Tropical Inversion Layers
Tropical Inversion Layers is a persistent atmospheric boundary layer phenomenon characterized by a stable temperature increase with altitude in the tropical lower troposphere, distinguishing it from diurnally driven or mid-latitude inversion processes.
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1.3K
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117
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68
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2017–2026
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Dynamical Adjustment of the Trade Wind Inversion Layer
Wayne H. Schubert, Paul E. Ciesielski, Chungu Lu et al. · Journal of the Atmospheric Sciences · 1995 · 73 citations · Full text
The Polar Summer Tropopause Inversion Layer
William J. Randel, Fei Wu · Journal of the Atmospheric Sciences · 2010 · 65 citations · Full text
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NSF National Center for Atmospheric Research
Boulder, United States
4 h-index
7 publications
992 citations
Meteorological Research Institute
Tsukuba, Japan
4 h-index
5 publications
336 citations
Colorado State University
Fort Collins, United States
3 h-index
8 publications
1K citations

University of Toronto
Toronto, Canada
2 h-index
5 publications
819 citations
Freie Universität Berlin
Berlin, Germany
2 h-index
2 publications
303 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
2 h-index
5 publications
174 citations

Tel Aviv University
Tel Aviv, Israel
2 h-index
4 publications
58 citations

Centre National de la Recherche Scientifique
Paris, France
2 h-index
5 publications
1.1K citations
1–8 of 68
5 publications · 366 citations
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JGR · 5 publications · 389 citations
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4 publications · 215 citations
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JASTP · 2 publications · 41 citations
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2 publications · 51 citations
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