A role of the altitude gradient of the thermospheric wind velocity in ionospheric F-region dynamics

Details A role of the altitude gradient of the thermospheric wind velocity in ionospheric F-region dynamics A role of the altitude gradient of the thermospheric wind velocity in ionospheric F-region dynamics

Jun 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011ge%26ae..51..377y&link_type=abstract

Geomagnetism and Aeronomy, Volume 51, Issue 3, pp.377-382

Computer Science

Sound

Scientific paper

By processing the data of vertical ionospheric sounding in Almaty for 2000-2009, we obtained the distributions of the heights of the maximum ( h m F) and bottom ( h bot F) of the F2-layer, incremental changes in its semi-thickness (δ h), the characteristic time of losses (τ), and the vertical displacement velocity of the node of the thermospheric wind ( V) during the transitional time of the day during nighttime increases in the electron concentration at the layer maximum. The comparison of the measured V and modeled V m velocities showed a certain discrepancy. The influence of the altitude gradient of the meridional thermospheric wind velocity on the behaviors of h m F, h bot F, δ h, and τ during nighttime increases in the electron concentration is studied.

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