Free Access

Fig. 9

thumbnail

Illustration of the projected emission layer width used for the derivation of the beam-specific, incident airglow intensities in the 3D scattering calculations. The extension of the scattering atmosphere is limited to the lower boundary of the airglow emission layer. Point O can be in a different plane from the other points (cf. Fig. 4).

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.