Projecting Changes in the Drivers of Compound Flooding in Europe Using CMIP6 Models

• Published in: Earth's future 2024-05, Vol.12 (5), p.n/a
• Main Authors: Hermans, Tim H. J., Busecke, Julius J. M., Wahl, Thomas, Malagón‐Santos, Víctor, Tadesse, Michael G., Jane, Robert A., Wal, Roderik S. W.
• Format: Article
• Language: English
• Subjects: Climate models; Climate variability; Cloud computing; CMIP6 ensemble; compound flooding; Decades; Emissions; Environmental Sciences; Extreme weather; Extreme wind speeds; Flooding; Floods; Gauges; joint probability; Mathematical models; Precipitation; Probability; projections; Robustness; Simulation; Statistical analysis; statistical storm surge model; Storm surges; Storms; Stormwater management; Tidal waves; Time series; Wind speed
• ISSN: 2328-4277; 2328-4277
• DOI: 10.1029/2023EF004188

When different flooding drivers co‐occur, they can cause compound floods. Despite the potential impact of compound flooding, few studies have projected how the joint probability of flooding drivers may change. Furthermore, existing projections may not be very robust, as they are based on only 5 to 6 climate model simulations. Here, we use a large ensemble of simulations from the Coupled Model Intercomparison Project 6 (CMIP6) to project changes in the joint probability of extreme storm surges and precipitation at European tide gauges under a medium and high emissions scenario, enabled by data‐proximate cloud computing and statistical storm surge modeling. We find that the joint probability will increase in the northwest and decrease in most of the southwest of Europe. Averaged over Europe, the absolute magnitude of these changes is 36%–49% by 2080, depending on the scenario. The large‐scale changes in the joint probability of extreme storm surges and precipitation are similar to those in the joint probability of extreme wind speeds and precipitation, but locally, differences can exceed the changes themselves. Due to internal climate variability and inter‐model differences, projections based on simulations of only 5 to 6 randomly chosen CMIP6 models have a probability of higher than 10% to differ qualitatively from projections based on all CMIP6 simulations in multiple regions, especially under the medium emissions scenario and earlier in the twenty‐first century. Therefore, our results provide a more robust and less uncertain representation of changes in the potential for compound flooding in Europe than previous projections. Plain Language Summary Extreme storm surges, rainfall or river discharge can cause flooding. When these events happen at the same time, even more severe flooding may follow. Climate change could affect the odds that drivers of flooding coincide, potentially leading to larger flood risk. However, few scientists have tried to compute such changes, using only a few different computer models of our climate. Here, we use a much larger set of climate models to compute how the odds that an extreme storm surge coincides with extreme precipitation could change in the future. We find that at the coasts of northwestern Europe, those odds will increase, whereas in southwestern Europe, they will mostly decrease. On average, the changes will be as large as 36%–49% of the current odds, depending on whether the concentration of greenhouse gases in th