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

Computer Science

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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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