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DS-777 Spatial Location of Gages with Total Flow and estimated Base Flow, organized by Seasonal Stress Periods for the Development Simulation Period for the Northern High Plains Groundwater-Flow Model in Parts of Colorado, Kansas, Nebraska, South Dakota, and Wyoming
Baseflow is the portion of streamflow derived from groundwater flow. It is an
important component of the groundwater budget, and can be estimated using
known total streamflow at given points through time. Daily streamflow data was
collected from 91 streamflow gaging stations across the northern High Plains
Groundwater Availability Study (NHPGAS) area from the National Water
Information System (NWIS) and the Nebraska Department of Natural Resources
Stream Gaging Data Bank. The data from each site was processed using the BFI
program, version 4.15 (Wahl and Wahl, 2007) to determine the baseflow component
of total streamflow at each site. The average daily baseflow was computed for the
months of April and October, spanning the development period model (1940-2009).
The resulting baseflow values were applied as calibration targets to corresponding
stress periods.
Complete Metadata
| accessLevel | public |
|---|---|
| bureauCode |
[
"010:12"
]
|
| contactPoint |
{
"fn": "Oklahoma-Texas Water Science Center",
"@type": "vcard:Contact",
"hasEmail": "mailto:gs-w-txpublic-info@usgs.gov"
}
|
| description | Baseflow is the portion of streamflow derived from groundwater flow. It is an important component of the groundwater budget, and can be estimated using known total streamflow at given points through time. Daily streamflow data was collected from 91 streamflow gaging stations across the northern High Plains Groundwater Availability Study (NHPGAS) area from the National Water Information System (NWIS) and the Nebraska Department of Natural Resources Stream Gaging Data Bank. The data from each site was processed using the BFI program, version 4.15 (Wahl and Wahl, 2007) to determine the baseflow component of total streamflow at each site. The average daily baseflow was computed for the months of April and October, spanning the development period model (1940-2009). The resulting baseflow values were applied as calibration targets to corresponding stress periods. |
| distribution |
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|
| identifier | http://datainventory.doi.gov/id/dataset/USGS_417b1f5d-2b47-4f81-a7d5-896cb6ab6234 |
| keyword |
[
"Big Blue River",
"Calamus River",
"Cedar River",
"Dismal River",
"Elkhorn River",
"Frenchman Creek",
"Kansas",
"Lodgepole Creek",
"Loup River",
"Middle Loup River",
"Nebraska",
"Niobrara River",
"North Loup River",
"North Platte River",
"Northern High Plains",
"Platte River",
"Republican River",
"South Dakota",
"South Loup River",
"USGS:417b1f5d-2b47-4f81-a7d5-896cb6ab6234",
"baseflow",
"environment",
"geohydrology",
"geoscientificInformation",
"groundwater",
"groundwater availability",
"hydrologic models",
"inlandWaters",
"surface-groundwater relations"
]
|
| modified | 2020-11-17T00:00:00Z |
| publisher |
{
"name": "U.S. Geological Survey",
"@type": "org:Organization"
}
|
| spatial | -104.130448, 38.896863, -96.275457, 43.415946 |
| theme |
[
"Geospatial"
]
|
| title | DS-777 Spatial Location of Gages with Total Flow and estimated Base Flow, organized by Seasonal Stress Periods for the Development Simulation Period for the Northern High Plains Groundwater-Flow Model in Parts of Colorado, Kansas, Nebraska, South Dakota, and Wyoming |