Critical-level Interaction
Critical-Level Interaction is a theoretical construct in atmospheric dynamics that identifies the altitude at which the horizontal wind speed matches the phase speed of a mountain wave, leading to wave absorption, reflection, or critical layer formation due to resonant energy transfer between the flow and the wave.
40
Publications
1.8K
Citations
96
Authors
75
Institutions
Publications per year
2017–2026
5
Parents
40
Stratospheric warmings: Observations and theory
M. R. Schoeberl · Reviews of Geophysics · 1978 · 257 citations
Parity-Affected Superconductivity in Ultrasmall Metallic Grains
Jan von Delft, Andrei D. Zaikin, Dmitry S. Golubev et al. · Physical Review Letters · 1996 · 206 citations · Full text
1–5 of 40
96
2
h-index
2
h-index
2
h-index
1
h-index
1
h-index
1–5 of 96
75

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
6 publications
315 citations

United States Naval Research Laboratory
Washington, United States
3 h-index
9 publications
597 citations
Laboratoire de Météorologie Dynamique
Palaiseau, France
2 h-index
2 publications
50 citations
Queen Mary University of London
London, United Kingdom
2 h-index
2 publications
47 citations
Northwest Research Associates
Redmond, United States
2 h-index
4 publications
148 citations
University of California, Berkeley
Berkeley, United States
2 h-index
5 publications
216 citations

Kyoto University
Kyoto, Japan
2 h-index
2 publications
104 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
6 publications
152 citations
1–8 of 75
9 publications · 301 citations
9
h-index
4 publications · 113 citations
4
h-index
2 publications · 115 citations
2
h-index
1 publications · 140 citations
1
h-index
Conference · 1 publications · 19 citations
1
h-index
1–5