Increasing heat is expected to extend dry conditions to far more farmland and cities by the end of the century than changes in rainfall alone, researchers said.
Much of concern about future drought under global warming has focused on rainfall projections, but higher evaporation rates may also play an important role as warmer temperatures wring more moisture from the soil, even in some places where rainfall is forecasted to increase, they said.
The study estimates that 12 per cent of land will be subject to drought by 2100 through rainfall changes alone; but the drying will spread to 30 per cent of land if higher evaporation rates from the added energy and humidity in the atmosphere is considered.
An increase in evaporative drying means that even regions expected to get more rain, including important wheat, corn and rice belts in the western US and southeastern China, will be at risk of drought. The study excluded Antarctica.
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In its latest climate report, the International Panel on Climate Change (IPCC) warns that soil moisture is expected to decline globally and that already dry regions will be at greater risk of agricultural drought, researchers said.
Using two drought metric formulations, the study authors analysed projections of both rainfall and evaporative demand from the collection of climate model simulations completed for the IPCC's 2013 climate report.
If precipitation were the only consideration, these great agricultural centres would not be considered at risk of drought, researchers said.
Researchers also said that dry zones in Central America, the Amazon and southern Africa will grow larger. In Europe, the summer aridity of Greece, Turkey, Italy and Spain is expected to extend farther north into continental Europe.
"For agriculture, the moisture balance in the soil is what really matters," said study coauthor Jason Smerdon.
The study was published in the journal Climate Dynamics.