Wintertime Convection
Wintertime Convection is a meteorological phenomenon characterized by the seasonal occurrence of vertical heat and moisture transport in polar regions during the winter months, driven by strong surface cooling and atmospheric instability distinct from convection in other seasons.
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5.8K
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368
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185
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2017–2026
25
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Oceanographic conditions at Ocean Weather Ship<i>Bravo</i>, 1964–1974
J. R. Lazier · ATMOSPHERE-OCEAN · 1980 · 262 citations · Full text
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Woods Hole Oceanographic Institution
Falmouth, United States
10 h-index
17 publications
1.5K citations

Centre National de la Recherche Scientifique
Paris, France
7 h-index
19 publications
901 citations
Bedford Institute of Oceanography
Dartmouth, Canada
6 h-index
8 publications
1.2K citations
University of Washington
Seattle, United States
5 h-index
28 publications
2.4K citations
Massachusetts Institute of Technology
Cambridge, United States
5 h-index
7 publications
241 citations
University of Bergen
Bergen, Norway
4 h-index
6 publications
126 citations
Bjerknes Centre for Climate Research
Bergen, Norway
4 h-index
6 publications
126 citations
Institut de Recherche pour le Développement
Marseille, France
3 h-index
7 publications
493 citations
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13 publications · 1.2K citations
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8 publications · 461 citations
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7 publications · 280 citations
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7 publications · 344 citations
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6 publications · 196 citations
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