4.6 Article

Long-term variability and trends in meteorological droughts in Western Europe (1851-2018)

期刊

INTERNATIONAL JOURNAL OF CLIMATOLOGY
卷 41, 期 -, 页码 E690-E717

出版社

WILEY
DOI: 10.1002/joc.6719

关键词

drought; instrumental period; Mediterranean; precipitation; Standardized Precipitation Index; trends; Western Europe

资金

  1. Spanish Commission of Science and Technology [PCIN-2015-220, CGL2017-82216-R]
  2. FEDER
  3. IMDROFLOOD - WaterWorks 2014
  4. AXIS (Assessment of Cross[X] - sectorial climate Impacts and pathways for Sustainable transformation) JPI-Climate
  5. FORMAS (SE)
  6. DLR (DE)
  7. BMWFW (AT)
  8. IFD (DK)
  9. MINECO (ES)
  10. ANR (FR)
  11. FCT (PT)
  12. European Union [690462]
  13. Irish Research Council COALESCE grant [COALESCE/2019/43]
  14. 'Juan de la Cierva' postdoctoral contract (Spanish Ministry of Economy and Competitiveness, MEC) [FJCI-2017-33652]
  15. Spanish Ministry of Science, Innovation and Universities [RTI2018-099711-J-I00]
  16. NERC [NE/L01016X/1, NE/L01016X/2] Funding Source: UKRI

向作者/读者索取更多资源

The study reveals that there is a general absence of statistically significant long-term trends in meteorological droughts across Western Europe, with some exceptions at specific stations. The spatial diversity of drought variability in Western Europe is strong, showing homogeneous temporal evolution in different regions. The temporal variability of drought in Western Europe is more dominant than long-term trends, indicating that long-term drought trends cannot be confirmed solely using precipitation records.
We analysed long-term variability and trends in meteorological droughts across Western Europe using the Standardized Precipitation Index (SPI). Precipitation data from 199 stations spanning the period 1851-2018 were employed, following homogenisation, to derive SPI-3 and SPI-12 series for each station, together with indices on drought duration and severity. Results reveal a general absence of statistically significant long-term trends in the study domain, with the exception of significant trends at some stations, generally covering short periods. The largest decreasing trends in SPI-3 (i.e., increasing drought conditions) were found for summer in the British and Irish Isles. In general, drought episodes experienced in the last two or three decades have precedents during the last 170 center dot years, emphasizing the importance of long records for assessing change. The main characteristic of drought variability in Western Europe is its strong spatial diversity, with regions exhibiting a homogeneous temporal evolution. Notably, the temporal variability of drought in Western Europe is more dominant than long-term trends. This suggests that long-term drought trends cannot be confirmed in Western Europe using precipitation records alone. This study provides a long-term regional assessment of drought variability in Western Europe, which can contribute to better understanding of regional climate change during the past two centuries.

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