The 1931 Yangtze River flood in eastern China is regarded as one of the world’s deadliest natural disasters on record. the origins of this monumental flood have remained largely unexplored due to the scarcity of historical records and pre-1950s meteorological data in China.
Based on multiple lines of evidence including instrumental observations, reanalysis datasets, and simulations conducted with atmospheric general circulation models driven by historical sea surface temperatures, researchers led by Prof. ZHOU Tianjun from the Institute of Atmospheric Physics (IAP) of the Chinese Academy of Sciences have investigated the underlying mechanisms of the 1931 Yangtze River flood.
They found that the flood resulted from the combined effects of tropical El Niño–related sea surface temperature forcing and extratropical wave activities over the Eurasian continent. They also suggested that the flood was a preconditioned compound event, potentially aggravated by preceding springtime heavy precipitation.
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