Streamflow and the Climate Transition Zone in the Western United States
Hydroclimatic variability in the western United States (the West) is characterized by a north-south dipole pattern of precipitation and streamflow variance, with centers of opposite association in the Pacific Northwest and the Desert Southwest. These dipole centers tend to react in opposite fashion...
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| Language: | EN |
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The University of Arizona.
2009
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| Online Access: | http://hdl.handle.net/10150/195178 |