Monsoon-Driven Mountain Climate is a climatological regime characterized by seasonal reverse of wind patterns and precipitation cycles in mountainous regions, distinguished by the dominant influence of monsoonal dynamics on temperature, humidity, and orographic rainfall distribution.
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The twentieth century was the wettest period in northern Pakistan over the past millennium
Kerstin Treydte, Gerhard H. Schleser, Gerhard Helle et al. · Nature · 2006 · 649 citations · Full text
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Chinese Academy of Sciences
Beijing, China
15 h-index
68 publications
6.7K citations
Institute of Atmospheric Physics
Beijing, China
6 h-index
17 publications
915 citations
Institute of Earth Environment
Xi'an, China
5 h-index
11 publications
798 citations
University of Chinese Academy of Sciences
Beijing, China
5 h-index
14 publications
1.5K citations
The Open University
Milton Keynes, United Kingdom
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4 publications
716 citations
Xishuangbanna Tropical Botanical Garden
Mengla, China
3 h-index
12 publications
1.9K citations
Lanzhou University
Lanzhou, China
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9 publications
351 citations
University of Bristol
Bristol, United Kingdom
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- Palaeogeography Palaeoclimatology Palaeoecology
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3 publications · 367 citations
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2 publications · 129 citations
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