AndreaBozzo/ceres-open-data-index huggingface dataset:
Model climate scenario output for the Blackstone, Pawcatuck, and Ipswich river basins, Massachusetts, 2036-2065 change from 1975-2004, Representative Concentration Pathways 4.5 and 8.5

This data release provides a set of Hydrological Simulation Program--Fortran (HSPF) model files representing 5 EPA-selected future climate change scenarios for each of three river basins: Blackstone in Massachusetts and Rhode Island, Pawcatuck in Rhode Island, and Ispwich in Massachusetts. Output from these models are intended for use as input to EPA Watershed Management Optimization Support Tool (WMOST) modeling. Climate scenarios, based on 2036-2065 change from 1975-2004 Representative Concentration Pathways (RCP) 4.5 and 8.5, model effects of air temperature and precipitation changes (in degrees F for air temperature, in percent for precipitation) made to the input historical meteorological time series 1975-2004. Blackstone meteorological data are from T.F. Green Airport (Providence) and Worcester Regional Airport (Worcester), Pawcatuck meteorological data are from T.F. Green Airport (Providence), and Ipswich meteorological data are from 30 local National Weather Service Stations (1975-1995) and Boston Logan Airport (1996-2004). Each set of climate scenario model files are derived from the original calibrated model files developed to support WMOST modeling (refer to Source Input fields in this metadata file).

Tags: blackstone, climate-change, hydrology, ipswich, pawcatuck-river, usgs-5840b08ae4b04fc80e47435b
Organization: Department of the Interior
Model Input and Output of the flood-inundation maps for the St. Joseph River at Elkhart, Indiana

Digital flood-inundation maps for a 6.6-mile reach of the St. Joseph River at Elkhart, Indiana were created by the U.S. Geological Survey (USGS) in cooperation with the Indiana Office of Community and Rural Affairs. The flood-inundation maps, which can be accessed through the USGS Flood Inundation Mapping Science Web site at http://water.usgs.gov/osw/flood_inundation/, depict estimates of the areal extent and depth of flooding corresponding to selected water levels (stages) at the USGS streamgage 04101000, St. Joseph River at Elkhart, Ind. Near-real-time stages at this streamgage may be obtained on the Internet from the USGS National Water Information System at http://waterdata.usgs.gov/ or the National Weather Service (NWS) Advanced Hydrologic Prediction Service at http:/water.weather.gov/ahps/, which also forecasts flood hydrographs at this site (NWS site EKMI3). Flood profiles were computed for the USGS streamgage 04101000, St. Joseph River at Elkhart, Ind., reach by means of a one-dimensional step-backwater hydraulic modeling software developed by the U.S. Army Corps of Engineers. The hydraulic model was calibrated using the current stage-discharge rating at the USGS streamgage 04101000, St. Joseph River at Elkhart, Ind. The hydraulic model was then used to compute 6 water-surface profiles for flood stages at 1-foot (ft) intervals referenced to the streamgage datum ranging from 23.0 ft (the NWS “action stage”) to 28.0 ft, which is the highest stage interval of the current USGS stage-discharge rating curve and 1 ft higher than the NWS “major flood stage.” The simulated water-surface profiles were then combined with a Geographic Information System digital elevation model (derived from light detection and ranging [lidar]) data having a 0.49-ft root mean squared error and 4.9-ft horizontal resolution) to delineate the area flooded at each stage. The availability of these maps, along with Internet information regarding current stage from the USGS streamgage and forecasted high-flow stages from the NWS, will provide emergency management personnel and residents with information that is critical for flood response activities such as evacuations and road closures, as well as for post-flood recovery efforts.

Tags: city-of-elkhart, elkhart, flood-inundation-maps, floodplain, floodplains, floods, geospatial-analysis, geospatial-datasets, high-water-marks, hydraulic-engineering, hydrology, indiana, inlandwaters, maps-and-atlases, river, st-joseph-river, stream, streamflow, united-states, usgs-584197dfe4b04fc80e518b6b
Organization: Department of the Interior
Inorganic and organic concentration data collected from 38 streams in the United States, 2012-2014, with supporting data, as part of the Chemical Mixtures and Environmental Effects Pilot Study.

