Major Flood
28 ft
Located in Tunica County, Mississippi on the Coldwater River. Live water level data from USGS gauge 07279700, updated every 15 minutes.
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Flood stages defined by the National Weather Service. Gage height data from USGS Water Resources.
28 ft
24 ft
18 ft
17 ft
Flood waters overtop the levee system on the right bank. Evacuations become necessary.
Roads east of the river between the river and the railroad tracks are flooded and may be impassable.
Many homes and roads are flooding.
Flooding is occurring on the left bank. Mainly agricultural land is flooded. The levee system protects the right bank from flooding.
Farmland flooding is widespread.
Low-lying farmland near the river begins to flood.
Impact statements from the National Weather Service, describing what typically happens at each water level.
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| Date | Stage | Flow |
|---|---|---|
| Apr 19, 1973 | 25 ft | — |
| Dec 19, 2002 | 23.92 ft | — |
| May 17, 2003 | 23.55 ft | 14,398 cfs |
SARM6
Coldwater River
Tunica, MS
34.5756°N, 90.2244°W
StormCast monitors this gauge and sends a push notification to your phone when the water level crosses into a new flood category — even at 3 AM.
The Coldwater River near Sarah gauge is maintained by USGS (site 07279700) and reports water levels every 15 minutes. Visit this page to see the latest reading updated live, or download StormCast to get push alerts when levels rise.
The NWS-defined flood stage for Coldwater River near Sarah is 18 feet. Action stage begins at 17 feet. Moderate flooding starts at 24 feet, and major flooding at 28 feet.
Download StormCast free on Google Play, go to River Gauges, and add Coldwater River near Sarah to your watchlist. StormCast will send a push notification to your phone whenever the water level crosses into a new NWS flood category.
The gauge is located in Tunica County, Mississippi at coordinates 34.5756°N, 90.2244°W. USGS site number: 07279700. Data is provided by the U.S. Geological Survey and the National Weather Service.
Data provided by: US Army Corps of Engineers, Observations courtesy of U.S. Geological Survey, Observations courtesy of U.S. Army Corps of Engineers