Planetary Cooling
Planetary Cooling is a geophysical process denoting the gradual reduction in a planet's internal thermal energy over time, driven primarily by conductive, convective, and radiative heat loss mechanisms distinct from external thermal influences.
83
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5.9K
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185
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112
Institutions
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2017–2026
15
Variants
Planetary Thermal Evolution
83
Cooling and ice growth across the Eocene-Oligocene transition
Caroline H. Lear, T. R. Bailey, Paul N. Pearson et al. · Geology · 2008 · 412 citations
The astronomical theory of climatic change on Mars
O. B. Toon, James B. Pollack, William R. Ward et al. · Icarus · 1980 · 350 citations
Mars: A New Core-Crystallization Regime
Andrew J. Stewart, Max W. Schmidt, W. van Westrenen et al. · Science · 2007 · 227 citations
Subsolidus convective cooling histories of terrestrial planets
G. Schubert, P. Cassen, Richard E. Young · Icarus · 1979 · 206 citations
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112
University of California, Los Angeles
Los Angeles, United States
5 h-index
6 publications
757 citations

Ames Research Center
Mountain View, United States
5 h-index
9 publications
1.3K citations
University of Arizona
Tucson, United States
4 h-index
7 publications
427 citations
Planetary Science Institute
Tucson, United States
4 h-index
6 publications
356 citations

Cornell University
Ithaca, United States
4 h-index
5 publications
568 citations
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
7 publications
553 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
7 publications
1.3K citations
Hebrew University of Jerusalem
Jerusalem, Israel
3 h-index
4 publications
241 citations
1–8 of 112
9 publications · 861 citations
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ApJ · 8 publications · 614 citations
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8 publications · 430 citations
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JGR · 7 publications · 420 citations
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6 publications · 718 citations
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