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Updated: Jul 6, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
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最近の地球の平らさの変動:気候変動の解消と氷河期後のリバウンド効果

Jean O Dickey1, Steven L Marcus, Olivier de Viron

  • 1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA. jean.o.dickey@jpl.nasa.gov

Science (New York, N.Y.)
|December 10, 2002
PubMed
まとめ

地球の平坦度 (J2) は,氷河の融解と海洋質量の移転により増加しており,単なる氷河後の反発ではありません. これらの急速な変化は,気候変動に関するさらなる調査を必要とする,重要な地球質量再分配の兆候である.

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