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

Citeable URL: https://ir.library.oregonstate.edu/concern/articles/kk91fr44p

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Attribute Name	Values
Creator	Mote, Philip W.
Abstract	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.
Resource Type	Article
DOI	https://doi.org/10.1029/2003GL017258
Fecha Disponible	2010-10-05T22:46:19+00:00
Fecha de Emisión	2003-06-17
Citation	Mote, P. W. (2003). 10.1029/2003GL017258. Geophysical Research Letters, 30(12). doi:10.1029/2003GL017258
Journal Title	Geophysical Research Letters
Journal Volume	30
Journal Issue/Number	12
Declaración de derechos	In Copyright
Publisher	American Geophysical Union
Language	English [eng]
Replaces	http://hdl.handle.net/1957/18711

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