IAHS2022-67
https://doi.org/10.5194/iahs2022-67
IAHS-AISH Scientific Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

The Effect of Water Vapor Originating from Land on the 2018 Drought Development in Europe

Fares Al Hasan1, Ruud van der Ent1, and Andreas Link2
Fares Al Hasan et al.
  • 1Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, Netherlands (r.j.vanderent@tudelft.nl)
  • 2Chair of Sustainable Engineering, Technical University of Berlin, Berlin, Germany

The 2018 summer drought in Europe was particularly extreme in terms of intensity and impact due to the combination of low rainfall and high temperatures. However, it remains unclear how this drought developed in time and space in such an extreme way. In this study we aimed to get a better understanding of the role of land-atmosphere interactions. More specifically, we investigated whether there was a change in water vapor originating from land, if that caused a reduction in rainfall, and by this mechanism possibly the propagation and intensification of the drought in Europe. We used a global gridded dataset of the fate of land evaporation (i.e., where it ends up as precipitation) to investigate whether the drought intensification and propagation was impacted by the reduction in water vapor transported from the regions that first experienced the drought. It was found that during the onset phase of the 2018 drought in Europe that the water vapor originating from land played an important role in mitigating the precipitation anomalies as, for example, the share of land evaporation contributing to precipitation increased from 27% (normal years) to 38% (2018) during July in West of Europe. Land evaporation played a minor role in amplifying it during the intensification phase of the drought as the share of land evaporation contribution to precipitation decreased from 23% (normal years) to 21% (2018) during August in West of Europe. These findings are somewhat in contrast to similar studies in other continents that found the land surface to play a strong amplifying role for drought development. These results were recently published here: https://doi.org/10.3390/w13202856. Speculating what this case study means for future extreme droughts in Europe, we can at least conclude that for West of Europe the positive feedback loop between drought, soil moisture, vegetation, evaporation and precipitation is still weak even under extreme circumstances, and that probably quite a severe climate changes scenario would be needed to change this.

How to cite: Al Hasan, F., van der Ent, R., and Link, A.: The Effect of Water Vapor Originating from Land on the 2018 Drought Development in Europe, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-67, https://doi.org/10.5194/iahs2022-67, 2022.