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Understanding equatorial Atlantic interannual variability.
Keenlyside, Noel and Latif, Mojib (2007) Understanding equatorial Atlantic interannual variability. Journal of Climate, 20 (1). pp. 131-142. DOI 10.1175/JCLI3992.1.
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Abstract
An observational-based analysis of coupled variability in the equatorial Atlantic and its seasonality is presented. Regression analysis shows that the three elements of the Bjerknes positive feedback exist in the Atlantic and are spatially similar to those of the Pacific. The cross-correlation functions of the elements of the Bjerknes feedback are also similar and consistent with an ocean–atmosphere coupled mode. However, the growth rate in the Atlantic is up to 50% weaker, and explained variance is significantly lower. The Bjerknes feedback in the Atlantic is strong in boreal spring and summer, and weak in other seasons, which explains why the largest sea surface temperature anomalies (SSTAs) occur in boreal summer. Its seasonality is determined by seasonal variations in both atmospheric sensitivity to SSTA and SSTA sensitivity to subsurface temperature anomalies.
Document Type: | Article |
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Keywords: | Climatology; interannual variability, equatorial Atlantic, climate; Sea surface temperature; El Nino; Enso |
Research affiliation: | OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-ME Maritime Meteorology Kiel University |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | AMS (American Meteorological Society) |
Projects: | DYNAMITE, AMMA, BMBF Nordatlantik |
Date Deposited: | 03 Dec 2008 16:51 |
Last Modified: | 04 Aug 2020 09:37 |
URI: | https://oceanrep.geomar.de/id/eprint/2470 |
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