This USGS data release contains station and laboratory method information and geospatial information, as well as concentration results for inorganic and organic compounds and bioluminescent yeast estrogen screen and transgenic zebrafish embryo estrogren bioassay, analyzed at 38 sites in 25 states as part of the Chemical Mixtures and Environmental Effects Pilot Study, 2012-2014.

Tags: chemical-mixtures, ecological-exposures, estrogen-bioassay, estrogen-screen, laboratory, laboratory-methods, landscape-metrics, station-information, stream-channels, streams, united-states, usgs-5841a2ace4b04fc80e518ba8
Organization: Department of the Interior
Conservation Planning for the Colorado River in Utah - Distance to Water for Open Land Species Model

This maps shows distances away from the channel boundary of the Colorado River mainstem.  The channel boundary was mapped from public available NAIP imagery flown on June 28, 2011, when the river flow was 886 m3/s at the Cisco gage.  The channel is subdivided into channel types: main channel, secondary channel, backwater, isolated pool and tributary channel.
Closer to the channel often non-preferred habitat for burrowing; 50-100 m is moderately non-preferred; &gt;100 m preferred.

Tags: arches-national-park, biota, canyonlands-national-park, colorado-river, conservation-planning, environment, grand-county, habitat-suitability, inlandwaters, moab, riparian, san-juan-county, tamarisk, upper-colorado-river, usgs-5866d76be4b0cd2dabe7c694, utah
Organization: Department of the Interior
Dataset for Alaska Marine Fish Ecology Catalog

This collection of GIS layers was prepared for the report Alaska Arctic Marine Fish Ecology Catalog (U.S. Geological Survey Scientific Investigations Report 2016–5038). The layers display geographic distribution and sampling locations for Arctic marine fish species in the region of United States sectors of the Chukchi and Beaufort Seas. Certain diadromous species (for example, Pacific salmon, char, and whitefishes) are treated as marine fishes (McDowall, 1987) because much of their life cycle is in marine and brackish environments. This synthesis of information is meant to provide current information and understanding of this fauna and its relative vulnerability to changing Arctic conditions.
There are 104 species in the collection - some species have both polygon and point data layers. The report (SIR 2016-5038) also describes for each species its names - species, common, and colloquial; ecological role; physical description/attributes; range (geographic); relative abundance; depth range; habitats and life history; behavior; populations or stocks, reproduction, food and feeding, biological interactions, resilience, traditional and cultural importance, commercial fisheries, potential effects of climate change, areas for future research, cited references, and bibliography.  
The published report has one map for each species showing the polygon and point data as well as land and relevant administrative boundaries. Although some of the species also have an inland water presence, this report was concerned only with their marine conditions; therefore, the land component (from the original sources) has been clipped and removed. The distribution areas may be greater in extent than that shown in the report map bounding box limits. Distributions of marine fishes are shown in adjacent Arctic seas where reliable data are available. The report can be accessed at: https://doi.org/10.3133/sir20165038
This metadata document describes the collection of species data layers. Each species layer file will have its own metadata with details specific to that layer.

Tags: alaska, arctic, beaufort-sea, bering-sea, bering-strait, biogeography, chukchi-beaufort-lease-area, chukchi-sea, distributions, ecology, fish, marine, marine-fishery-resources, northeast-russia, northwest-canada, northwest-territories, nunavut, u-s-exclusive-economic-zone, usgs-5841a424e4b04fc80e518bb5, yukon
Organization: Department of the Interior
Transient electromagnetic (TEM) sounding data; San Luis Valley, Colorado, 2009

