitation":"Stein, R.S., 2004, Tidal triggering caught in the act: Science, v. 305, no. 5688, p. 1248-1249, https://doi.org/10.1126/science.1100726.","productDescription":"2 p.","startPage":"1248","endPage":"1249","costCenters":[],"links":[{"id":412093,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              130.2624851665547,\n              31.016871377471873\n            ],\n            [\n              130.71817693176672,\n              30.699870581802756\n            ],\n            [\n              131.63798556370062,\n              31.074572502104203\n            ],\n            [\n              132.01336556340834,\n              32.42818275824477\n            ],\n            [\n              133.09956670096972,\n              32.74251368186246\n            ],\n            [\n              133.68461664218614,\n              33.18133000228731\n            ],\n            [\n              134.18927526112088,\n              32.87109601976043\n            ],\n            [\n              134.82291564737739,\n              33.63760238777\n            ],\n            [\n              135.79453504209698,\n              33.17286185982147\n            ],\n            [\n              136.4828866150138,\n              33.95690494591088\n            ],\n            [\n              137.4511150279037,\n              34.41585542715093\n            ],\n            [\n              138.33459839459954,\n              34.5010811858958\n            ],\n            [\n              138.84670709116222,\n              34.30113709932945\n            ],\n            [\n              140.08638161434158,\n              34.74797174284441\n            ],\n            [\n              141.0528724815705,\n              35.604542101944304\n            ],\n            [\n              140.8380882861378,\n              36.51917178956609\n            ],\n            [\n              141.26952252748367,\n              37.11197578573092\n            ],\n            [\n              141.28634806986616,\n              38.13085194234418\n            ],\n            [\n              142.0139963478921,\n              38.86018094340187\n            ],\n            [\n              142.2458872298888,\n              39.66143474742185\n            ],\n            [\n              142.03932021884395,\n              40.431395794744844\n            ],\n            [\n              141.64243607228627,\n              41.11513804842622\n            ],\n            [\n              141.67312377683345,\n              42.29192810081187\n            ],\n            [\n              143.46310603185202,\n              41.76344012601626\n            ],\n            [\n              143.974726299983,\n              42.779156919376874\n            ],\n            [\n              145.1265780469928,\n              42.84571080895492\n            ],\n            [\n              147.28655519725805,\n              43.67894563102763\n            ],\n            [\n              147.47135653056807,\n              44.33910252764221\n            ],\n            [\n              151.11350154740433,\n              45.95672315112944\n            ],\n            [\n              151.053311733211,\n              46.49357301179384\n            ],\n            [\n              149.99592082829497,\n              46.501078671174554\n            ],\n            [\n              145.5963933670855,\n              44.64870169360202\n            ],\n            [\n              144.08053718416392,\n              44.23508517806425\n            ],\n            [\n              142.3939680131508,\n              45.45655334121881\n            ],\n            [\n              141.26260313462342,\n              45.89030808231607\n            ],\n            [\n              140.59900272926228,\n              45.656855806710695\n            ],\n            [\n              140.8220119232053,\n              44.946505128909365\n            ],\n            [\n              141.42190844148098,\n              44.84704324753227\n            ],\n            [\n              141.18820072230108,\n              44.09863930904385\n            ],\n            [\n              139.49131354983678,\n              42.82411195793037\n            ],\n            [\n              139.0458318594919,\n              42.159440876191724\n            ],\n            [\n              139.5280155515166,\n              40.7876932492637\n            ],\n            [\n              139.02343865877253,\n              38.80350709701864\n            ],\n            [\n              136.34380336918662,\n              37.44239781244775\n            ],\n            [\n              136.2768928465655,\n              36.849769748818986\n            ],\n            [\n              135.54339553700947,\n              35.87697807520169\n            ],\n            [\n              132.81550277219378,\n              35.67221086071889\n            ],\n            [\n              