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FY 2009

Retrospective analysis of sea surface temperature in the northern Bering and Chukchi seas

Ladd, C., and J.E. Overland

NOAA Tech. Memo. OAR PMEL-145, NOAA/Pacific Marine Environmental Laboratory, Seattle, WA, 17 pp (2009)


Sea surface temperature (SST) data from the Chukchi and northern Bering seas beginning in the 1920s are analyzed to investigate low-frequency variability. Although surface air temperatures at Nome, AK, and adjacent weather stations show a shift in the late 1930s and a strong warming signal after 1977, spatial variability and sparse oceanic sampling make it impossible to draw robust conclusions regarding low-frequency temporal variability in SST. Given the data at hand, however, there is no conclusive evidence for decadal-scale or regime-shift variability in SST in the northern Bering/Chukchi Sea region during the 20th century, and the data can be considered to be a single climatology. The warmest SSTs ever measured in eastern Bering Strait were obtained in 2004 during a RUSALCA cruise, and the warmest temperatures measured in western Bering Strait were observed in 2006, providing evidence that we are seeing a distinct warm period in the current decade relative to the 20th century. A cruise from 1880 shows SSTs consistent with the 20th-century climatology.



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