Warm Core Evolution
Warm Core Evolution is a meteorological framework that characterizes the thermodynamic transformation of extratropical cyclones over oceans through the development of a vertically coherent warm temperature anomaly in the cyclone's core, distinguishing it from baroclinic-driven intensification mechanisms.
112
Publications
7.4K
Citations
258
Authors
135
Institutions
Publications per year
2017–2026
23
112
1–5 of 112
258
5
h-index
4
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4
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3
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3
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1–5 of 258
135

University of Hawaiʻi at Mānoa
Honolulu, United States
9 h-index
15 publications
670 citations
Colorado State University
Fort Collins, United States
5 h-index
9 publications
757 citations
University of Reading
Reading, United Kingdom
5 h-index
8 publications
498 citations
University of Maryland, College Park
College Park, United States
5 h-index
9 publications
894 citations

Naval Postgraduate School
Monterey, United States
5 h-index
9 publications
1K citations
University at Albany, State University of New York
Albany, United States
4 h-index
7 publications
720 citations
Japan Fisheries Research and Education Agency
Yokohama, Japan
4 h-index
6 publications
669 citations

Nanjing University of Information Science and Technology
Nanjing, China
4 h-index
8 publications
380 citations
1–8 of 135
16 publications · 1.3K citations
16
h-index
16 publications · 1.6K citations
14
h-index
JGR · 9 publications · 371 citations
9
h-index
8 publications · 509 citations
8
h-index
7 publications · 244 citations
7
h-index
1–5