130.69238901644565,\n              34.55391936686223\n            ],\n            [\n              130.42502452716815,\n              34.04903766840482\n            ],\n            [\n              129.20068464979715,\n              33.54248634098316\n            ],\n            [\n              129.6580862526473,\n              31.709728103540897\n            ],\n            [\n              130.2624851665547,\n              31.016871377471873\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"305","issue":"5688","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stein, Ross S. 0000-0001-7586-3933 rstein@usgs.gov","orcid":"https://orcid.org/0000-0001-7586-3933","contributorId":2604,"corporation":false,"usgs":true,"family":"Stein","given":"Ross","email":"rstein@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":861959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121930,"text":"70121930 - 2004 - New seafloor map of the Puerto Rico Trench helps assess earthquake and tsunami hazards","interactions":[],"lastModifiedDate":"2018-02-16T13:40:50","indexId":"70121930","displayToPublicDate":"2004-08-25T13:43:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"New seafloor map of the Puerto Rico Trench helps assess earthquake and tsunami hazards","docAbstract":"The Puerto Rico Trench, the deepest part of the Atlantic Ocean, is located where the North American (NOAM) plate is subducting under the Caribbean plate (Figure l). The trench region may pose significant seismic and tsunami hazards to Puerto Rico and the U.S.Virgin Islands, where 4 million U.S. citizens reside. Widespread damage in Puerto Rico and Hispaniola from an earthquake in 1787 was estimated to be the result of a magnitude 8 earthquake north of the islands [McCann et al., 2004]. A tsunami killed 40 people in NW Puerto Rico following a magnitude 7.3 earthquake in 1918 [Mercado and McCann, 1998]. Large landslide escarpments have been mapped on the seafloor north of Puerto Rico [Mercado et al., 2002; Schwab et al., 1991],although their ages are unknown.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Eos, Transactions American Geophysical Union","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1029/2004EO370001","usgsCitation":"ten Brink, U., Danforth, W., Polloni, C., Andrews, B., Llanes Estrada, P., Smith, S., Parker, E., and Uozumi, T., 2004, New seafloor map of the Puerto Rico Trench helps assess earthquake and tsunami hazards: Eos, Transactions, American Geophysical Union, v. 85, no. 37, p. 349-354, https://doi.org/10.1029/2004EO370001.","productDescription":"6 p.","startPage":"349","endPage":"354","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":478026,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1029/2004eo370001","text":"External Repository"},{"id":292989,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004EO370001"},{"id":292990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Puerto Rico","otherGeospatial":"Puerto Rico Trench","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -68.049,18.6523 ], [ -68.049,21.3363 ], [ -63.951,21.3363 ], [ -63.951,18.6523 ], [ -68.049,18.6523 ] ] ] } } ] }","volume":"85","issue":"37","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"53fc4dd9e4b0413fd75d6afc","contributors":{"authors":[{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":499357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danforth, William","contributorId":49026,"corporation":false,"usgs":true,"family":"Danforth","given":"William","affiliations":[],"preferred":false,"id":499353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Polloni, Christopher","contributorId":52451,"corporation":false,"usgs":true,"family":"Polloni","given":"Christopher","affiliations":[],"preferred":false,"id":499354,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Andrews, Brian D. bandrews@usgs.gov","contributorId":2132,"corporation":false,"usgs":true,"family":"Andrews","given":"Brian D.","email":"bandrews@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":499350,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Llanes Estrada, Pilar","contributorId":37264,"corporation":false,"usgs":true,"family":"Llanes Estrada","given":"Pilar","email":"","affiliations":[],"preferred":false,"id":499352,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Shepard","contributorId":69898,"corporation":false,"usgs":true,"family":"Smith","given":"Shepard","affiliations":[],"preferred":false,"id":499356,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Parker, Eugene","contributorId":52902,"corporation":false,"usgs":true,"family":"Parker","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":499355,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Uozumi, Toshihiko","contributorId":14518,"corporation":false,"usgs":true,"family":"Uozumi","given":"Toshihiko","email":"","affiliations":[],"preferred":false,"id":499351,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70121918,"text":"70121918 - 2004 - Physical geography: The global environment","interactions":[],"lastModifiedDate":"2017-08-28T11:02:35","indexId":"70121918","displayToPublicDate":"2004-08-25T12:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Physical geography: The global environment","docAbstract":"No abstract available.","language":"English","publisher":"Oxford University Press","usgsCitation":"de Blij, H.J., Muller, P.O., and Williams, R., 2004, Physical geography: The global environment (3), 702 p.","productDescription":"702 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":292977,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4ddee4b0413fd75d6b20","contributors":{"authors":[{"text":"de Blij, Harm J.","contributorId":102000,"corporation":false,"usgs":true,"family":"de Blij","given":"Harm","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":499337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muller, Peter O.","contributorId":10342,"corporation":false,"usgs":true,"family":"Muller","given":"Peter","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":499335,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Richard S. Jr.","contributorId":90679,"corporation":false,"usgs":true,"family":"Williams","given":"Richard S.","suffix":"Jr.","affiliations":[],"preferred":false,"id":499336,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70121915,"text":"70121915 - 2004 - Book review: Bard of Iceland: Jonas Hallgrimsson, poet and scientist","interactions":[],"lastModifiedDate":"2017-08-23T10:58:03","indexId":"70121915","displayToPublicDate":"2004-08-25T11:23:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1955,"text":"ISIS, Journal of the History of Science Society","active":true,"publicationSubtype":{"id":10}},"title":"Book review: Bard of Iceland: Jonas Hallgrimsson, poet and scientist","docAbstract":"<p>No abstract available<br></p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"ISIS, Journal of the History of Science Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"University of Chicago Press","doi":"10.1086/432341","usgsCitation":"Williams, R., 2004, Book review: Bard of Iceland: Jonas Hallgrimsson, poet and scientist: ISIS, Journal of the History of Science Society, v. 95, no. 4, p. 736-736, https://doi.org/10.1086/432341.","productDescription":"1 p.","startPage":"736","endPage":"736","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292974,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4de9e4b0413fd75d6b85","contributors":{"authors":[{"text":"Williams, Richard S. Jr.","contributorId":90679,"corporation":false,"usgs":true,"family":"Williams","given":"Richard S.","suffix":"Jr.","affiliations":[],"preferred":false,"id":499333,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121905,"text":"70121905 - 2004 - Dispersal forcing of a southern California river plumes, based on field and remote sensing observations","interactions":[],"lastModifiedDate":"2014-08-25T10:36:20","indexId":"70121905","displayToPublicDate":"2004-08-25T10:27:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Dispersal forcing of a southern California river plumes, based on field and remote sensing observations","docAbstract":"River plumes are important pathways of terrestrial materials entering the sea.  In southern California, rivers are known to be the dominant source of littoral, shelf and basin sediment and coastal pollution, although a basic understanding of the dynamics of these river inputs does not exist.  Here we evaluate forcing parameters of a southern California river plume using ship-based hydrographic surveys and satellite remote sensing measurements to provide the first insights of river dispersal dynamics in southern California.  Our results suggest that plumes of the Santa Clara River are strongly influenced by river inertia, producing jet-like structures ~10 km offshore during annual recurrence (~two-year) flood events and ~30 km during exceptional (~10-year recurrence) floods.  Upwelling-favorable winds may be strong following stormwater events and can alter dispersal pathways of thse plumes.  Due to similar runoff relationships and other reported satellite observations, we hypothesize that interia-dominated dispersal may be an important characteristic of the small, mountainous rivers throughout southern California.