Long‐Term Earth‐Moon Evolution With High‐Level Orbit and Ocean Tide Models

Tides and Earth‐Moon system evolution are coupled over geological time. Tidal energy dissipation on Earth slows Earth′s rotation rate, increases obliquity, lunar orbit semi‐major axis and eccentricity, and decreases lunar inclination. Tidal and core‐mantle boundary dissipation within the Moon decrea...

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Bibliographic Details
Published in:Journal of geophysical research. Planets Vol. 126; no. 12; pp. e2021JE006875 - n/a
Main Authors: Daher, Houraa, Arbic, Brian K., Williams, James G., Ansong, Joseph K., Boggs, Dale H., Müller, Malte, Schindelegger, Michael, Austermann, Jacqueline, Cornuelle, Bruce D., Crawford, Eliana B., Fringer, Oliver B., Lau, Harriet C. P., Lock, Simon J., Maloof, Adam C., Menemenlis, Dimitris, Mitrovica, Jerry X., Green, J. A. Mattias, Huber, Matthew
Format: Journal Article
Language:English
Published: Washington Blackwell Publishing Ltd 01.12.2021
John Wiley and Sons Inc
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ISSN:2169-9097, 2169-9100
Online Access:Get full text
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