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Preparing lake level chart... The Drought Monitor focuses on broad-scale conditions. Local conditions may vary. See accompanying text summary for forecast statements.
Water volume and surface area of the Great Salt Lake between 1984 and today. Click or tap the "Play" button to see a timelapse video. Recent data show a downward trend in water levels, and we expect this trend to continue.
Monitoring location 10010000 is associated with a Lake, Reservoir, Impoundment in Salt Lake County, Utah. Current conditions of Lake or reservoir water surface elevation above NGVD 1929 are available. Water data back to 1847 are available online.
The Great Salt Lake’s water level is influenced by precipitation, temperature, evaporation and runoff. It is a terminal basin, meaning it has no outlet, and once water arrives in the lake, it stays until it evaporates.
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The Great Salt Lake's levels have fallen to lows akin to 2021, raising some concerns about its current state. Record temperatures and drought conditions contributed to the lake's decline this summer.
Below are data specific to the north arm of Great Salt Lake, presented by water year. A water year starts Oct. 1 of each year, offering a more accurate representation of water resource management. The default plot shows the current water year with a line indicating the median value (1966-present).
Monitoring location 10010100 is associated with a Lake, Reservoir, Impoundment in Box Elder County, Utah. Current conditions of Lake or reservoir water surface elevation above NGVD 1929 are available. Water data back to 1966 are available online.
Lake levels for the southern and northern arms of the lake and discharge for locations on major surface water inflows are included. Interactive map that provides real-time stream, lake and reservoir, and groundwater data for USGS observation stations.
Water levels averaged 4,193.4 in the south arm and 4,190.8 in the north arm. As of Sept. 30, the end of the water year, the south half of the Great Salt Lake sits at 4,192.5 feet and the north...