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s00367-003-0163-9","usgsCitation":"Warrick, J., Mertes, L.A., Washburn, L., and Siegel, D.A., 2004, Dispersal forcing of a southern California river plumes, based on field and remote sensing observations: Geo-Marine Letters, v. 24, no. 1, p. 46-52, https://doi.org/10.1007/s00367-003-0163-9.","productDescription":"7 p.","startPage":"46","endPage":"52","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292957,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292956,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00367-003-0163-9"}],"country":"United States","state":"California","otherGeospatial":"Santa Barbara Channel;Santa Clara River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.0,33.0 ], [ -121.0,35.0 ], [ -118.0,35.0 ], [ -118.0,33.0 ], [ -121.0,33.0 ] ] ] } } ] }","volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fc4dc9e4b0413fd75d6a80","contributors":{"authors":[{"text":"Warrick, Jonathan A. 0000-0002-0205-3814","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":48255,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan A.","affiliations":[],"preferred":false,"id":499315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mertes, Leal A.K.","contributorId":61761,"corporation":false,"usgs":true,"family":"Mertes","given":"Leal","email":"","middleInitial":"A.K.","affiliations":[],"preferred":false,"id":499316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Washburn, Libe","contributorId":96609,"corporation":false,"usgs":true,"family":"Washburn","given":"Libe","email":"","affiliations":[],"preferred":false,"id":499317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Siegel, David A.","contributorId":22264,"corporation":false,"usgs":true,"family":"Siegel","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":499314,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70121901,"text":"70121901 - 2004 - Estimating suspended sediment concentrations in turbid coastal waters of the Santa Barbara Channel with SeaWiFS","interactions":[],"lastModifiedDate":"2014-08-25T10:22:36","indexId":"70121901","displayToPublicDate":"2004-08-25T10:18:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Estimating suspended sediment concentrations in turbid coastal waters of the Santa Barbara Channel with SeaWiFS","docAbstract":"A technique is presented for estimating suspended sediment concentrations of turbid coastal waters with remotely sensed multi-spectral data. The method improves upon many standard techniques, since it incorporates analyses of multiple wavelength bands (four for Sea-viewing Wide Field of view Sensor (SeaWiFS)) and a nonlinear calibration, which produce highly accurate results (expected errors are approximately ±10%). Further, potential errors produced by erroneous atmospheric calibration in excessively turbid waters and influences of dissolved organic materials, chlorophyll pigments and atmospheric aerosols are limited by a dark pixel subtraction and removal of the violet to blue wavelength bands. Results are presented for the Santa Barbara Channel, California where suspended sediment concentrations ranged from 0–200+ mg l<sup>−1</sup> (±20 mg l<sup>−1</sup>) immediately after large river runoff events. The largest plumes were observed 10–30 km off the coast and occurred immediately following large El Niño winter floods.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","doi":"10.1080/01431160310001619535","usgsCitation":"Warrick, J., Mertes, L., Siegel, D., and Mackenzie, C., 2004, Estimating suspended sediment concentrations in turbid coastal waters of the Santa Barbara Channel with SeaWiFS: International Journal of Remote Sensing, v. 25, no. 10, p. 1995-2002, https://doi.org/10.1080/01431160310001619535.","productDescription":"8 p.","startPage":"1995","endPage":"2002","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292950,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/01431160310001619535"}],"country":"United States","state":"California","otherGeospatial":"Santa Barbara Channel","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.146119,34.094231 ], [ -120.146119,34.389398 ], [ -119.633881,34.389398 ], [ -119.633881,34.094231 ], [ -120.146119,34.094231 ] ] ] } } ] }","volume":"25","issue":"10","noUsgsAuthors":false,"publicationDate":"2010-06-02","publicationStatus":"PW","scienceBaseUri":"53fc4dcde4b0413fd75d6a98","contributors":{"authors":[{"text":"Warrick, J.A.","contributorId":53503,"corporation":false,"usgs":true,"family":"Warrick","given":"J.A.","affiliations":[],"preferred":false,"id":499308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mertes, L.A.K.","contributorId":50681,"corporation":false,"usgs":true,"family":"Mertes","given":"L.A.K.","affiliations":[],"preferred":false,"id":499307,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Siegel, D.A.","contributorId":70576,"corporation":false,"usgs":true,"family":"Siegel","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":499309,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mackenzie, C.","contributorId":42894,"corporation":false,"usgs":true,"family":"Mackenzie","given":"C.","email":"","affiliations":[],"preferred":false,"id":499306,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70121633,"text":"70121633 - 2004 - The mixed value of environmental regulations: do acroporid corals deserve endangered species status?","interactions":[],"lastModifiedDate":"2014-08-22T16:04:10","indexId":"70121633","displayToPublicDate":"2004-08-22T16:02:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"The mixed value of environmental regulations: do acroporid