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- W187187355 abstract "Sea-surface temperature (SST) data, which are reflective of air-sea interactions, are only available for the periods 1924 to 1940 and 1949 to 1972. In order to augment this short-term data, reconstruction of SST data are made using climatically sensitive tree-ring data. This involves multiple linear regression analyses between SST for 1 squares off southern California and Baja California (22N to 33N) and tree-ring data from seven sites in western North America. A reconstructed summer SST series is shown to be negatively correlated (r = -0.49) with anaerobic sediment core estimates of variations in northern anchovy populations off southern Baja California since 1785. Examination of the reconstructed SST reveals that the period 1671 to 1800 was typified by warm winter SST's and cool summer SST's. By the early 18OO's, summers became anoqalously warm off Baja California, and this summer warming climaxed in the 1840's and 1850's. During this warm summer period, SST anomalies were in excess of +2.0°C, and this is equivalent to a 2 latitudinal shift in SST fields, and a 2 northward shift in the oceanic front off southern Baja California." @default.
- W187187355 created "2016-06-24" @default.
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- W187187355 date "1980-01-01" @default.
- W187187355 modified "2023-09-27" @default.
- W187187355 title "GEOPHYSICAL ESTIMATES OF SEA-SURFACE TEMPERATURES OFF WESTERN NORTH AMERICA SINCE 1671" @default.
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- W187187355 hasPublicationYear "1980" @default.
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