Transient electromagnetic (TEM) soundings were made in the San Luis Valley, Colorado, to map the location of a blue clay unit as well as to investigate the presence of suspected faults. A total of 147 soundings were made near and in Great Sand Dunes National Park and Preserve, and an additional 6 soundings were made near Hansen Bluff on the eastern edge of the Alamosa National Wildlife Refuge. The blue clay is a significant hydrologic feature in the area that separates an unconfined surface aquifer from a deeper confined aquifer. Knowledge of its location is important to regional hydrological models. Previous analysis of well logs has shown that the blue clay has a resistivity of 10 ohm-meters or less, which is in contrast to the higher resistivity of sand, gravel, and other clay units found in the area, making it a very good target for TEM soundings. The top of the blue clay was found to have considerable relief suggesting the possibility of deformation of the clay during or after deposition. Because of rift activity deformation is to be expected. Of the TEM profiles made across faults identified by aeromagnetic data, some showed resistivity variations and (or) subsurface elevation relief of resistivity units suggestive of faulting. Such patterns were not associated with all suspected faults. The Hansen Bluff profile showed variations in resistivity and depth to conductor that coincide with a scarp between the highlands to the east and the floodplain of the Rio Grande River to the west.

Tags: alamosa-county, alamosa-national-wildlife-refuge, aquifer, clay, clay-deposits, colorado, electromagnetic-surveying, fault-detection, faulting-geologic, geophysics, geoscientificinformation, great-sand-dunes-national-park, great-sand-dunes-national-preserve, groundwater, saguache-county, san-luis-valley, subsurface-mapping, subsurface-maps, tem, transient-electromagnetic-sounding, usgs-5841bc9fe4b04fc80e518c66
Organization: Department of the Interior
Transient electromagnetic (TEM) sounding data; San Luis Valley, Colorado, 2007

Transient electromagnetic (TEM) soundings were made in the San Luis Valley, Colorado, to map the location of a blue clay unit as well as to investigate the presence of suspected faults. A total of 147 soundings were made near and in Great Sand Dunes National Park and Preserve, an additional 6 soundings were made near Hansen Bluff on the eastern edge of the Alamosa National Wildlife Refuge. The blue clay is a significant hydrologic feature in the area that separates an unconfined surface aquifer from a deeper confined aquifer. Knowledge of its location is important to regional hydrological models. Previous analysis of well logs has shown that the blue clay has a resistivity of 10 ohm-meters or less, which is in contrast to the higher resistivity of sand, gravel, and other clay units found in the area, making it a very good target for TEM soundings. The top of the blue clay was found to have considerable relief suggesting the possibility of deformation of the clay during or after deposition. Because of rift activity deformation is to be expected. Of the TEM profiles made across faults identified by aeromagnetic data, some showed resistivity variations and (or) subsurface elevation relief of resistivity units suggestive of faulting. Such patterns were not associated with all suspected faults. The Hansen Bluff profile showed variations in resistivity and depth to conductor that coincide with a scarp between the highlands to the east and the floodplain of the Rio Grande River to the west.

Tags: alamosa-county, alamosa-national-wildlife-refuge, aquifer, clay, clay-deposits, colorado, electromagnetic-surveying, fault-detection, faulting-geologic, geophysics, geoscientificinformation, great-sand-dunes-national-park, great-sand-dunes-national-preserve, groundwater, saguache-county, san-luis-valley, subsurface-mapping, subsurface-maps, tem, transient-electromagnetic-sounding, usgs-5841c009e4b04fc80e518c89
Organization: Department of the Interior
Transient electromagnetic (TEM) sounding data; San Luis Valley, Colorado, 2007

