Wintertime Surface Cooling
Wintertime Surface Cooling is a climatological process denoting the net loss of heat from the ocean's surface layer to the atmosphere during the winter months, primarily driven by atmospheric heat exchange, which enhances surface water density and can initiate deep convection in high-latitude regions.
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Winter warming from large volcanic eruptions
Alan Robock, Jianping Mao · Geophysical Research Letters · 1992 · 347 citations · Full text
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Chinese Academy of Sciences
Beijing, China
9 h-index
17 publications
959 citations
Woods Hole Oceanographic Institution
Falmouth, United States
5 h-index
7 publications
203 citations
Institute of Atmospheric Physics
Beijing, China
5 h-index
9 publications
755 citations
University of Maryland, College Park
College Park, United States
5 h-index
17 publications
1.1K citations
University of Chinese Academy of Sciences
Beijing, China
4 h-index
4 publications
301 citations
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
Guangzhou, China
4 h-index
6 publications
199 citations
University of Cambridge
Cambridge, United Kingdom
4 h-index
9 publications
386 citations

Tohoku University
Sendai, Japan
4 h-index
9 publications
346 citations
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13 publications · 1.3K citations
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JGR · 17 publications · 891 citations
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8 publications · 1.1K citations
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