Articles | Volume 1, issue 2
https://doi.org/10.5194/wcd-1-675-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-1-675-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Attribution of precipitation to cyclones and fronts over Europe in a kilometer-scale regional climate simulation
Stefan Rüdisühli
CORRESPONDING AUTHOR
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Michael Sprenger
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
David Leutwyler
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Christoph Schär
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Heini Wernli
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
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17 citations as recorded by crossref.
- Fingerprints of Frontal Passages and Post‐Depositional Effects in the Stable Water Isotope Signal of Seasonal Alpine Snow F. Aemisegger et al. 10.1029/2022JD037469
- Linking Large‐Scale Circulation Descriptors to Precipitation Variability in the Northern French Alps A. Blanc et al. 10.1029/2021GL093649
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- Empirical estimate of forestation-induced precipitation changes in Europe R. Meier et al. 10.1038/s41561-021-00773-6
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- Convection‐permitting modeling with regional climate models: Latest developments and next steps P. Lucas‐Picher et al. 10.1002/wcc.731
- Meteorological history of low-forest-greenness events in Europe in 2002–2022 M. Hermann et al. 10.5194/bg-20-1155-2023
- Influence of atmospheric rivers and associated weather systems on precipitation in the Arctic M. Lauer et al. 10.5194/acp-23-8705-2023
- Iberian hydroclimate variability and the Azores High during the last 1200 years: evidence from proxy records and climate model simulations D. Thatcher et al. 10.1007/s00382-022-06427-6
- Explaining recent trends in extreme precipitation in the Southwestern Alps by changes in atmospheric influences J. Blanchet et al. 10.1016/j.wace.2021.100356
- Noah‐MP With the Generic Crop Growth Model Gecros in the WRF Model: Effects of Dynamic Crop Growth on Land‐Atmosphere Interaction K. Warrach‐Sagi et al. 10.1029/2022JD036518
- The increasing influence of atmospheric moisture transport on hydrometeorological extremes in the Euromediterranean region with global warming L. Gimeno-Sotelo et al. 10.1038/s43247-024-01787-9
- Anthropogenic warming induced intensification of summer monsoon frontal precipitation over East Asia S. Moon et al. 10.1126/sciadv.adh4195
- The climatology and nature of warm-season convective cells in cold-frontal environments over Germany G. Pacey et al. 10.5194/nhess-23-3703-2023
- Objective identification of meteorological fronts and climatologies from ERA-Interim and ERA5 P. Sansom & J. Catto 10.5194/gmd-17-6137-2024
- Extreme wet seasons – their definition and relationship with synoptic-scale weather systems E. Flaounas et al. 10.5194/wcd-2-71-2021
- Measurement report: Spatial variability of northern Iberian rainfall stable isotope values – investigating atmospheric controls on daily and monthly timescales A. Moreno et al. 10.5194/acp-21-10159-2021
Latest update: 16 Nov 2024
Short summary
Most precipitation over Europe is linked to low-pressure systems, cold fronts, warm fronts, or high-pressure systems. Based on a massive computer simulation able to resolve thunderstorms, we quantify in detail how much precipitation these weather systems produced during 2000–2008. We find distinct seasonal and regional differences, such as fronts precipitating a lot in fall and winter over the North Atlantic but high-pressure systems mostly in summer over the continent by way of thunderstorms.
Most precipitation over Europe is linked to low-pressure systems, cold fronts, warm fronts, or...