The Atlantic Multidecadal Oscillation without a role for ocean circulation

Amy Clement, Katinka Bellomo, Lisa N. Murphy, Mark A. Cane, Thorsten Mauritsen, Gaby Rädel, Bjorn Stevens

Research output: Contribution to journalArticle

160 Scopus citations

Abstract

The Atlantic Multidecadal Oscillation (AMO) is a major mode of climate variability with important societal impacts. Most previous explanations identify the driver of the AMO as the ocean circulation, specifically the Atlantic Meridional Overturning Circulation (AMOC). Here we show that the main features of the observed AMO are reproduced in models where the ocean heat transport is prescribed and thus cannot be the driver. Allowing the ocean circulation to interact with the atmosphere does not significantly alter the characteristics of the AMO in the current generation of climate models. These results suggest that the AMO is the response to stochastic forcing from the mid-latitude atmospheric circulation, with thermal coupling playing a role in the tropics. In this view, the AMOC and other ocean circulation changes would be largely a response to, not a cause of, the AMO.

Original languageEnglish (US)
Pages (from-to)320-324
Number of pages5
JournalScience
Volume350
Issue number6258
DOIs
StatePublished - Oct 16 2015

ASJC Scopus subject areas

  • General

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    Clement, A., Bellomo, K., Murphy, L. N., Cane, M. A., Mauritsen, T., Rädel, G., & Stevens, B. (2015). The Atlantic Multidecadal Oscillation without a role for ocean circulation. Science, 350(6258), 320-324. https://doi.org/10.1126/science.aab3980