Wave-critical Layer Interaction
Wave-Critical Layer Interaction is a theoretical construct in atmospheric and oceanic dynamics that describes the nonlinear feedback mechanism between a propagating baroclinic wave and the localized region of strong vertical shear—its critical layer—where the wave phase speed matches the mean flow velocity, leading to wave amplification, distortion, or breakdown through resonant energy transfer.
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156
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101
Institutions
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2017–2026
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Streaklines in a Perturbed Shear Flow
Francis R. Hama · The Physics of Fluids · 1962 · 179 citations
Steady water waves with a critical layer
Erik Wahlén · Journal of Differential Equations · 2008 · 163 citations
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Naval Postgraduate School
Monterey, United States
7 h-index
17 publications
2K citations
Northwest Research Associates
Redmond, United States
5 h-index
6 publications
589 citations
University of Illinois Urbana-Champaign
Urbana, United States
4 h-index
5 publications
404 citations
University of Washington
Seattle, United States
3 h-index
4 publications
123 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
8 publications
123 citations

Glenn Research Center
Cleveland, United States
3 h-index
7 publications
347 citations
University of Cambridge
Cambridge, United Kingdom
3 h-index
4 publications
222 citations
Institute of Oceanology. PP Shirshov Russian Academy of Sciences
Moscow, Russia
2 h-index
3 publications
63 citations
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14 publications · 602 citations
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13 publications · 596 citations
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JGR · 6 publications · 391 citations
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6 publications · 220 citations
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3 publications · 536 citations
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