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Trends in snow water equivalent in the Pacific Northwest and their climatic causes
Article first published online: 17 JUN 2003
DOI: 10.1029/2003GL017258
Copyright 2003 by the American Geophysical Union.
Additional Information
How to Cite
(2003), Trends in snow water equivalent in the Pacific Northwest and their climatic causes, Geophys. Res. Lett., 30, 1601, doi:10.1029/2003GL017258, 12.
Publication History
- Issue published online: 17 JUN 2003
- Article first published online: 17 JUN 2003
- Manuscript Accepted: 15 MAY 2003
- Manuscript Revised: 7 MAY 2003
- Manuscript Received: 5 MAR 2003
- Abstract
- Article
- References
- Cited By
[1] 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.