In the Rocky Mountains, spring (February - March) warming since the 1980s has been largely responsible for recent
snowpack declines at mid - and low - elevation sites (Pederson et al. 2013b).
Not exact matches
A new study of long - term snow monitoring sites in the western United States found
declines in
snowpack at more than 90 percent of those sites — and one - third of the
declines were deemed significant.
This time, no return to cooler period Tim Barnett, a climatologist
at Scripps Institution of Oceanography, said the new results appear to agree with his earlier work that used climate models to show humans» greenhouse gas emissions have contributed to
declining snowpack in the western United States.
«The Northern Rockies have shown the greatest response to warming in terms of
snowpack decline,» said lead author Greg Pederson, a research scientist
at the U.S. Geological Survey's Northern Rocky Mountain Research Center.
Singer suggested a regional
decline in
snowpacks and less groundwater recharge
at the mountain fronts has negatively affected water resources.
The observed melting is greatest
at lower elevations, a trend matched in
snowpack declines across the Western U.S.
A new study of long - term snow monitoring sites in the western United States found
declines in
snowpack at more than 90 percent of those sites - and one - third of the
declines were deemed significant.
Snowfall varies across the region, comprising less than 10 % of total precipitation in the south, to more than half in the north, with as much as two inches of water available in the
snowpack at the beginning of spring melt in the northern reaches of the river basins.81 When this amount of snowmelt is combined with heavy rainfall, the resulting flooding can be widespread and catastrophic (see «Cedar Rapids: A Tale of Vulnerability and Response»).82 Historical observations indicate
declines in the frequency of high magnitude snowfall years over much of the Midwest, 83 but an increase in lake effect snowfall.61 These divergent trends and their inverse relationships with air temperatures make overall projections of regional impacts of the associated snowmelt extremely difficult.
If treatments
at this scale are completed and repeated over the next several decades, increases in runoff could help offset the current and projected
declines in
snowpack and stream flow due to warming while improving the resilience of forest stands.
The magnitude of observed
declines in
snowpack in the Southwest, in the range of 20 %, is similar to the increases in runoff associated with thinning from this study, suggesting that accelerated thinning may
at least offset or ameliorate runoff losses due to climate change.
In the winter despite a small increase in precipitation, retained
snowpack at the end of the winter has
declined.
Those who do come to the Northwest will be faced with an unpleasant reality, she adds, reciting a list of problems expected to strike the region before the turn of the century: regional temperature increases between 5.5 and 9.1 degrees Fahrenheit; drier summers making the Northwest's forests more susceptible to fire;
declining snowpack, as more precipitation falls as rain instead of snow
at higher elevations, straining regional water supplies and increasing the risk of flooding downstream.