Monsoon Trough is a low-pressure synoptic-scale meteorological feature characterized by a elongated region of minimum sea-level pressure that extends from the continental landmass over adjacent oceanic regions, distinguished by its persistent association with seasonal wind reversals and convectional rainfall maxima in monsoon systems.
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Monsoon Trough Of Low Pressure
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334
David K. Adams, Andrew C. Comrie · Bulletin of the American Meteorological Society · 1997 · 1.2K citations · Full text
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Chinese Academy of Sciences
Beijing, China
23 h-index
83 publications
5.4K citations
Institute of Atmospheric Physics
Beijing, China
22 h-index
81 publications
4.9K citations
Nanjing University of Information Science and Technology
Nanjing, China
19 h-index
47 publications
2.7K citations
University of Hawaiʻi at Mānoa
Honolulu, United States
15 h-index
29 publications
3.7K citations
City University of Hong Kong
Hong Kong, Hong Kong
13 h-index
23 publications
1.5K citations
University of Hawaii System
Honolulu, United States
13 h-index
22 publications
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Indian Institute of Tropical Meteorology
Pune, India
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46 publications
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Chinese Academy of Meteorological Sciences
Beijing, China
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21 publications
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- Monthly Weather Review
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- Journal of Climate
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- International Journal of Climatology
20 publications · 1.2K citations
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- Journal of the Meteorological Society of Japan Ser II
16 publications · 891 citations
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- Geophysical Research Letters
17 publications · 2K citations
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