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Frequency-dependent Effects of the Atlantic Meridional Overturning on the Tropical Pacific Ocean : Volume 6, Issue 1 (27/02/2009)

By Te Raa, L. A.

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Book Id: WPLBN0003977977
Format Type: PDF Article :
File Size: Pages 14
Reproduction Date: 2015

Title: Frequency-dependent Effects of the Atlantic Meridional Overturning on the Tropical Pacific Ocean : Volume 6, Issue 1 (27/02/2009)  
Author: Te Raa, L. A.
Volume: Vol. 6, Issue 1
Language: English
Subject: Science, Ocean, Science
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Historic
Publication Date:
2009
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Philip, S. Y., Dijkstra, H. A., Van Oldenborgh, G. J., & Te Raa, L. A. (2009). Frequency-dependent Effects of the Atlantic Meridional Overturning on the Tropical Pacific Ocean : Volume 6, Issue 1 (27/02/2009). Retrieved from http://worldlibrary.net/


Description
Description: Institute for Marine and Atmospheric research Utrecht, Utrecht University, The Netherlands. Using the ECHAM5/MPI-OM model, we study the relation between the variations in the Atlantic meridional overturning circulation (AMOC) and both the Pacific sea surface temperature (SST) and the El Niño-Southern Oscillation (ENSO) amplitude. In a 17-member 20C3M/SRES-A1b ensemble for 1950–2100 the Pacific response to AMOC variations on different time scales and amplitudes is considered. The Pacific response to AMOC variations associated with the Atlantic Multidecadal Oscillation (AMO) is very small. In a 5-member hosing ensemble where the AMOC collapses due to a large freshwater anomaly, the Pacific SST response is large and in agreement with previous work. Our results show that the modelled connection between AMOC and ENSO depends very strongly on the frequency and/or the amplitude of the AMOC variations. Interannual AMOC variations, decadal AMOC variations and an AMOC collapse lead to with entirely different responses in the Pacific Ocean.

Summary
Frequency-dependent effects of the Atlantic meridional overturning on the tropical Pacific Ocean

Excerpt
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