Abstract

Record rainfall and severe flooding struck eastern China in the summer of 2020. The extreme summer rainfall occurred during the COVID-19 pandemic, which started in China in early 2020 and spread rapidly across the globe. By disrupting human activities, substantial reductions in anthropogenic emissions of greenhouse gases and aerosols might have affected regional precipitation in many ways. Here, we investigate such connections and show that the abrupt emissions reductions during the pandemic strengthened the summer atmospheric convection over eastern China, resulting in a positive sea level pressure anomaly over northwestern Pacific Ocean. The latter enhanced moisture convergence to eastern China and further intensified rainfall in that region. Modeling experiments show that the reduction in aerosols had a stronger impact on precipitation than the decrease of greenhouse gases did. We conclude that through abrupt emissions reductions, the COVID-19 pandemic contributed importantly to the 2020 extreme summer rainfall in eastern China.

Highlights

  • Record rainfall and severe flooding struck eastern China in the summer of 2020

  • We find that the emissions reductions during COVID‐19 enhanced the summer atmospheric convection over eastern China

  • The simulated precipitation increase is mainly contributed by the decreases in aerosols and precursor emissions (Fig. 1d), which alone account for about one-third (32%) of the observed precipitation increase relative to the 1979–2019 summer mean over eastern China

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Summary

Introduction

Record rainfall and severe flooding struck eastern China in the summer of 2020. The extreme summer rainfall occurred during the COVID-19 pandemic, which started in China in early 2020 and spread rapidly across the globe. Our model results suggest that COVID-related reduction in aerosols could have contributed to about one-third of the observed 2020 extreme summer precipitation increase in eastern China.

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