The West’s declining snowpack: is global warming to blame? Philip Mote Climate Impacts Group University of Washington
20th century decline in NH snow cover R.D. Brown, J. Climate, 2000
Trends in snowpack Use VIC and met data to evaluate trends, roles of temperature and precipitation
Snow course data Collected primarily ~April 1 beginning in 1915 (most in 1940s), added other months Purpose: streamflow forecasting Administered by USDA Natural Resource Conservation Service Mostly discontinued, some replaced by SNOTEL
Snow course ???
Courtesy USDA NRCS Data: NRCS CA DWR BC SRM
Courtesy USDA NRCS
decrease increase Trends in April 1 SWE, snow courses 73% – trends Large – trends PNW Some + trends SW
decrease increase Trends in April 1 SWE, Relative to 1950 value
Former snow course location
Relating SWE to climate data US Historical Climate Network (USHCN) Use nearest 5 stations to form reference time series T(t) and P(t) Regression: SWE(t)=a T T(t) + a P P(t)+ (t)
At almost every USHCN station, winters warmed + signs: warming but not statistically significant
Winters wetter in much of the West Drier in some of Northwest (PDO)
Correlations between Nov-Mar climate and Apr 1 SWE X-direction: precip Y-direction: temp Coldest locations insensitive to temperature Cascades very sensitive
April 1 SWE trends, a P a T
April 1 SWE trends, a P a T
SNOTEL data: cold-season melt events vs Apr 1 SWE
Relative trends
Declining snowpack in the Cascades From a simulation with a hydrology model
relative trends vs DJF temperature Obs VIC
Trends in April 1 SWE in VIC simulation with fixed precipitation
As the West warms, winter flows rise and summer flows drop Figure by Iris Stewart, Scripps Inst. of Oceanog. (UC San Diego)
Simulation of future snowpack with VIC hydrologic model Trend in total April 1 snowpack, : -11% Courtesy Andrew W. Wood, University of Washington
SNOTEL data: cold-season melt events vs Apr 1 SWE Figure by Martyn Clark, Univ. of Colorado
Regional average April 1 SWE Obs o VIC x
Changes in SWE vs changes in precip 1930s to 1990s to 1990s Obs SWEVIC SWEPrecipObs SWEVIC SWEPrecip Cascades-14%+1%+4%-29%-16%-5% Rockies+11%+2%+9%-16%-9%+1% California+3%-14%+10%-2%-25%-1% Interior+9%-6%+10%-22%-18%+2%
Trends/15yr in snow days in Switzerland From Scherrer et al., GRL 2004
Trends in Swiss snow days attributed to temperature and precipitation precip and temp attributions; contour lines indicate the sum. Attribution of trends shown by pseudo vectors; altitude and latitude From Scherrer et al., GRL 2004 days/42 yrs.
Conclusions Observations show substantial declines in western snowpack; corroboration with VIC suggests they are real and largely temperature-driven Cascades, N. Calif most temp-sensitive Large increases in precipitation have offset warming in some places Is global warming causing the decline? Too soon to tell.