Geophysical Research Letters
Here we present new isotope records derived from snow samples from the McMurdo Dry Valleys, Antarctica and re-analysis data of the European Centre for Medium-Range Weather Forecasts (ERA-40) to explain the connection between the warming of the Pacific sector of the Southern Ocean [Jacka and Budd, 1998; Jacobs et al., 2002] and the current cooling of the terrestrial Ross Sea region [Doran et al., 2002a]. Our analysis confirms previous findings that the warming is linked to the El Niño Southern Oscillation (ENSO) [Kwok and Comiso, 2002a, 2002b; Carleton, 2003; Ribera and Mann, 2003; Turner, 2004], and provides new evidence that the terrestrial cooling is caused by a simultaneous ENSO driven change in atmospheric circulation,sourced in the Amundsen Sea and West Antarctica.
Bertler, Nancy A. N.; Barrett, Peter J.; Mayewski, Paul Andrew; Fogt, Ryan L.; Kreutz, Karl J.; and Shulmeister, James, "El Niño Suppresses Antarctic Warming" (2004). Earth Science Faculty Scholarship. 197.
Bertler, N. A. N., P. J. Barrett, P. A. Mayewski, R. L. Fogt, K. J. Kreutz, and J. Shulmeister (2004), El Niño suppresses Antarctic warming, Geophysical Research Letters, 31, L15207, doi:10.1029/2004GL020749. http://www.agu.org/pubs/crossref/2004/2004GL020749.shtml
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