Vertical Temperature Profiles
Vertical Temperature Profiles is a geophysical construct that represents the equilibrium distribution of atmospheric temperature as a function of altitude, derived from the balance between absorbed solar radiation and emitted thermal radiation, distinguishing it from other atmospheric models by explicitly characterizing the steady-state thermal structure imposed by radiative transfer processes.
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The Halogen Occultation Experiment
James M. Russell, L. L. Gordley, Jae H. Park et al. · Journal of Geophysical Research Atmospheres · 1993 · 974 citations · Full text
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Centre National de la Recherche Scientifique, France
13 publications · 654 citations
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Jet Propulsion Laboratory
Pasadena, United States
38 h-index
189 publications
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Goddard Space Flight Center
Greenbelt, United States
37 h-index
168 publications
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Centre National de la Recherche Scientifique
Paris, France
36 h-index
215 publications
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NSF National Center for Atmospheric Research
Boulder, United States
33 h-index
100 publications
7.9K citations
University of Colorado Boulder
Boulder, United States
27 h-index
102 publications
4.9K citations
University of Oxford
Oxford, United Kingdom
24 h-index
57 publications
5.9K citations
Massachusetts Institute of Technology
Cambridge, United States
23 h-index
44 publications
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Colorado State University
Fort Collins, United States
23 h-index
48 publications
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JGR · 192 publications · 17.6K citations
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59 publications · 6.1K citations
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62 publications · 3.5K citations
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50 publications · 2.7K citations
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