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The analysis aims at analysing the evolution of the 0°C isothermal altitude during intense rainfall events. The following steps are followed: • The rainfall events of around 100 meteorological stations measuring at hourly time step are considered. • Two meteorological sounding stations launching two weather balloons per day are considered. • The variation of the 0°C is analysed depending on the rainfall event duration. • The analysis is carried out distinguishing between winter (December-February) and summer (June-August).
Julia Schmale, Andrea Baccarini, Roman Pohorsky
David Andrew Barry, Ulrich Lemmin, Htet Kyi Wynn, Anton Ivanov, Abolfazl Irani Rahaghi, Stepan Tulyakov, Ludovic Zulliger, Nawaaz Sidharth Gujja Shaik, Jean-Luc Liardon, Philippe Olivier Paccaud, Jérôme Béguin, Beat Marcel Geissmann, Pascal Klaus