Document Type
Article
Publication Title
Geophysical Research Letters
Rights and Access Note
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Publication Date
8-14-2004
Issue Number
15
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 Nino 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 Nino Suppresses Aantarctic Warming" (2004). Earth Science Faculty Scholarship. 29.
https://digitalcommons.library.umaine.edu/ers_facpub/29
Citation/Publisher Attribution
Bertler, NAN, Barrett, PJ, Mayewski, PA, Fogt, RL, Kreutz, KJ, and Shulmeister, J, 2004, El Nino Suppresses Aantarctic Warming: Geophysical Research Letters, v. 31, L15207. To view the published open abstract, go to http://dx.doi.org and enter the DOI.
Publisher Statement
© Copyright 2004 American Geophysical Union
DOI
10.1029/2004GL020749
Version
publisher's version of the published document