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Heatwaves are known to arise from the interplay between large-scale climate variability, synoptic weather patterns and regional to local scale surface processes. While recent research has made important progress for each individual contributing factor, ways to properly incorporate multiple or all of them in a unified analysis are still lacking.
1 INTRODUCTION Apart from temperature increase and sea-level rise, the reaction of the global hydrological cycle is one of the most interesting and potentially dangerous aspects of climate change. From a purely thermodynamic point of view, one would expect that the phase equilibrium in a warmer world is shifted slightly towards the gas phase, thereby increasing the amount of precipitable water (Seneviratne et al., 2021).
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