Physics
Scientific paper
Feb 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987jatp...49..153f&link_type=abstract
Journal of Atmospheric and Terrestrial Physics (ISSN 0021-9169), vol. 49, Feb. 1987, p. 153-164.
Physics
34
Atmospheric Tides, Diurnal Variations, Gravity Waves, Middle Atmosphere, Atmospheric Heating, Atmospheric Moisture, Dissipation, Insolation, Thermodynamic Equilibrium
Scientific paper
Using an equivalent gravity wave f-plane model, it is shown that longitude variations in diurnal insolation absorption by tropospheric H2O can account for longitudinal variations of at least + or - 12-15 percent about zonal mean values in the diurnal wind amplitude at low latitudes (0-20 deg) between 80 and 100 km, by virtue of the nonmigrating propagating tidal modes which are excited. Phase variations of about + or - 0.75 h also occur. These percentage variations are conservative estimates, since the background migrating (1, 1, 1) mode appears to be slightly overestimated in amplitude. In addition, the assumed eddy dissipation values, which appear necessary to model the breaking (1, 1, 1) mode, are larger than generally considered 'reasonable' by photochemical modelers. For a photochemically more reasonable eddy diffusion profile, estimates of longitude differences in diurnal wind amplitude are quite similar to the above values below 87 km, but increase to + or - 17-25 percent near 100 km, with accompanying phase variations of + or - 1-2 h about zonal mean values. In addition, it is shown that radiative damping by CO2 parameterized by a scale-dependent Newtonian cooling coefficient accounts for no more than a 20 percent reduction in the amplitudes of diurnal propagating tides above 80 km.
Forbes Jeffrey M.
Groves Gerald V.
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