Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 41, Issue 20, Pages 7298-7305Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL061661
Keywords
drought; Dust Bowl; aerosols
Categories
Funding
- NSF [AGS-1243204, AGS-1401400]
- National Aeronautics and Space Administration Modeling Analysis and Prediction Program [WBS 281945.02.04.02.74]
- Div Atmospheric & Geospace Sciences
- Directorate For Geosciences [1401400, 1243204] Funding Source: National Science Foundation
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During the summer of 1934, over 70% of western North America experienced extreme drought, placing this summer far outside the normal range of drought variability and making 1934 the single worst drought year of the last millennium. Strong atmospheric ridging along the West Coast suppressed cold season precipitation across the Northwest, Southwest, and California, a circulation pattern similar to the winters of 1976-1977 and 2013-2014. In the spring and summer, the drying spread to the Midwest and Central Plains, driven by severe precipitation deficits downwind from regions of major dust storm activity, consistent with previous work linking drying during the Dust Bowl to anthropogenic dust aerosol forcing. Despite a moderate La Nina, contributions from sea surface temperature forcing were small, suggesting that the anomalous 1934 drought was primarily a consequence of atmospheric variability, possibly amplified by dust forcing that intensified and spread the drought across nearly all of western North America.
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