Document Type
Article
Publication Title
Geophysical Research Letters
Rights and Access Note
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Publication Date
2004
Publication Number
L15207
Volume Number
31
Abstract/ Summary
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.
Repository Citation
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.
https://digitalcommons.library.umaine.edu/ers_facpub/197
Citation/Publisher Attribution
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
Publisher Statement
© Copyright American Geophysical Union
DOI
10.1029/2004GL020749
Version
publisher's version of the published document