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Warmer Springs Causing Loss of Snow Cover throughout the Rocky Mountains
Released: 5/13/2013 2:00:00 PM
Contact Information:
U.S. Department of the Interior, U.S. Geological Survey
Office of Communications and Publishing
12201 Sunrise Valley Dr, MS 119
Reston, VA 20192
Greg Pederson http://www.usgs.gov/newsroom/[email protected]&n=Greg+Pederson
Phone: 406-994-7390
Paul Laustsen http://www.usgs.gov/newsroom/[email protected]&n=Paul++Laustsen
Phone: 650-329-4046
In partnership with: American Geophysical Union
The new study has teased apart and quantified the different influences of winter temperature, spring temperature, and precipitation on historic snowpack variations and trends in the region. To distinguish those varying influences, the researchers implemented a regional snow model that uses inputs of monthly temperature and precipitation data from 1895 to 2011.
"Each year we looked at temperature and precipitation variations and the amount of water contained within the snowpack as of April," said USGS scientist Greg Pederson, the lead author of the study. "Snow deficits were consistent throughout the Rockies due to the lack of precipitation during the cool seasons during the 1930s coinciding with the Dust Bowl era. From 1980 on, warmer spring temperatures melted snowpack throughout the Rockies early, regardless of winter precipitation. The model in turn shows temperature as the major driving factor in snowpack declines over the past thirty years."
Runoff from Rocky Mountain winter snowpack accounts for 60 to 80 percent of the annual water supply for more than 70 million people living in the western U.S., and is influenced by factors such as the snowpacks water content, known as snow water equivalent, and the timing of snowmelt
The study, "Regional patterns and proximal causes of the recent snowpack decline in the Rocky Mountains," is available from Geophysical Research Letters, a journal of the American Geophysical Union.
Released: 5/13/2013 2:00:00 PM
Contact Information:
U.S. Department of the Interior, U.S. Geological Survey
Office of Communications and Publishing
12201 Sunrise Valley Dr, MS 119
Reston, VA 20192
Greg Pederson http://www.usgs.gov/newsroom/[email protected]&n=Greg+Pederson
Phone: 406-994-7390
Paul Laustsen http://www.usgs.gov/newsroom/[email protected]&n=Paul++Laustsen
Phone: 650-329-4046
In partnership with: American Geophysical Union
The new study has teased apart and quantified the different influences of winter temperature, spring temperature, and precipitation on historic snowpack variations and trends in the region. To distinguish those varying influences, the researchers implemented a regional snow model that uses inputs of monthly temperature and precipitation data from 1895 to 2011.
"Each year we looked at temperature and precipitation variations and the amount of water contained within the snowpack as of April," said USGS scientist Greg Pederson, the lead author of the study. "Snow deficits were consistent throughout the Rockies due to the lack of precipitation during the cool seasons during the 1930s coinciding with the Dust Bowl era. From 1980 on, warmer spring temperatures melted snowpack throughout the Rockies early, regardless of winter precipitation. The model in turn shows temperature as the major driving factor in snowpack declines over the past thirty years."
Runoff from Rocky Mountain winter snowpack accounts for 60 to 80 percent of the annual water supply for more than 70 million people living in the western U.S., and is influenced by factors such as the snowpacks water content, known as snow water equivalent, and the timing of snowmelt
The study, "Regional patterns and proximal causes of the recent snowpack decline in the Rocky Mountains," is available from Geophysical Research Letters, a journal of the American Geophysical Union.