A factor related to the atmosphere could influence the increase in the severity of droughts
Atmospheric evaporative demand is a measure of the atmosphere's ability to extract moisture from the soil and influences the availability of water on the Earth's surface. An international team has analysed global drought data from 1901 to 2022 and found that this demand has contributed to a 40% increase in drought severity since 1981. Furthermore, this trend is accelerating and will most likely continue due to climate change, according to the authors. The results are published in the journal Nature.