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-wave-induced PSCs (e.g., Maturilli and Dörnbrack 2006 , their Fig. 9). This first, qualitative interpretation is supported by the very structured ice PSCs occurring in a region both above and downstream of Svalbard’s mountains and above the underlying clouds near the tropopause as mentioned above. As shown later, the satellite trace (as sketched in Figs. 3 and 6 ) was nearly parallel to the stratospheric winds at this time and the mountain-wave-induced temperature anomalies are tilted into the ambient wind
-wave-induced PSCs (e.g., Maturilli and Dörnbrack 2006 , their Fig. 9). This first, qualitative interpretation is supported by the very structured ice PSCs occurring in a region both above and downstream of Svalbard’s mountains and above the underlying clouds near the tropopause as mentioned above. As shown later, the satellite trace (as sketched in Figs. 3 and 6 ) was nearly parallel to the stratospheric winds at this time and the mountain-wave-induced temperature anomalies are tilted into the ambient wind
