Intense heat in the southwestern United States broke records last summer partly because it hit in tandem with an unusually severe drought, finds a new Johns Hopkins study measuring for the first time how the two extreme weather events dangerously interacted in real time.
Though the drought’s impact on that heat wave was modest in general, it pushed up temperatures by four degrees in some areas, and the researchers say similarly dueling weather events likely drove this year’s New Mexico wildfire to historic proportions. Moreover, as climate change advances, these one-two weather punches and their inherent hazards will become increasingly common.
“With more extremes happening, the possibility of an extreme drought plus a heat wave and even a fire, together, the odds are just better that it’s going to happen,” said co-author Benjamin Zaitchik. “Understanding how a compound event can lead to a cascade where you end up in a record-shattering situation that can be really damaging for people and ecosystems is something that many climate scientists are trying to understand.”
The findings are newly published in Geophysical Research Letters.
Climate change is expected to increase extreme weather events, particularly heat waves. There is also increasing concern about more compound events, two or more weather episodes happening together, which then work together or cascade, to become record-shattering episodes.
“We’re not just going to see records fall, we’re going to see records get blown out of the water,” Zaitchik says.
The June 2021 heatwave happening at the same time as a severe drought was an opportunity to better understand exactly if and how real cascading events unite to amplify conditions.
“We had the drought. We had the heat wave on top of that. Were they really cascading?” said Zaitchik, who’s a hydroclimate scientist. “They were happening together and it was bad, but what we were able to do with our experiments is determine if it was a cascade and if it was, did that help to explain why it broke records.”
Using climate modeling and satellite images, the team measured the link between the heat wave and the drought. Or more simply put, they discovered what happened to the heat wave if they took the drought out of the picture.
The drought pushed up temperatures about a half a degree on average but in some areas, particularly forested areas, it was four degrees higher over the course of an entire week, said lead author Mahmoud Osman, also a hydroclimate scientist and a postdoctoral fellow in the university’s Morton K. Blaustein Department of Earth and Planetary Science.
The heat’s effect on the drought was harder to capture, both because the conditions were already so profoundly dry, so further drying might have been imperceptible, and because the simulations weren’t designed to capture all of the impacts that heat has on drought. Still the team found signs, not clear affirmation, that the drought elevated heat, which increased demand for evaporation, adding to the water stress of already very dry conditions.
Fires are another element that could easily become part of a heat/drought cascade, Osman and Zaitchik said, adding that it seems to already be happening this year in Texas and New Mexico.
“We now have earlier springs leading to earlier drying of the soil which leads to increased fire risk, leading to this kind of heat/drought/fire cascade that our study speaks to,” Zaitchik said, “We’re already seeing it this year and we’re going to see it every year.”
The authors also included Nathaniel Winstead, principal staff scientist at the Johns Hopkins University Applied Physics Laboratory.
The work was supported by: National Science Foundation Grant No. 1854902.
Materials provided by Johns Hopkins University. Original written by Jill Rosen. Note: Content may be edited for style and length.