corals deserve endangered species status?","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Pollution Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.marpolbul.2004.07.007","usgsCitation":"Stinn, E., 2004, The mixed value of environmental regulations: do acroporid corals deserve endangered species status?: Marine Pollution Bulletin, v. 49, no. 7-8, p. 531-533, https://doi.org/10.1016/j.marpolbul.2004.07.007.","productDescription":"3 p.","startPage":"531","endPage":"533","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292914,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.marpolbul.2004.07.007"}],"volume":"49","issue":"7-8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f85994e4b03f038c5c1941","contributors":{"authors":[{"text":"Stinn, Eugene","contributorId":78654,"corporation":false,"usgs":true,"family":"Stinn","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":499240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121630,"text":"70121630 - 2004 - Sediment dynamics in the Adriatic Sea investigated with coupled models","interactions":[],"lastModifiedDate":"2018-04-09T13:23:22","indexId":"70121630","displayToPublicDate":"2004-08-22T15:52:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2929,"text":"Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Sediment dynamics in the Adriatic Sea investigated with coupled models","docAbstract":"Several large research programs focused on the Adriatic Sea in winter 2002-2003, making it an exciting place for sediment dynamics modelers (Figure 1). Investigations of atmospheric forcing and oceanic response (including wave generation and propagation, water-mass formation, stratification, and circulation), suspended material, bottom boundary layer dynamics, bottom sediment, and small-scale stratigraphy were performed by European and North American researchers participating in several projects. The goal of EuroSTRATAFORM researchers is to improve our ability to understand and simulate the physical processes that deliver sediment to the marine environment and generate stratigraphic signatures. Scientists involved in the Po and Apennine Sediment Transport and Accumulation (PASTA) experiment benefited from other major research programs including ACE (Adriatic Circulation Experiment), DOLCE VITA (Dynamics of Localized Currents and Eddy Variability in the Adriatic), EACE (the Croatian East Adriatic Circulation Experiment project), WISE (West Istria Experiment), and ADRICOSM (Italian nowcasting and forecasting) studies.","language":"English","publisher":"Oceanography Society","publisherLocation":"Washington, D.C.","doi":"10.5670/oceanog.2004.04","usgsCitation":"Sherwood, C.R., Book, J.W., Carniel, S., Cavaleri, L., Chiggiato, J., Das, H., Doyle, J.D., Harris, C.K., Niedoroda, A.W., Perkins, H., Poulain, P., Pullen, J., Reed, C.W., Russo, A., Sclavo, M., Signell, R.P., Traykovski, P.A., and Warner, J., 2004, Sediment dynamics in the Adriatic Sea investigated with coupled models: Oceanography, v. 17, no. 4, p. 58-69, https://doi.org/10.5670/oceanog.2004.04.","productDescription":"12 p.","startPage":"58","endPage":"69","costCenters":[{"id":183,"text":"Coastal and Marine Geology","active":false,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":478027,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5670/oceanog.2004.04","text":"Publisher Index Page"},{"id":292912,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Italy","otherGeospatial":"Adriatic Sea","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 12.24,39.61 ], [ 12.24,45.79 ], [ 20.02,45.79 ], [ 20.02,39.61 ], [ 12.24,39.61 ] ] ] } } ] }","volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f8598ae4b03f038c5c18f5","contributors":{"authors":[{"text":"Sherwood, Christopher R. 0000-0001-6135-3553 csherwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6135-3553","contributorId":2866,"corporation":false,"usgs":true,"family":"Sherwood","given":"Christopher","email":"csherwood@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Book, Jeffrey W.","contributorId":68209,"corporation":false,"usgs":true,"family":"Book","given":"Jeffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":499222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carniel, Sandro","contributorId":7636,"corporation":false,"usgs":true,"family":"Carniel","given":"Sandro","email":"","affiliations":[],"preferred":false,"id":499214,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cavaleri, Luigi","contributorId":69902,"corporation":false,"usgs":true,"family":"Cavaleri","given":"Luigi","email":"","affiliations":[],"preferred":false,"id":499224,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chiggiato, Jacopo","contributorId":13081,"corporation":false,"usgs":true,"family":"Chiggiato","given":"Jacopo","email":"","affiliations":[],"preferred":false,"id":499215,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Das, Himangshu","contributorId":24702,"corporation":false,"usgs":true,"family":"Das","given":"Himangshu","email":"","affiliations":[],"preferred":false,"id":499217,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Doyle, James