The PolyU study, published in Nature Communications, found that southeast China – the region spanning from the Yangtze River Delta to Hainan province – is at a higher risk of experiencing more rapid drying, with an increase in the proportion of flash droughts developed within five days by as much as 18.67 per cent during 2000 – 2020. Ordinary droughts usually take five to six months or an even longer time to develop to full strength.
Dr WANG Shuo, Assistant Professor of PolyU’s Department of Land Surveying and Geo-Informatics, who led the research, said the nature of flash droughts, characterised by rapid onset in less than a month and a fast depletion of water availability, means there are less early warning indicators for impact preparation, potentially causing more severe impacts on agriculture and society than slowly evolving droughts.
“Flash drought occurrence is often accompanied by above-average temperatures and a precipitation deficit, which may trigger compound extreme events such as the concurrence of flash drought and heat wave. Thus, flash droughts can pose even more serious threats to urbanised areas like Hong Kong due to the urban heat island effect,” he said.
The in-depth analysis was devised to address the following scientific questions: how fast flash droughts evolve and why. In the study, the research team mapped the onset timescales of flash droughts globally and the causes of the rapid onset speed, providing valuable insights for policymakers and stakeholders on the potential risks of flash droughts, and an impetus for innovators to advance flash drought forecasts and early warning systems.
Based on different data sets that use satellite soil moisture measurements, the study found that although flash droughts are not becoming more frequent in most parts of the world, they are developing at a faster rate (i.e. in a shorter period of time). Out of all flash droughts that occurred in the past two decades, these data sets showed that there was about 33.64 – 46.18 per cent of flash droughts that developed within five days, representing an increase of 3.23 – 19.03 per cent during the period.
Such adverse climate events tend to occur in humid and semi-humid regions, including Southeast Asia, East Asia, the Amazon Basin, eastern North America and southern South America. Atmospheric aridity – caused by high temperature, low precipitation and a high vapour pressure deficit (VPD) – is likely to trigger flash droughts, the study indicates.
Dr Wang explained that “atmospheric aridity creates a perfect condition for the occurrence of flash droughts, and the joint influence of soil moisture depletion and atmospheric aridity further reinforces the rapid onset of flash droughts. In other words, low soil moisture combined with a high vapour pressure deficit accelerates the decline in soil moisture through land–atmosphere feedback loops. Thus, southeast China with strong land–atmosphere coupling is more vulnerable to flash droughts.”
Compared with traditional, slowly developing droughts, flash droughts evolve with a relatively fast depletion of soil moisture that may cause an imbalance of ecosystems and agricultural systems. The flash drought in the summer of 2012 led to an estimated US$35.7 billion in losses of corn crops in the central United States.
“Governments and the public should realise the increasing flash drought risk in addition to commonly known extreme weather events, and adapt to such emerging climate-induced natural disasters. It is crucial to improve traditional drought monitoring systems and indicators for capturing rapidly evolving flash droughts,” Dr Wang said.
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