Transient electromagnetic (TEM) soundings were made in the San Luis Valley, Colorado, to map the location of a blue clay unit as well as to investigate the presence of suspected faults. A total of 147 soundings were made near and in Great Sand Dunes National Park and Preserve, an additional 6 soundings were made near Hansen Bluff on the eastern edge of the Alamosa National Wildlife Refuge. The blue clay is a significant hydrologic feature in the area that separates an unconfined surface aquifer from a deeper confined aquifer. Knowledge of its location is important to regional hydrological models. Previous analysis of well logs has shown that the blue clay has a resistivity of 10 ohm-meters or less, which is in contrast to the higher resistivity of sand, gravel, and other clay units found in the area, making it a very good target for TEM soundings. The top of the blue clay was found to have considerable relief suggesting the possibility of deformation of the clay during or after deposition. Because of rift activity deformation is to be expected. Of the TEM profiles made across faults identified by aeromagnetic data, some showed resistivity variations and (or) subsurface elevation relief of resistivity units suggestive of faulting. Such patterns were not associated with all suspected faults. The Hansen Bluff profile showed variations in resistivity and depth to conductor that coincide with a scarp between the highlands to the east and the floodplain of the Rio Grande River to the west.

Tags: alamosa-county, alamosa-national-wildlife-refuge, aquifer, clay, clay-deposits, colorado, electromagnetic-surveying, fault-detection, faulting-geologic, geophysics, geoscientificinformation, great-sand-dunes-national-park, great-sand-dunes-national-preserve, groundwater, saguache-county, san-luis-valley, subsurface-mapping, subsurface-maps, tem, transient-electromagnetic-sounding, usgs-5841ca6ae4b04fc80e518cab
Organization: Department of the Interior
Transient electromagnetic (TEM) sounding data; San Luis Valley, Colorado, 2007

Transient electromagnetic (TEM) soundings were made in the San Luis Valley, Colorado, to map the location of a blue clay unit as well as to investigate the presence of suspected faults. A total of 147 soundings were made near and in Great Sand Dunes National Park and Preserve, an additional 6 soundings were made near Hansen Bluff on the eastern edge of the Alamosa National Wildlife Refuge. The blue clay is a significant hydrologic feature in the area that separates an unconfined surface aquifer from a deeper confined aquifer. Knowledge of its location is important to regional hydrological models. Previous analysis of well logs has shown that the blue clay has a resistivity of 10 ohm-meters or less, which is in contrast to the higher resistivity of sand, gravel, and other clay units found in the area, making it a very good target for TEM soundings. The top of the blue clay was found to have considerable relief suggesting the possibility of deformation of the clay during or after deposition. Because of rift activity deformation is to be expected. Of the TEM profiles made across faults identified by aeromagnetic data, some showed resistivity variations and (or) subsurface elevation relief of resistivity units suggestive of faulting. Such patterns were not associated with all suspected faults. The Hansen Bluff profile showed variations in resistivity and depth to conductor that coincide with a scarp between the highlands to the east and the floodplain of the Rio Grande River to the west.

Tags: alamosa-county, alamosa-national-wildlife-refuge, aquifer, clay, clay-deposits, colorado, electromagnetic-surveying, fault-detection, faulting-geologic, geophysics, geoscientificinformation, great-sand-dunes-national-park, great-sand-dunes-national-preserve, groundwater, saguache-county, san-luis-valley, subsurface-mapping, subsurface-maps, tem, transient-electromagnetic-sounding, usgs-5841caa4e4b04fc80e518cad
Organization: Department of the Interior
Stratigraphic, geochemical, and hydrologic data for the Boston Peak wetland, Larimer County, CO, USA

Comprehensive sampling of peat, underlying lakebed sediments, and coexisting waters of a naturally uraniferous montane wetland are combined with hydrologic measurements to define the important controls on uranium (U) supply and uptake. The major source of U to the wetland is groundwater flowing through locally fractured and faulted granite gneiss of Proterozoic age. Dissolved U concentrations in four springs and one seep ranged from 20 to 83 ppb (µg/l). Maximum U concentrations are ~300 ppm (mg/kg) in lakebed sediments and &gt;3000 ppm in peat. This study documents the conditions and processes controlling the efficient uptake of U in a relatively remote, natural wetland that is absent of reported U occurrences, mining impacts, or other obvious sources of pollution. Unlike previous studies of U-rich wetlands, this study is distinguished because it provides an exceptionally detailed three-dimensional view of the distribution of uranium in as much as 3.7 m of Holocene peat, underlain by organic-rich lacustrine silt and clay (gyttja) and organic-poor clay and silt of a precursor post-glacial lake, with a combined thickness of as much as 8.5 m. The hydrologic characteristics of the entire sedimentary package from surface to bedrock were investigated with an extensive array of installed piezometers and water-table monitoring wells. Mechanisms of U uptake were investigated by a variety of techniques that utilize analyses of waters and of core and auger samples collected from depths as great as 11 m.

