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Figure : end-of-season-snow-water-equivalent-depth-at-lewis-lake-divide
End of Season Snow Water Equivalent Depth at Lewis Lake Divide
Figure 50.5Cooperative Institute for Climate and Satellites - NC
Kenneth E. Kunkel
Variations in the April 1 snow water equivalent at the Lewis Lake Divide, Wyoming SNOTEL site. Snow water equivalent (SWE) is the amount of water contained within the snowpack. SWE varies widely from year to year. In 2011, the SWE was almost double the long-term average at the end of May. The melting and runoff of this above-normal snowpack in May and June 2011 caused flooding downstream along the Snake River in Idaho. Source: SNOTEL.
Free to use with credit to the original figure source.
The time range for this figure is March 01, 1981 (00:00 AM) to May 01, 2015 (00:00 AM).
This figure was created on May 21, 2015.
The spatial range for this figure is 40.9946° to 45.0060° latitude, and -104.0518° to -111.0563° longitude.
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