Open Access

Fig. 7.


Download original image

Maps for the daytime vertical plasma transport caused by horizontal thermospheric wind at December and June solstice (a), (b). Panel (c) shows the local winters longitudinal variations of the vertical plasma transport averaged in the 40–60° geographic latitude bands in the Northern (blue) and Southern (red) Hemispheres. Bold gray curves (a), (b) are the geomagnetic equator and ±15° geomagnetic latitudes.

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.