Over a mere four days this summer, snow from the previous winter melted into a pond of slush on Canada’s Lowell Glacier. Mauri Pelto, a glaciologist at Nichols College, called the area of water-saturated snow a “snow swamp.”
The false-color image above shows the progression of the rapid snow melt in the Kluane National Park in the Yukon Territory. The image was acquired on July 26, 2018, by the Operational Land Imager (OLI) on the Landsat 8 satellite (bands 6-5-4).
In the image, short wavelength infrared (SWIR) bands are combined to better differentiate areas of water that are frozen (light blue) from those that contain significant meltwater (dark blue). Rocks are brown; vegetation is green. On July 26, the slush covered an area of more than 25 square miles (40 square kilometers).
Pelto has seen similar puddles of slush on other glaciers, but the rapid development of such a large melt area on Lowell Glacier is unusual. “The only way to generate such an extensive snow swamp is to have the snow saturated with water all the way to the surface,” he said.
High temperatures caused the extensive ablation event—the loss of surface ice due to melting—according to Pelto. During those four days, daily temperatures at nearby Haines Junction (approximately 40 miles/60 kilometers northeast of the glacier) reached 84 degrees Fahrenheit (29 degrees Celsius)—higher than normal for the region in July.
The slushy pool disappeared quickly as the snowpack melted. By August 11, the slush was lost from the glacier system, flowing into Lowell Lake at the end of the glacier. Pelto said such a large loss of water should drive the glacier to retreat more.
Image and Story Credit: NASA/Joshua Stevens/USGS/European Space Agency/Kasha Patel
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