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<p>Spatiotemporal variations in thunderstorm occurrence frequency are considered here using an environmental dataset derived from ERA5 reanalysis data. Interannual variability in the thunderstorm environments is examined for the period 1979–2023, with the standard deviation and coefficient of variation showing considerable spatial differences through the world. Atmospheric and oceanic modes of climate variability account for some of this interannual variability, particularly for the El Niño-Southern Oscillation through tropical and maritime regions, as well as to a lesser degree for the Indian Ocean Dipole, Arctic Oscillation and Antarctic Oscillation. Long-term trends can also contribute to interannual variability, with results showing increases are more common than decreases in the thunderstorm environments through the study region over the period 1979–2023. Analysis from an ensemble of global climate models shows increases in thunderstorm environments throughout most of the world, of about 29% on average per degree Celsius of global warming, indicating more favorable conditions for thunderstorms in a warmer world. The study findings are intended to be complementary to other studies and contribute as part of a broader range of information available on thunderstorms and climate variability.</p>

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Climatological variability of a thunderstorm environment dataset in tropical and temperate regions

  • 期刊论文

  • 出版模式：

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  • 发表日期：

    2026年2月5日

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  • Andrew Dowdy,
  • Andrew Brown,
  • Todd P. Lane,
  • Mateusz Taszarek

摘要

Spatiotemporal variations in thunderstorm occurrence frequency are considered here using an environmental dataset derived from ERA5 reanalysis data. Interannual variability in the thunderstorm environments is examined for the period 1979–2023, with the standard deviation and coefficient of variation showing considerable spatial differences through the world. Atmospheric and oceanic modes of climate variability account for some of this interannual variability, particularly for the El Niño-Southern Oscillation through tropical and maritime regions, as well as to a lesser degree for the Indian Ocean Dipole, Arctic Oscillation and Antarctic Oscillation. Long-term trends can also contribute to interannual variability, with results showing increases are more common than decreases in the thunderstorm environments through the study region over the period 1979–2023. Analysis from an ensemble of global climate models shows increases in thunderstorm environments throughout most of the world, of about 29% on average per degree Celsius of global warming, indicating more favorable conditions for thunderstorms in a warmer world. The study findings are intended to be complementary to other studies and contribute as part of a broader range of information available on thunderstorms and climate variability.