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|Created:||Jun 28, 2018 at 3:12 p.m.|
|Last updated:|| Jun 29, 2018 at 4:48 p.m.
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The Corps Water Management System (CWMS) includes four interrelated models to assist with water management for the basin:
- GeoHMS (Geospatial Hydrologic Modeling Extension)
- ResSIM (Reservoir System Simulation)
- RAS (River Analysis System)
- FIA (Flood Impact Analysis)
The White River Basin contains 27,818 square miles: about 38 percent is in Missouri and 62 percent is in Arkansas. The fan-shaped basin is about 250 miles long in a northerly direction and varies in width from 210 miles near the Missouri-Arkansas State line to about 50 miles near the mouth of the river. Approximately three-fourths of the basin is in the Ozark highlands where the topography consists of rough dissected plateaus rugged hills, and rolling woodland. The eastern escarpment of the Ozark Mountains extends southwestward across the basin from the vicinity of Poplar Bluff, MO; along the west side of the Black River to Batesville, AR, on the White River; and thence to the vicinity of Searcy, AR, in the little Red River Basin. East of the escarpment, the basin lies in the flat terrain of the Gulf Coastal Plain. The eastern watershed divide between the White and St. Francis Rivers is formed by Crowley’s’ Ridge, which extends in a north-south direction and rises about 150 feet above the floodplain.
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|USACE CWMS - White River Watershed Centerline||Resource||Jessie Myers||Discoverable||Open Access|
|USACE CWMS - White River Watershed Conversion Points||Resource||Jessie Myers||Discoverable||Open Access|
|USACE CWMS - White River Watershed||Resource||Jessie Myers||Discoverable||Open Access|
|USACE CWMS - White River Watershed Study Area||Resource||Jessie Myers||Discoverable||Open Access|
|USACE CWMS - White River Watershed Bank Lines||Resource||Jessie Myers||Discoverable||Open Access|
|USACE Model Registry||Point of contact: USACEModelRegistryAdmin@usace.army.mil|
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This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/
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