Trends in snow water equivalent in the Pacific Northwest and their climatic causes

Details Trends in snow water equivalent in the Pacific Northwest and their climatic causes Trends in snow water equivalent in the Pacific Northwest and their climatic causes

Jun 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30l...3m&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 12, pp. 3-1, CiteID 1601, DOI 10.1029/2003GL017258

Physics

44

Global Change: Water Cycles (1836), Hydrology: Snow And Ice (1827), Global Change: Impact Phenomena

Scientific paper

Observations of snow water equivalent (SWE) in the Pacific Northwest are examined and compared with variability and trends in temperature and precipitation at nearby climate stations. At most locations, especially below about 1800 m, substantial declines in SWE coincide with significant increases in temperature, and occur in spite of increases in precipitation.

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