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A Gill–Matsuno‐type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall

Kucharski, F., Bracco, A., Yoo, J. H., Tompkins, A. M., Feudale, L., Ruti, P., Dell'Aquila, A.·2009·Quarterly Journal of the Royal Meteorological Society

Abstract

Recent studies using coupled atmosphere–ocean models have shown that the tropical Atlantic has a significant impact on the Indian monsoon. In this article, the observational basis for this teleconnection is examined and the physical mechanism responsible for bridging sea‐surface temperatures (SSTs) in the Atlantic and precipitation over India is investigated with idealized atmospheric general circulation model (AGCM) experiments in which constant SST anomalies are prescribed and ‘switched on’ in the tropical Atlantic region. A simple Gill–Matsuno‐type quadrupole response is proposed to explain the teleconnection between the tropical Atlantic and the Indian basin, with an enforcement of the eastward response likely due to nonlinear interactions with the mean monsoon circulation. The simplicity of this mechanism suggests the reproducibility of this result with a broad range of AGCMs. Copyright © 2009 Royal Meteorological Society

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Metadata

Authors
Kucharski, F., Bracco, A., Yoo, J. H., Tompkins, A. M., Feudale, L., Ruti, P., & Dell'Aquila, A.
Venue
Quarterly Journal of the Royal Meteorological Society
Publisher
Wiley
Published
2009-04
Volume
135
Issue
640
Pages
569-579
ISSN
  • 0035-9009 (ISSN-L)
  • 1477-870X
OpenAlex
W2030971212
Cited by
267
References
6
FWCI
9.69
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: A Gill–Matsuno‐type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall. https://app.cochat.ai/papers/10.1002/qj.406
The paper
Kucharski, F., Bracco, A., Yoo, J. H., Tompkins, A. M., Feudale, L., Ruti, P., & Dell'Aquila, A. (2009). A Gill–Matsuno‐type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall. Quarterly Journal of the Royal Meteorological Society. https://doi.org/10.1002/qj.406

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