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Mechanismen der Ausloesung hochreichender Konvektion im suedwestdeutschen Mittelgebirgsraum
註釋The study discusses the occurrence of precipitation induced by deep convection in Germany's southwestern low mountain range in summer of 2007. Based on statistical methods and a case study, the mechanisms triggering the precipitation are described. The complex terrain proved to be a significant factor (divergent flow regimes), among others.