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Increasing spatial extent and frequency of flash drought in Europe with each degree of global warming

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F25%3A102106" target="_blank" >RIV/60460709:41330/25:102106 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://iopscience.iop.org/article/10.1088/1748-9326/ae11c8" target="_blank" >https://iopscience.iop.org/article/10.1088/1748-9326/ae11c8</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1088/1748-9326/ae11c8" target="_blank" >10.1088/1748-9326/ae11c8</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Increasing spatial extent and frequency of flash drought in Europe with each degree of global warming

  • Popis výsledku v původním jazyce

    Flash droughts, characterised by sudden and severe development of dry soil moisture conditions, have detrimental impacts on agriculture and ecosystems. Since reliable projections of any kind of drought are crucial for drought risk mitigation, studying how these flash droughts evolve as warming increases becomes essential. Herein, we analyse changes in flash drought frequency, geographic extent, and regional variability across Europe under incremental global warming levels of 1 °C, 1.5 °C, 2 °C and 3 °C. Soil moisture simulations are obtained using the mesoscale hydrologic model (mHM), which has been forced with the bias-corrected meteorological data from ISIMIP3b (Inter-Sectoral Impact Model Intercomparison Project, phase 3b). We use a percentile-based method to determine the rapid decline in soil moisture conditions during the growing season. Our results show that Northern and Central Europe are expected to see more frequent flash drought events at higher warming levels above 1.5 °C. As temperatures increase, new areas experience flash drought in Central Europe. In contrast, the increase in frequency and area is less in the Mediterranean. Across Europe, we expect the mean frequency of flash droughts to increase from around 3 events each decade at 1 °C to 5 events at 3 °C. The median value of the spatial area covered in flash drought is expected to increase from around 30% at 1 °C to close to 44% at 3 °C. Each degree of increase in warming is expected to add around one more flash drought event each decade and more than 6% of the area across Europe under flash drought. The threshold of 1.5 °C marks a significant increase in the area affected by flash droughts, highlighting the importance of adhering to the Paris Agreement targets and adaptation measures to counter such flash drought conditions and safeguard the agricultural economy, food security, and ecosystems.

  • Název v anglickém jazyce

    Increasing spatial extent and frequency of flash drought in Europe with each degree of global warming

  • Popis výsledku anglicky

    Flash droughts, characterised by sudden and severe development of dry soil moisture conditions, have detrimental impacts on agriculture and ecosystems. Since reliable projections of any kind of drought are crucial for drought risk mitigation, studying how these flash droughts evolve as warming increases becomes essential. Herein, we analyse changes in flash drought frequency, geographic extent, and regional variability across Europe under incremental global warming levels of 1 °C, 1.5 °C, 2 °C and 3 °C. Soil moisture simulations are obtained using the mesoscale hydrologic model (mHM), which has been forced with the bias-corrected meteorological data from ISIMIP3b (Inter-Sectoral Impact Model Intercomparison Project, phase 3b). We use a percentile-based method to determine the rapid decline in soil moisture conditions during the growing season. Our results show that Northern and Central Europe are expected to see more frequent flash drought events at higher warming levels above 1.5 °C. As temperatures increase, new areas experience flash drought in Central Europe. In contrast, the increase in frequency and area is less in the Mediterranean. Across Europe, we expect the mean frequency of flash droughts to increase from around 3 events each decade at 1 °C to 5 events at 3 °C. The median value of the spatial area covered in flash drought is expected to increase from around 30% at 1 °C to close to 44% at 3 °C. Each degree of increase in warming is expected to add around one more flash drought event each decade and more than 6% of the area across Europe under flash drought. The threshold of 1.5 °C marks a significant increase in the area affected by flash droughts, highlighting the importance of adhering to the Paris Agreement targets and adaptation measures to counter such flash drought conditions and safeguard the agricultural economy, food security, and ecosystems.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10501 - Hydrology

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/GA23-08056S" target="_blank" >GA23-08056S: Sledování dynamiky vývoje suchých epizod a jejich klasifikace v globálním měřítku - DynamicDrought</a><br>

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Environmental Research Letters

  • ISSN

    1748-9326

  • e-ISSN

    1748-9326

  • Svazek periodika

    20

  • Číslo periodika v rámci svazku

    11

  • Stát vydavatele periodika

    CZ - Česká republika

  • Počet stran výsledku

    12

  • Strana od-do

    1-12

  • Kód UT WoS článku

    001599553900001

  • EID výsledku v databázi Scopus

    2-s2.0-105020671632