Rossby Wave Amplification is a geophysical phenomenon characterized by the increase in the amplitude of planetary-scale Rossby waves in the atmosphere or ocean, resulting from changes in the background flow or thermal gradients that enhance wave energy propagation and growth.
39
Publications
4.4K
Citations
143
Authors
100
Institutions
Publications per year
2017–2026
15
Parents
Publications
39
1–5 of 39
Authors
143
- PC
2
h-index
- DC
2
h-index
- XL
2
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- HN
2
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- GD
2
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1–5 of 143
Institutions
100
Chinese Academy of Sciences
Beijing, China
4 h-index
13 publications
244 citations
Institute of Atmospheric Physics
Beijing, China
4 h-index
10 publications
193 citations
University of Oxford
Oxford, United Kingdom
3 h-index
4 publications
509 citations
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
Guangzhou, China
3 h-index
11 publications
1.3K citations
Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)
Zhuhai, China
3 h-index
11 publications
1.3K citations
Ocean University of China
Qingdao, China
2 h-index
5 publications
78 citations
University of Bergen
Bergen, Norway
2 h-index
3 publications
77 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
2 h-index
2 publications
264 citations
1–8 of 100
Venues
- Journal of the Atmospheric Sciences
6 publications · 786 citations
6
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- Monthly Weather Review
4 publications · 161 citations
4
h-index
- Geophysical Research Letters
4 publications · 2K citations
4
h-index
- Journal of Geophysical Research Atmospheres
JGR · 3 publications · 87 citations
3
h-index
- Journal of the Meteorological Society of Japan Ser II
3 publications · 94 citations
3
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1–5