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 [Formula: see text] rotation rate, increases obliquity, lunar orbit semi‐major axis and eccentricity, and decreases lunar inclination. Tidal and core‐mantle boundary dissipation within the...

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Detalles Bibliográficos
Autores principales: 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
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9285098/
https://www.ncbi.nlm.nih.gov/pubmed/35846556
http://dx.doi.org/10.1029/2021JE006875

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