Synoptic-Scale Tropical Circulation is a large-scale atmospheric circulation system characterized by horizontal dimensions of approximately 1000 to 10,000 kilometers and time scales of several days to a week, occurring within the tropics and primarily driven by diabatic heating and moisture convergence, that governs the organization and evolution of weather systems such as tropical depressions, monsoon lows, and easterly waves.
92
Publications
5.2K
Citations
292
Authors
162
Institutions
Publications per year
2017–2026
19
Publications
92
1–5 of 92
Authors
292
- AH
3
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- AM
3
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- PK
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- CR
2
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- JA
2
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1–5 of 292
Institutions
162
Chinese Academy of Sciences
Beijing, China
7 h-index
22 publications
859 citations
Institute of Atmospheric Physics
Beijing, China
5 h-index
18 publications
785 citations
Columbia University
New York, United States
5 h-index
6 publications
312 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
4 h-index
9 publications
173 citations
University of Chinese Academy of Sciences
Beijing, China
4 h-index
7 publications
191 citations
Centre National de la Recherche Scientifique
Paris, France
3 h-index
8 publications
432 citations
University of Manchester
Manchester, United Kingdom
3 h-index
5 publications
217 citations
University of Colorado Boulder
Boulder, United States
3 h-index
5 publications
259 citations
1–8 of 162
Venues
- Monthly Weather Review
12 publications · 1.1K citations
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- Climate Dynamics
10 publications · 542 citations
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- Journal of Climate
6 publications · 240 citations
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- Theoretical and Applied Climatology
6 publications · 250 citations
6
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- International Journal of Climatology
5 publications · 191 citations
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1–5