Tags: boston-peak, colorado, geochemistry, groundwater-hydrology, laramie-river-valley, larimer-county, uranium, usgs-5841cfeae4b04fc80e518ccf, wetland
Organization: Department of the Interior
Magnetotelluric sounding data, station 26, San Luis Valley, Colorado, 2007

This dataset includes the magnetotelluric (MT) sounding data collected in 2007 in and near the San Luis Valley, Colorado. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Valley to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Valley region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's groundwater resources.

Tags: apparent-resistivity, aquifer, cggsc, colorado, crustal-geophysics-and-geochemistry-science-center, electromagnetic-surveying, geophysics, geoscientificinformation, gps-measurement, groundwater, hydrogeology, impedance, impedance-phase, impedance-strike, magnetic-field-earth, magnetic-surveying, magnetotelluric, mineral-resources-program, mrp, mt, rocky-mountains, saguache-county, san-luis-valley, sounding, tipper, usgs-5841d6a0e4b04fc80e518cea
Organization: Department of the Interior
Magnetotelluric sounding data, station 27, San Luis Valley, Colorado, 2007

This dataset includes the magnetotelluric (MT) sounding data collected in 2007 in and near the San Luis Valley, Colorado. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Valley to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Valley region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's groundwater resources.

Tags: apparent-resistivity, aquifer, cggsc, colorado, crustal-geophysics-and-geochemistry-science-center, electromagnetic-surveying, geophysics, geoscientificinformation, gps-measurement, groundwater, hydrogeology, impedance, impedance-phase, impedance-strike, magnetic-field-earth, magnetic-surveying, magnetotelluric, mineral-resources-program, mrp, mt, rocky-mountains, saguache-county, san-luis-valley, sounding, tipper, usgs-5841d8fce4b04fc80e518cef
Organization: Department of the Interior
Magnetotelluric sounding data, station 28, San Luis Valley, Colorado, 2007

This dataset includes the magnetotelluric (MT) sounding data collected in 2007 in and near the San Luis Valley, Colorado. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Valley to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Valley region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's groundwater resources.

Tags: alamosa-county, apparent-resistivity, aquifer, cggsc, colorado, crustal-geophysics-and-geochemistry-science-center, electromagnetic-surveying, geophysics, geoscientificinformation, gps-measurement, groundwater, hydrogeology, impedance, impedance-phase, impedance-strike, magnetic-field-earth, magnetic-surveying, magnetotelluric, mineral-resources-program, mrp, mt, rocky-mountains, san-luis-valley, sounding, tipper, usgs-5841da8fe4b04fc80e518cf2
Organization: Department of the Interior
Magnetotelluric sounding data, station 29, San Luis Valley, Colorado, 2007

This dataset includes the magnetotelluric (MT) sounding data collected in 2007 in and near the San Luis Valley, Colorado. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Valley to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Valley region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's groundwater resources.

Tags: apparent-resistivity, aquifer, cggsc, colorado, crustal-geophysics-and-geochemistry-science-center, electromagnetic-surveying, geophysics, geoscientificinformation, gps-measurement, groundwater, hydrogeology, impedance, impedance-phase, impedance-strike, magnetic-field-earth, magnetic-surveying, magnetotelluric, mineral-resources-program, mrp, mt, rocky-mountains, saguache-county, san-luis-valley, sounding, tipper, usgs-5841df36e4b04fc80e518cf5
Organization: Department of the Interior