In the future, should we try to fight climate change by spraying sulfur dioxide into the upper atmosphere to form a cloud that cools the Earth (a process called geoengineering), ending that plan abruptly could have severe, planet-wide effects on animals and plants, researchers argue in a new paper.
“Imagine large droughts or floods around the world that could be blamed on geoengineering, and demands that it stop. Can we ever risk that?”
“Rapid warming after stopping geoengineering would be a huge threat to the natural environment and biodiversity,” says paper coauthor Alan Robock, a professor in the environmental sciences department at Rutgers University.
“If geoengineering ever stopped abruptly, it would be devastating, so you would have to be sure that it could be stopped gradually, and it is easy to think of scenarios that would prevent that,” Robock says. “Imagine large droughts or floods around the world that could be blamed on geoengineering, and demands that it stop. Can we ever risk that?”
Geoengineering means attempting to control the climate in addition to stopping the burning of fossil fuels, the main cause of global warming, Robock says. While scientists have studied the climate impacts of geoengineering in detail, they know almost nothing about its potential impacts on biodiversity and ecosystems, the study notes.
The geoengineering idea that’s attracted the most attention is to create a sulfuric acid cloud in the upper atmosphere as large volcanic eruptions do, Robock says. The cloud, formed after airplanes spray sulfur dioxide, would reflect solar radiation and cool the planet. But airplanes would have to continuously fly into the upper atmosphere to maintain the cloud because it would last only about a year if spraying stopped, Robock says. He adds that the airplane spraying technology may be developed within a decade or two.
In their study, the scientists used a global scenario with moderate cooling through geoengineering, and looked at the impacts on land and in the ocean from suddenly stopping it. They assumed that airplanes would spray 5 million tons of sulfur dioxide a year into the upper atmosphere at the Equator from 2020 to 2070. That’s the annual equivalent of about one quarter of the sulfur dioxide ejected during the 1991 eruption of Mount Pinatubo in the Philippines, Robock says.
The spraying would lead to an even distribution of sulfuric acid clouds in the Northern and Southern Hemispheres. And that would lower the global temperature by about 1 degree Celsius (about 1.8 degrees Fahrenheit)—about the level of global warming since the Industrial Revolution began in the mid-1800s. But halting geoengineering would lead to rapid warming—10 times faster than if geoengineering had not been deployed, Robock says.
The scientists then calculated how fast organisms would have to move to remain in the climate—in terms of both temperature and precipitation—that they are accustomed to and could survive in, he says.
“In many cases, you’d have to go one direction to find the same temperature but a different direction to find the same precipitation,” Robock says. “Plants, of course, can’t move reasonably at all. Some animals can move and some can’t.”
He notes that national parks, forests, and wildlife refuges serve as sanctuaries for animals, plants, and other organisms. But if rapid warming forced them to move, and even if they could move fast enough, they may not be able find places with enough food to survive, he says.
One surprising side effect of rapidly starting geoengineering would be an El Niño warming of the sea surface in the tropical Pacific Ocean, which would cause a devastating drought in the Amazon, he says.
“We really need to look in a lot more detail at the impact on specific organisms and how they might adapt if geoengineering stops suddenly,” he says.
The study appears online today in Nature Ecology & Evolution.
Additional coauthors of the paper are from Rutgers University, the University of Maryland, Yale University, and Stony Brook University.
Source: Rutgers University
Publisher: Princeton University Press
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