Correlation between the horizontal wind direction and orientation of cross-field anisotropy of small-scale irregularities in the F region of midlatitude ionosphere


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Radio sounding of midlatitude ionosphere shows that natural small-scale electron density irregularities in the F region are cross-field anisotropic. The orientation of the cross-field anisotropy is different under different geophysical conditions. The cross-field anisotropy orientation is matched with the horizontal wind direction calculated within the HWM07 model for each event. It is ascertained that natural irregularities in a plane perpendicular to the magnetic field are stretched along the horizontal wind direction under different geophysical conditions.

Sobre autores

N. Romanova

Polar Geophysical Institute, Kola Scientific Center

Autor responsável pela correspondência
Email: romanova@pgi.ru
Rússia, Murmansk, 183010

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