Analysing 23 years of warm-season derechos in France: a climatology and investigation of synoptic and environmental changes

被引:3
|
作者
Fery, Lucas [1 ,2 ]
Faranda, Davide [1 ,3 ,4 ]
机构
[1] Univ Paris Saclay, Lab Sci Climat & Environm, UMR 8212, CEA CNRS UVSQ,IPSL, F-91191 Gif Sur Yvette, France
[2] Univ Paris Saclay, SPEC, CEA, CNRS,CEA Saclay, F-91191 Gif Sur Yvette, France
[3] London Math Lab, 8 Margravine Gardens, London W6 8RH, England
[4] Sorbonne Univ, PSL Res Univ, Ecole Normale Super, Lab Meteorol Dynam,IPSL,CNRS Ecole Polytech, F-75005 Paris, France
来源
WEATHER AND CLIMATE DYNAMICS | 2024年 / 5卷 / 01期
基金
欧盟地平线“2020”;
关键词
MESOSCALE CONVECTIVE SYSTEMS; EASTERN UNITED-STATES; PART I; WEATHER; EUROPE; THUNDERSTORMS; VARIABILITY; ATTRIBUTION; EXTREMES; TRENDS;
D O I
10.5194/wcd-5-439-2024
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Derechos are severe convective storms known for producing widespread damaging winds. While less frequent than in the United States of America (USA), derechos also occur in Europe. The notable European event on 18 August 2022 exhibited gusts exceeding 200 km h - 1 , spanning 1500 km in 12 h. This study presents a first climatology of warm-season derechos in France, identifying 38 events between 2000 and 2022. Typically associated with a southwesterly mid-level circulation, warm-season derechos in France generally initiate in the afternoon and exhibit peak activity in July, with comparable frequencies in June and August. Predominantly impacting the northeast of France, these events exhibit a maximum observed frequency of 0.65 events per year, on average, within a 200 km by 200 km square region. These characteristics are similar to those observed in Germany, with notable differences seen in the USA, where frequencies can attain significantly higher values. The study also examines synoptic and environmental changes linked with analogues of the 500 hPa geopotential height patterns associated with past warm-season derechos, comparing analogues from a relatively distant past (1950-1980) with a recent period (1992-2022). For most events, a notable increase in convective available potential energy (CAPE) is observed, aligning with trends identified in previous studies for southern Europe. However, no consistent change in 0-6 km vertical wind shear is observed in the recent period. These environmental shifts align with higher near-surface temperatures, altered mid-level atmospheric flow patterns and often increased rainfall. The role of anthropogenic climate change in these changes remains uncertain, given potential influences of natural variability factors such as the El Nino-Southern Oscillation (ENSO) or the Atlantic Multidecadal Oscillation (AMO).
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页码:439 / 461
页数:23
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