4.6 Article

Large increases of multi-year droughts in north-western Europe in a warmer climate

期刊

CLIMATE DYNAMICS
卷 60, 期 5-6, 页码 1781-1800

出版社

SPRINGER
DOI: 10.1007/s00382-022-06373-3

关键词

Drought; Multi-year; Compound event; Climate change; Large ensemble; SMILE

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This study investigates multi-year drought events in the Rhine basin, focusing on their occurrence probability in the present and future warmer climates. The research identifies two types of multi-year drought events and shows their frequency and potential impacts. The findings indicate that summer precipitation decreases and atmospheric evaporative demand increases with future warming, leading to a doubling of event probability and longer durations. The study highlights the need for further investigation of multi-year drought hazard and vulnerability in the region to address projected trends and potential societal and ecological impacts.
Three consecutive dry summers in western Europe (2018-2019-2020) had widespread negative impacts on society and ecosystems, and started societal debate on (changing) drought vulnerability and adaptation measures. We investigate the occurrence of multi-year droughts in the Rhine basin, with a focus on event probability in the present and in future warmer climates. Additionally, we investigate the temporally compounding physical drivers of multi-year drought events. A combination of multiple reanalysis datasets and multi-model large ensemble climate model simulations was used to provide a robust analysis of the statistics and physical processes of these rare events. We identify two types of multi-year drought events (consecutive meteorological summer droughts and long-duration hydrological droughts), and show that these occur on average about twice in a 30 year period in the present climate, though natural variability is large (zero to five events can occur in a single 30 year period). Projected decreases in summer precipitation and increases in atmospheric evaporative demand, lead to a doubling of event probability at 1 degrees C additional global warming relative to present-day and an increase in the average length of events. Consecutive meteorological summer droughts are forced by two, seemingly independent, summers of lower than normal precipitation and higher than normal evaporative demand. The soil moisture response to this temporally compound meteorological forcing has a clear multi-year imprint, resulting in a relatively larger reduction of soil moisture content in the second year of drought, and potentially more severe drought impacts. Long-duration hydrological droughts start with a severe summer drought followed by lingering meteorologically dry conditions. This limits and slows down the hydrological recovery of soil moisture content, leading to long-lasting drought conditions. This initial exploration provides avenues for further investigation of multi-year drought hazard and vulnerability in the region, which is advised given the projected trends and vulnerability of society and ecosystems.

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