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Decadal interactions between the western tropical Pacific and the North Atlantic Oscillation

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Abstract

The relationship between interdecadal variations of tropical sea surface temperature (SST) in the last 120 years and circulation anomalies related to the North Atlantic Oscillation (NAO) is investigated in this study. Using an atmospheric general circulation model (AGCM), we confirm observational evidence that variations in the SST gradient in the western tropical Pacific are related to the NAO anomalies on decadal timescale, and may be contributing to the shift towards the positive NAO phase observed in the late 20th century. The role played by the Indian Ocean-NAO teleconnection, advocated in recent studies focused on the last 50 years, is also assessed in the context of the 120-year long record. It is suggested that a positive feedback between the Pacific SST and the hemispheric circulation pattern embedding the decadal NAO signal may act to enhance the internal variability of the coupled ocean–atmosphere system, and justify the stronger teleconnection found in observational data than in SST-forced AGCM experiments.

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Notes

  1. Alternatively, it is possible to calculate first the global meridional SST gradient and then to regress the SST gradient onto the NAO index. This provides a direct measure of the SST gradient field related to the NAO. An index, analogous to the one in the paper, can then be defined as the maximum gradient located at about [150°E to 170°W, 5°N to 10°N]. Results do not change significantly, and we prefer the definition in Sect. 3 because of its simplicity and of smoother fields.

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Acknowledgments

The authors wish to thank Giulio Boccaletti and George Philander for useful discussions during the preparation of this manuscript. We also thank the two anonymous reviewers for their constructive suggestions.

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Correspondence to Fred Kucharski.

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Kucharski, F., Molteni, F. & Bracco, A. Decadal interactions between the western tropical Pacific and the North Atlantic Oscillation. Clim Dyn 26, 79–91 (2006). https://doi.org/10.1007/s00382-005-0085-5

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