Neutral winds in the F-region

Details Neutral winds in the F-region Neutral winds in the F-region

Mar 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975p%26ss...23..401i&link_type=abstract

Planetary and Space Science, vol. 23, Mar. 1975, p. 401-408.

Statistics

Computation

Atmospheric Circulation, Atmospheric Models, F Region, Navier-Stokes Equation, Wind Velocity Measurement, Atmospheric Density, Atmospheric Temperature, Equations Of Motion, Equinoxes, Ionospheric Drift, Night, Synoptic Measurement, Transequatorial Propagation, Wind Pressure

Scientific paper

The Navier-Stokes equations are solved by introducing a statistical model of density and a distinct temperature model. The non-linear terms of inertia and the viscous term are not included. The computations have been made for equinoctial conditions at a height of 300 km and at different latitudes. The results are presented in the form of a global wind pattern. The most important features are: the existence of transequatorial winds by night, the asymmetrical structure of the wind pattern and the agreement of the computed velocities with observations.

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