Hadley Circulation
Hadley Circulation is a planetary-scale meridional overturning circulation in the tropical atmosphere characterized by rising air near the equator, poleward upper-level flow, and sinking air in the subtropics, driven primarily by differential solar heating and modulated by Earth's rotation.
551
Publications
44.6K
Citations
1.1K
Authors
381
Institutions
Publications per year
2017–2026
140
Variants
Hadley Cell
551
Global Warming and the Weakening of the Tropical Circulation
Gabriel A. Vecchi, Brian J. Soden · Journal of Climate · 2007 · 1.3K citations · Full text
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Institute of Atmospheric Physics
Beijing, China
26 h-index
87 publications
3.7K citations
University of Washington
Seattle, United States
24 h-index
46 publications
4.8K citations

Chinese Academy of Sciences
Beijing, China
24 h-index
80 publications
3.2K citations

NSF National Center for Atmospheric Research
Boulder, United States
23 h-index
40 publications
6.5K citations
California Institute of Technology
Pasadena, United States
22 h-index
52 publications
4.2K citations
Massachusetts Institute of Technology
Cambridge, United States
21 h-index
33 publications
5.4K citations
Columbia University
New York, United States
20 h-index
40 publications
2.6K citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
20 h-index
36 publications
8.4K citations
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110 publications · 9.3K citations
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104 publications · 8.4K citations
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60 publications · 5.5K citations
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JGR · 33 publications · 3K citations
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26 publications · 1.5K citations
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