The effect of vertical transfer on the composition of the thermosphere during geomagnetic disturbances

Details The effect of vertical transfer on the composition of the thermosphere during geomagnetic disturbances The effect of vertical transfer on the composition of the thermosphere during geomagnetic disturbances

Sep 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983kosis..21..725v&link_type=abstract

Kosmicheskie Issledovaniia (ISSN 0023-4206), vol. 21, Sept.-Oct. 1983, p. 725-730. In Russian.

Computer Science

1

Ionospheric Composition, Magnetic Disturbances, Mass Transfer, Thermosphere, Vertical Distribution, Atmospheric Models, Atmospheric Turbulence, Diffusion

Scientific paper

A nonstationary solution is obtained to the system of equations of motion and continuity for the principal neutral components (O, O2, and N2) of the thermosphere and geomagnetic-disturbance conditions with allowance for multicomponent diffusion, turbulent transfer, and mean mass transfer. Results are compared with those of a semiempirical model. It is shown that midlatitude variations of the thermospheric composition during geomagnetic disturbances can be modeled theoretically by taking into account two factors: an increase in exospheric temperature and upward mean mass transfer.

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