Showing posts with label SNOTEL. Show all posts
Showing posts with label SNOTEL. Show all posts

Sunday, February 17, 2013

Average year (so far) for Snow in Glacier National Park

According to the latest data published by the Flattop Mountain SNOTEL (SNOw TELemetry) station, the amount of snow in Glacier National Park is right at the 40-year average for mid-February. As of February 15th, the SNOTEL is measuring a total of 34.8 inches of Snow Water Equivalent (SWE), which is the weight of snow water equivalent to inches of water.

The Flattop Mountain SNOTEL station is located at an elevation of approximately 6300 feet on Flattop Mountain, which is a high plateau between the Lewis and Livingston Ranges in Glacier National Park. According to the website, "Flattop Mountain is a useful indicator of snowfall throughout Glacier National Park because it is subject to the factors that influence conditions elsewhere in the park".

Data from the Flattop Mountain SNOTEL is compiled by water year, which runs from October 1st through September 30th.

The following is a graph that compares SWE for 2013 versus the average and other significant water years (you can click here for a larger version):




Jeff
Hiking in Glacier National Park

Thursday, March 22, 2012

Snowpack in Glacier finally reaches 41-year average

The SNOTEL (SNOw TELemetry) station on Flattop Mountain is reporting that snowpack in Glacier National Park has finally reached it's long-term average. Up until the beginning of March snowpack has been below average. There is currently 42.5 inches of water-equivalent snow on Flattop Mountain.

The Flattop Mountain SNOTEL station is one of nearly 600 similar stations operated throughout the western United States by the Natural Resources Conservations Service under the U.S. Department of Agriculture. These stations measure and record Snow Water Equivalent, which is the weight of snow water equivalent to inches of water.

The Flattop Mountain SNOTEL station is located at approximately 6300 feet in elevation, on a high plateau between the Lewis and Livingston Ranges in Glacier National Park. Flattop Mountain is a useful indicator of snowfall throughout Glacier National Park because it is subject to the factors that influence conditions elsewhere in the park.

Below is a graph comparing snow water equivalent for 2012 versus other significant water years and the 41-year average:





Jeff
Hiking in Glacier.com