What is in this article?:
- The warming and snowpack decline are projected to worsen through the 21st century, foreshadowing a strain on water supplies.
- Runoff from winter snowpack accounts for 60 percent to 80 percent of the annual water supply for more than 70 million people living in the Western U.S.
Brunt of loss
"Over most of the 20th century, and especially since the 1980s, the northern Rockies have borne the brunt of the snowpack losses," said USGS scientist Gregory Pederson, the lead author of the study.
"Most of the land and snow in the northern Rockies sits at lower and warmer elevations than the southern Rockies, making the snowpack more sensitive to seemingly small increases in temperature. Also, winter storm tracks were displaced to the south in the early 20th century and post-1980s. Forest fires were larger, more frequent and harder to fight, while Glacier National Park lost 125 of its 150 glaciers."
Pederson conducted part of the research at UA's Laboratory for Tree-Ring Research. He earned his doctorate from the UA in 2010.
USGS scientist and co-author Julio Betancourt said, "The difference in snowpack along the north and south changed in the 1980s, as the unprecedented warming in the springtime began to overwhelm the precipitation effect, causing snowpack to decline simultaneously in the north and south. Throughout the West, springtime tends to be warmer during El Niño than La Niña years, but the warming prior to the 1980s was usually not enough to offset the strong influence of precipitation on snowpack."
The La Niña episode this year is an example with lots of snow in the north while severe drought afflicts the south. But, in the north, this year's gains are only a small blip on a century-long snowpack decline.
In the West, the average position of the winter storm tracks tend to fluctuate north and south around a latitudinal line connecting Denver, Salt Lake City and Sacramento. In El Niño years, winter storms track south of that line, while in La Niña years, they track to the north.
This study supports research by others estimating that between 30 percent to 60 percent of the declines in the late 20th century are likely due to greenhouse gas emissions. The remaining part of the trend can be attributed to natural decadal variability in the ocean and atmosphere, which is making springtime temperatures that much warmer.
Pederson said, "What we have seen in the last few decades may signal a fundamental shift from precipitation to temperature as the dominant influence on western snowpack."
The study, "The unusual nature of recent snowpack declines in the North American Cordillera," is available from Science magazine online.
USGS provides science for a changing world. For more information visit www.usgs.gov.