Fig. 8From: Comparison of the tidal signatures in sporadic E and vertical ion convergence rate, using FORMOSAT-3/COSMIC radio occultation observations and GAIA modelMonth-to-month amplitude variation of SW1 (left column) and SW3 (right column) components of VIC (first row), zonal wind term in VIC (second row) and the zonal wind term VIC without the effect of magnetic field zonal asymmetry (third row) at different altitudesBack to article page