Amplified intensity and duration of heatwaves by concurrent droughts in China
Compound hot-dry climate extremes could lead to severer natural disasters and socio-economic impacts compared to individual events. An improved understanding of historical heatwave-drought compounds and their differences compared to heatwaves alone is needed for better predicting the occurrence and...
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Veröffentlicht in: | Atmospheric research 2021-10, Vol.261, p.105743, Article 105743 |
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Sprache: | eng |
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Zusammenfassung: | Compound hot-dry climate extremes could lead to severer natural disasters and socio-economic impacts compared to individual events. An improved understanding of historical heatwave-drought compounds and their differences compared to heatwaves alone is needed for better predicting the occurrence and impacts of extremes under a changing climate. In this study, we investigated spatiotemporal variations of heatwave-drought compounds using meteorological data from more than 2000 stations in China during 1980–2017, and compared the heatwave intensity and duration in heatwave-drought compounds with that in heatwaves alone. The annual occurrence of heatwave-drought compounds increased significantly during 1980–2017. At the national level, heatwave intensity in heatwave-drought compounds was 34.24 °C ± 4.39 °C, which was higher than that in heatwaves alone of 33.33 °C ± 4.35 °C. The occurrence of long-lasting (duration >7 days) heatwaves accounted for about 34.42% - 50.70% in heatwave-drought compounds, while this ratio was only 11.82% -21.55% in heatwaves alone. The quantitative evaluation of heatwave-drought compounds and heatwaves alone in China highlighted the amplified heatwave severity and duration in heatwave-drought compounds versus that in heatwaves alone.
•Heatwave-drought compounds occur increasingly in China since 1980s.•Heatwave intensity in heatwave-drought compound is 0.91 °C higher than heatwave alone.•Occurrence of long-lasting heatwave accounts for 41.04% in heatwave-drought compounds. |
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ISSN: | 0169-8095 1873-2895 |
DOI: | 10.1016/j.atmosres.2021.105743 |