Abstract (eng)
The Wienerwald is a hilly landscape representing the most northeastern parts of the european alps. The highest mountain within this region is about \SI{600}{m} to \SI{700}{m} higher than the surrounding area. In the past, alpine meteorology effects have been observed repeatedly nearby the Wienerwald. Existing studies and field experiments in the field of the alpine meteorology are mostly considering middle or high montains like the European Alps or the Rocky Mountains in North America. Therefore, a qualitative statement about the occurrence of the effects in relation to a hilly landscape should be conducted. In addition it should also be investigated which adaptations have to be carried out during the transition of the concepts to a hilly landscape like the Wienerwald. In this master's thesis, six effects from the field of alpine meteorology are investigated in connection with the Wienerwald. This is done partly by statistical evaluations and partly by the analysis of eight case studies. For this purpose, high temporal resolution measurements, observations, remote sensing data such as satellite images or radar data and analysis models are available. It turns out that each of the considered alpinemeteorolgical effects can be observed in connection with the Wienerwald, at least in a weakened form. An adaptation to the concepts from higher mountains is necessary almost everywhere.