In North America and Europe, cropland that had a 32% annual chance of a flash drought a few years ago could have as much as a 53% annual chance of a flash drought by the final decades of this century. The result would put food production, energy and water supplies under increasing pressure. The cost of damage will also rise. A flash drought in the Dakotas and Montana in 2017 caused US$2.6 billion in agricultural damage in the U.S. alone.
How flash droughts develop
All droughts begin when precipitation stops. What’s interesting about flash droughts is how fast they reinforce themselves, with some help from the warming climate.
When the weather is hot and dry, soil loses moisture rapidly. Dry air extracts moisture from the land, and rising temperatures can increase this “evaporative demand.” The lack of rain during a flash drought can further contribute to the feedback processes.
Under these conditions, crops and vegetation begin to die much more quickly than they do during typical long-term droughts.
Global warming and flash droughts
In our new study, we used climate models and data from the past 170 years to gauge the drought risks ahead under three scenarios for how quickly the world takes action to slow global warming.
If greenhouse gas emissions from vehicles, power plants and other human sources continue at a high rate, we found that cropland in much of North America and Europe would have a 49% and 53% annual chance of flash droughts, respectively, by the final decades of this century. Globally, the largest projected increases would be in Europe and the Amazon.
Slowing emissions can reduce the risk significantly, but we found flash droughts would still increase by about 6% worldwide under a low-emissions scenario.
Timing is everything for agriculture
We’ve lived through a number of flash drought events, and they’re not pleasant. People suffer. Farmers lose crops. Ranchers may have to sell off cattle. In 2022, a flash drought slowed barge traffic on the Mississippi River, which carries more than 90% of U.S. agriculture exports.
If a flash drought occurs at a critical point in the growing season, it could devastate an entire crop.
Corn, for example, is most vulnerable during its flowering phase, called silking. That typically happens in the heat of summer. If a flash drought occurs then, it’s likely to have extreme consequences. However, a flash drought closer to harvest can actually help farmers, as they can get their equipment into the fields more easily.
In the southern Great Plains, winter wheat is at its highest risk during seeding, in September to October the year before the crop’s spring harvest. When we looked at flash droughts in that region during that fall seeding period, we found greatly reduced yields the following year.
Looking globally, paddy rice, a staple for more than half the global population, is at risk in northeast China and other parts of Asia. Other crops are at risk in Europe.
Ranches can also be hit hard by flash droughts. During the huge flash drought in 2012 in the central U.S., cattle ran out of forage and water became scarcer. If rain doesn’t fall during the growing season for natural grasses, cattle don’t have food, and ranchers may have little choice but to sell off part of their herds. Again, timing is everything.
It’s not just agriculture. Energy and water supplies can be at risk, too. Europe’s intense summer drought in 2022 started as a flash drought that became a larger event as a heat wave settled in. Water levels fell so low in some rivers that power plants shut down because they couldn’t get water for cooling, compounding the region’s problems. Events like those are a window into what countries are already facing and could see more of in the future.
Not every flash drought will be as severe as what the U.S. and Europe saw in 2012 and 2022, but we’re concerned about what may be ahead.
Can agriculture adapt?
One way to help agriculture adapt to the rising risk is to improve forecasts for rainfall and temperature, which can help farmers as they make crucial decisions, such as whether they’ll plant or not.
When we talk with farmers and ranchers, they want to know what the weather will look like over the next one to six months. Meteorology is pretty adept at short-term forecasts that look out a couple of weeks, and at longer-term climate forecasts using computer models. But flash droughts evolve in a midrange window of time that is difficult to forecast.
Increasing awareness can also help. If short-term forecasts show that an area is not likely to get its usual precipitation, that should immediately set off alarm bells. If forecasters are also seeing the potential for increased temperatures, that heightens the risk for a flash drought’s developing.
Nothing is getting easier for farmers and ranchers as global temperatures rise. Understanding the risk from flash droughts will help them, and anyone concerned with water resources, manage yet another challenge of the future.
Jeff Basara is an associate professor at the University of Oklahoma. Jordan Christian is a postdoctoral researcher in meteorology in the Climate, Hydrology, Ecosystems, Weather Research Group. Through its opinion section, Kansas Reflector works to amplify the voices of people who are affected by public policies or excluded from public debate. Find information, including how to submit your own commentary, here.
Our stories may be republished online or in print under Creative Commons license CC BY-NC-ND 4.0. We ask that you edit only for style or to shorten, provide proper attribution and link to our web site. Please see our republishing guidelines for use of photos and graphics.
Jeff Basara is an associate professor at the University of Oklahoma and has a joint appointment between the School of Meteorology and the School of Civil Engineering and Environmental Science. His specific research interests are focused on the integration of our understanding across weather, climate, water, and ecosystems with a specific focuses on processes that drive environmental extremes and associated impacts. This includes (flash) drought, excessive precipitation and floods, land-atmosphere interactions, the physical processes which impact the development of the planetary boundary layer, urban meteorology, severe weather, and the development, validation, and improvement of instrumentation and models that improve monitoring and predictability of extreme events.