Article ID Journal Published Year Pages File Type
4450661 Atmospheric Research 2010 7 Pages PDF
Abstract

Data suggest that the arrival of winter's permanent snowpack impacts daily high and low surface temperatures in Fairbanks, Alaska. Given temperatures at 850 hPa ranging from 0 °C to − 5 °C in October, high temperatures on days with snow on the ground are 4.9 °C colder than high temperatures on days with no snow on the ground. The difference for low temperatures is 7.3 °C. While the exact date the snowpack is established varies from year to year, standardizing this date in time as “S-Day” reveals that the drop in daily high and low temperatures through the period from 5 days before S-Day to 5 days after S-Day is from 5 to 7 °C greater than the gradual cooling associated with the change of seasons from fall to winter.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Atmospheric Science
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