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| The graph to the right shows Sacramento River Basin annual (hydrologic year, October-September) precipitation for 1895-2002 compared to reconstructed annual streamflow for 869-1977. The Sacramento annual streamflow was reconstucted to A.D. 869 using tree-ring data in northern California and surrounding areas. The reconstruction is of high quality, reflecting 64% (back to 869) to 81% (back to 1630) of the flow variance in the gage record. The reconstruction suggests that the 1930s drought is representative of extreme 6-10 years droughts in the long-term record. However, the instrumental period may be less representative of extreme droughts that last longer than a decade. Prior to 1400, the reconstruction is characterized by multidecadal periods of persistent low and high flow. Although these periods of persistent high or low flow occur in the earlier and least accurate part of the reconstruction, they would represent challenges to water managers were they to occur today. | ![]() "Graph showing reconstructed Sacramento annual streamflow-precipitation Chronology, 869-2002" |
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Reference:
Meko, D.M., M. D. Therrell, C. H. Baisan, and M. K. Hughes, 2001. "Sacramento River Flow Reconstructed to A.D. 869 From Tree Rings", Journal of the American Water Resources Association, v.37, No.4, August 2001. Data and description: ftp://ftp.ngdc.noaa.gov/paleo/treering/reconstructions/california/sacramento_flow.txt |
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