Abstract
In order to understand the regional impacts of variations in the extent of the Hadley circulation in the Southern Hemisphere, regional Hadley circulations are defined in three sectors centered on the main tropical heat sources over Africa, Asia-Pacific (Maritime Continent) and the Americas. These regional circulations are defined by computing a streamfunction from the divergent component of the meridional wind. A major finding from this study is that year-to-year variability in the extent of the hemispheric Hadley circulation in the Southern Hemisphere is primarily governed by variations of the extent of the Hadley circulation in the Asia-Pacific sector, especially during austral spring and summer when there is little co-variability with the African sector, and the American sector exhibits an out of phase behavior. An expanded Hadley circulation in the Southern Hemisphere (both hemispherically and in the Asia-Pacific sector) is associated with La Niña conditions and a poleward expansion of the tropical wet zone in the Asia-Pacific sector. While La Niña also promotes expansion in the American and African sectors during austral winter, these tropical conditions tend to promote contraction in the two sectors during austral summer as a result of compensating convergence over the Americas and Africa sectors: a process driven by variations in the Walker circulation and Rossby wave trains emanating from the tropical Indian Ocean.
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Acknowledgements
This project is supported by the Victorian Climate Initiative (VicCI). E. Maloney was supported by the Climate and Large-Scale Dynamics Program of the National Science Foundation under Grant AGS-1441916, and G. Boschat by the Australian Research Council grant DP140102855. We warmly thank Josephine Brown and Kevin Tory for their insightful comments on the manuscript prior to submission.
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Nguyen, H., Hendon, H.H., Lim, E.P. et al. Variability of the extent of the Hadley circulation in the southern hemisphere: a regional perspective. Clim Dyn 50, 129–142 (2018). https://doi.org/10.1007/s00382-017-3592-2
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DOI: https://doi.org/10.1007/s00382-017-3592-2