D.","contributorId":54124,"corporation":false,"usgs":true,"family":"Doyle","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":499220,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Harris, Courtney K.","contributorId":19620,"corporation":false,"usgs":false,"family":"Harris","given":"Courtney","email":"","middleInitial":"K.","affiliations":[{"id":6708,"text":"Virginia Institute of Marine Science","active":true,"usgs":false}],"preferred":false,"id":499216,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Niedoroda, Alan W.","contributorId":40138,"corporation":false,"usgs":true,"family":"Niedoroda","given":"Alan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":499219,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Perkins, Henry","contributorId":61759,"corporation":false,"usgs":true,"family":"Perkins","given":"Henry","email":"","affiliations":[],"preferred":false,"id":499221,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Poulain, Pierre-Marie","contributorId":104825,"corporation":false,"usgs":true,"family":"Poulain","given":"Pierre-Marie","email":"","affiliations":[],"preferred":false,"id":499228,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Pullen, Julie","contributorId":103591,"corporation":false,"usgs":true,"family":"Pullen","given":"Julie","email":"","affiliations":[],"preferred":false,"id":499227,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Reed, Christopher W.","contributorId":75071,"corporation":false,"usgs":true,"family":"Reed","given":"Christopher","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":499225,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Russo, Aniello","contributorId":98234,"corporation":false,"usgs":true,"family":"Russo","given":"Aniello","email":"","affiliations":[],"preferred":false,"id":499226,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Sclavo, Mauro","contributorId":28910,"corporation":false,"usgs":true,"family":"Sclavo","given":"Mauro","email":"","affiliations":[],"preferred":false,"id":499218,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Signell, Richard P. rsignell@usgs.gov","contributorId":1435,"corporation":false,"usgs":true,"family":"Signell","given":"Richard","email":"rsignell@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":499211,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Traykovski, Peter A. 0000-0002-8163-6857","orcid":"https://orcid.org/0000-0002-8163-6857","contributorId":69487,"corporation":false,"usgs":false,"family":"Traykovski","given":"Peter","email":"","middleInitial":"A.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":499223,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":499212,"contributorType":{"id":1,"text":"Authors"},"rank":18}]}}
,{"id":70121604,"text":"70121604 - 2004 - A new protocol for surveying elkhorn and staghorn coral","interactions":[],"lastModifiedDate":"2014-08-22T15:15:02","indexId":"70121604","displayToPublicDate":"2004-08-22T15:11:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3241,"text":"Reef Encounters","active":true,"publicationSubtype":{"id":10}},"title":"A new protocol for surveying elkhorn and staghorn coral","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Reef Encounters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"International Society for Reef Studies","usgsCitation":"Rogers, C., Loomis, C., and Devine, B.E., 2004, A new protocol for surveying elkhorn and staghorn coral: Reef Encounters, v. 32, p. 49-51.","productDescription":"2 p.","startPage":"49","endPage":"51","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292907,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292906,"type":{"id":15,"text":"Index Page"},"url":"https://coralreefs.org/publications/reef-encounters/"}],"country":"United States","otherGeospatial":"Virgin Islands","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -65.0855,17.6739 ], [ -65.0855,18.4129 ], [ -64.5655,18.4129 ], [ -64.5655,17.6739 ], [ -65.0855,17.6739 ] ] ] } } ] }","volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f85943e4b03f038c5c1747","contributors":{"authors":[{"text":"Rogers, Caroline 0000-0001-9056-6961","orcid":"https://orcid.org/0000-0001-9056-6961","contributorId":102406,"corporation":false,"usgs":true,"family":"Rogers","given":"Caroline","affiliations":[],"preferred":false,"id":499197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loomis, Christy","contributorId":83452,"corporation":false,"usgs":true,"family":"Loomis","given":"Christy","email":"","affiliations":[],"preferred":false,"id":499196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Devine, Barry E.","contributorId":11136,"corporation":false,"usgs":true,"family":"Devine","given":"Barry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":499195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}