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• W2077737588 abstract "Abstract Streamflow since 1560 A.D. for four rivers within the Sacramento River Basin, California, has been reconstructed dendroclimatically. Both the highest and the lowest reconstructed streamflows occurred during the historical period, with high flows from 1854 to 1916 and low flows from 1917 to 1950. Prolonged (decade-scale) excursions from the mean have been the norm throughout the reconstructed period. The periods of high and low streamflow in the Sacramento Basin are generally synchronous with wet and dry periods reconstructed by dendroclimatic studies in the western United States. The record indicates a number of asynchronous droughts or wet years. The strongest contrasts are developed between northern (western Washington and Oregon or the Columbia Basin) and southern (the Sacramento Basin or central California) climate regions. These asynchronous events may be due to variation in the latitude of the subtropical high and in the latitudinal position of winter storms coming off the Pacific. No association was found with El Niño-Southern Oscillation events." @default.
• W2077737588 created "2016-06-24" @default.
• W2077737588 creator A5054535847 @default.
• W2077737588 date "1993-05-01" @default.
• W2077737588 modified "2023-09-27" @default.
• W2077737588 title "Asynchronous Droughts in California Streamflow as Reconstructed from Tree Rings" @default.
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• W2077737588 doi "https://doi.org/10.1006/qres.1993.1036" @default.
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