Upper Atmospheric Heating
Upper Atmospheric Heating is a geophysical phenomenon characterized by the increase in thermal energy of the thermosphere and ionosphere due to the absorption of solar extreme ultraviolet and X-ray radiation and the dissipation of energy from magnetospheric and auroral processes.
75
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4.4K
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213
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122
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2017–2026
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75
Joule Heating of the Upper Atmosphere
KD Cole · Australian Journal of Physics · 1962 · 228 citations · Full text
Evolution of the North American Monsoon System
Mathew Barlow, Sumant Nigam, Ernesto Hugo Berbery · Journal of Climate · 1998 · 212 citations
Dynamical heating of the upper atmosphere
C. O. Hines · Journal of Geophysical Research Atmospheres · 1965 · 206 citations · Full text
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Goddard Space Flight Center
Greenbelt, United States
7 h-index
8 publications
320 citations
University of Arizona
Tucson, United States
6 h-index
8 publications
394 citations
Boston University
Boston, United States
4 h-index
9 publications
505 citations

Chinese Academy of Sciences
Beijing, China
4 h-index
12 publications
280 citations
University of California, Los Angeles
Los Angeles, United States
3 h-index
3 publications
212 citations
University College London
London, United Kingdom
3 h-index
9 publications
408 citations

University of Leicester
Leicester, United Kingdom
3 h-index
5 publications
207 citations
The Aerospace Corporation
El Segundo, United States
3 h-index
6 publications
418 citations
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JGR · 15 publications · 1.1K citations
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5 publications · 349 citations
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4 publications · 148 citations
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3 publications · 288 citations
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3 publications · 143 citations
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