The Earth's atmosphere rotates synchronously with the planet due to frictional drag
Geophysical studies and angular momentum budgets confirm that the Earth's atmosphere rotates synchronously with the planet overall, driven and coupled largely through surface friction and mountain torques.
The retrieved papers provide theoretical and modeling backing regarding the planetary boundary layer, frictional torques, and angular momentum exchange between the solid Earth and its atmosphere. These mechanisms explain how the atmosphere maintains its overall rotational coupling with the planet.
Harald Lejenäs, Roland A. Madden, James J. Hack. Global atmospheric angular momentum and Earth‐atmosphere exchange of angular momentum simulated in a general circulation model. 1997. https://doi.org/10.1029/96jd03264
Simulates global atmospheric angular momentum and frictional torques demonstrating how the atmosphere exchanges angular momentum with the rotating Earth.
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Eric B. Kraus, Joost A. Businger. The Planetary Boundary Layer. 1995. https://doi.org/10.1093/oso/9780195066180.003.0010
Discusses the planetary boundary layer where surface frictional drag and momentum fluxes couple the rotating Earth's surface to the fluid envelope above.
Jean O. Dickey. Angular momentum exchange between atmosphere and Earth. 1993. https://doi.org/10.1029/93eo00219
Examines angular momentum exchange between the atmosphere and Earth, noting that without such interactions and internal torques the entire planet and its fluid layers would rotate synchronously.
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