Effect of background wind and dissipation processes on the semidiurnal component of atmospheric solar tides
Author:
Funder
Department of Science and Technology, Ministry of Science and Technology, India
Publisher
Elsevier BV
Reference30 articles.
1. Atmospheric Tides;Chapman,1970
2. The diurnal and semidiurnal tides over Ascension Island (°S, 14° W) and their interaction with the stratospheric quasi-biennial oscillation: studies with meteor radar, eCMAM and WACCM;Davis;Atmos. Chem. Phys.,2013
3. Flattery, T.W., 1967. Hough functions (Doctoral dissertation, The University of Chicago).
4. Atmospheric tides: 1. model description and results for the solar diurnal component;Forbes;J. Geophys. Res. Space Phys.,1982
5. Thermal excitation of atmospheric tides due to insolation absorption by O3 and H2O;Forbes;Geophys. Res. Lett.,1978
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