Inertial Gravity Waves
Inertial Gravity Waves is a type of atmospheric or oceanic wave that results from the restoring forces of buoyancy and the Coriolis effect, distinguished by its propagation in stably stratified rotating fluids where oscillations occur at frequencies between the inertial and buoyancy frequencies.
224
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9.9K
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447
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243
Institutions
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2017–2026
35
Variants
Inertial-gravity Waves
Parents
224
Balance and Ensemble Kalman Filter Localization Techniques
Steven J. Greybush, Eugenia Kalnay, Takemasa Miyoshi et al. · Monthly Weather Review · 2010 · 264 citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
14 h-index
27 publications
790 citations

NSF National Center for Atmospheric Research
Boulder, United States
13 h-index
18 publications
1K citations
Wuhan University
Wuhan, China
12 h-index
55 publications
1.4K citations

University of Edinburgh
Edinburgh, United Kingdom
10 h-index
18 publications
846 citations

Kyoto University
Kyoto, Japan
9 h-index
19 publications
858 citations

Nanjing University of Information Science and Technology
Nanjing, China
8 h-index
9 publications
192 citations
Maxwell Institute for Mathematical Sciences
Edinburgh, United Kingdom
8 h-index
14 publications
654 citations
University of Cambridge
Cambridge, United Kingdom
7 h-index
15 publications
1.5K citations
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45 publications · 2.7K citations
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26 publications · 1K citations
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JGR · 13 publications · 633 citations
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12 publications · 519 citations
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10 publications · 330 citations
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