Stable extension of the unified model into the mesosphere and lower thermosphere | Journal of Space Weather and Space Climate

Topical Issue - Scientific Advances from the European Commission H2020 projects on Space Weather

Open Access

Fig. 1

The default sponge layer with vertical damping coefficient s⁻¹ and 100 km model lid. The sponge layer can be seen to be at s⁻¹ for most latitudes and for high altitudes but is doubled at the polar latitudes for all altitudes to help numerical stability in this area.

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.