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Published on: April 3, 2018
The three-dimensional plasma structures and flows of the Earth's upper atmosphere due to the Moon's gravitational
Jann-Yenq Liu1,2,3, Tsung-Yu Wu4,5, Chi-Yen Lin4,5
1Center for Astronautical Physics and Engineering, National Central University, Taoyuan, Taiwan. jyliu@jupiter.ss.ncu.edu.tw.
Abstract:
The semidiurnal (12.42 h) and semimonthly (14.76 days) lunar tides have been well-known by fishermen for several centuries. The gravitational force of the relative positions between the Sun, the Moon, and the Earth results in two symmetrical tidal bulges (double bulges) appearing at equatorial latitudes directly under and opposite the Moon. We utilize ionospheric GNSS (Global Navigation Satellite System) radio occultation soundings to show the global three-dimensional structures and dynamics of the double bulges of ionospheric lunar tides for the first time. The double-bulge amplitude of ionospheric F2-peak height hmF2, lagging the sublunar or antipodal point by about 2-3 h, is about 3-5 km at the equator and 1.5-2.0 km at ± 35° magnetic latitude. The electron density further depicts global three-dimensional plasma flows in the ionosphere.
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