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- W758185332 abstract "The upper atmosphere wind distribution is calculated by solving the Navier-Stokes equations with models of upper atmospheric densities and ion distribution. All non-linear terms and viscous terms are included. It is found that the velocities from the non-linear solutions are smaller than those obtained from a linear treatment and that in the equatorial region the magnitude of the average meridional velocity is strongly dependent upon the latitudinal coupling. No appreciable super-rotation is obtained by the inclusion of the nonlinear terms; the small value of the average zonal velocity is mainly due to the ion distribution." @default.
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- W758185332 date "1973-01-01" @default.
- W758185332 modified "2023-09-23" @default.
- W758185332 title "The global wind system in the thermosphere." @default.
- W758185332 hasPublicationYear "1973" @default.
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