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A Large California Flood and Correlative Global Climatic Events 400 Years Ago

Published online by Cambridge University Press:  20 January 2017

Arndt Schimmelmann ,
Meixun Zhao ,
Colin C. Harvey  and
Carina B. Lange
Arndt Schimmelmann*
Affiliation:
Department of Geological Sciences, Indiana University, Bloomington, Indiana, 47405-1403
Meixun Zhao*
Affiliation:
Department of Earth Sciences, Dartmouth College, Hanover, New Hampshire, 03755-3571
Colin C. Harvey*
Affiliation:
Department of Geological Sciences, Indiana University, Bloomington, Indiana, 47405-1403
Carina B. Lange*
Affiliation:
Scripps Institution of Oceanography, MLRG and GRD, La Jolla, California, 92093-0215
*
1 E-mail: aschimme@indiana.edu.
2 E-mail: meixun.zhao@dartmouth.edu.
3 E-mail: ccharvey@indiana.edu.
4 E-mail: clange@ucsd.edu.
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Abstract

A gray silt layer 1–2 cm thick in the central Santa Barbara Basin, dated by varve counts to A.D. 1605 ± 5 yr, implies an intensity of precipitation, flooding of regional rivers, and transport of terrigenous detritus unmatched in the last 1000 yr. The inferred flood may correlate with the reported rare occurrence of a perennial lake (14C dated to 390 ± 90 B.P.) in California's Mojave Desert, 300 km east of the area draining into the Santa Barbara Basin. The dating of the A.D. 1605 ± 5 yr flood event is consistent with tree-ring evidence for a wet and cold paleoclimate elsewhere in the region. Regional and global climate evidence indicates that much of the world also experienced rapid, intense cooling around A.D. 1605. This cooling was probably accompanied by an equatorward shift of prevailing wind patterns and associated storm tracks.

Keywords

floodsedimentSanta Barbara Basinclimatic teleconnectionpaleoclimateLittle Ice Age
Type
Research Article
Information
Quaternary Research , Volume 49 , Issue 1 , January 1998 , pp. 51 - 61
Copyright
University of Washington

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