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Reaching the lower stratosphere: validating an extended vertical grid for COSMO

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Figure

Figure 1. The vertical grids of the COSMO model considered inthis study. The damping layers are also given as shaded areas.
Figure 4. Temperature values of all soundings of the station JanMayen, station no. 20
Figure 6. Mean temperature values at each height for the station on Jan Mayen, station no
Figure 8. Mean difference in temperature over all heights (top) andcorresponds in color to the full line which is always half the standarddeviation of the difference above and below the mean value
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