Net emissions from the warming Arctic may be much smaller than thought, according to a new study.
Rising global temperatures are expected to thaw Arctic permafrost, reinvigorating the microorganisms that live in the region’s carbon-rich soils. When that happens, those microbes will begin consuming the carbon stored in the permafrost and emitting massive amounts of methane, one of the most powerful greenhouse gases on the planet.
This injection of methane into the atmosphere is a concern for climate scientists worried that it will exacerbate global warming. But Purdue University scientists say that while there will likely be more methane—and still a concerning amount—the net emissions may be much smaller than expected.
Permafrost thaw increases not only methane production in Arctic wetlands but also methane consumption in upland areas, say Qianlai Zhuang, a professor in the departments of Earth, atmospheric, and planetary sciences and agronomy, and Youmi Oh, a graduate student in Zhuang’s lab.
Upland dry and mineral-based soils account for 87% of Arctic soils and are rich in microbes called methanotrophs that consume methane.
Methanotrophs waking up
“This group of bacteria utilizes atmospheric methane as an energy source,” Zhuang says. “The emissions from wetlands will potentially be quite large, but if you consider the uplands, then the area-aggregated net emissions will be much smaller than previously thought.”
Arctic organic-rich soils emit methane to the atmosphere when their methane production by methanogens is larger than the methane consumption by methanotrophs. The methanotrophs in those soils require high-level methane concentrations to survive and reproduce.
In contrast, scientists discovered novel methanotrophs in Arctic mineral uplands. These high-affinity methanotrophs require less than 1% of the methane concentration level that allows their wetland counterparts to thrive. That means they can survive and reproduce on atmospheric methane concentration levels and can pull methane from the atmosphere.
Zhuang and Oh included the role of these microorganisms in methane consumption into a biogeochemical model and found that they significantly reduce the net regional methane emissions to the atmosphere. Their results appear in the journal Nature Climate Change.
Their findings more closely resemble recent observed trends in methane levels in the Arctic where emissions have increased, but atmospheric accumulations have not increased as quickly as models had simulated.
“We do believe that Arctic methane emissions will increase by the end of this century as other studies have shown, but the net increase to the atmosphere will be much smaller once upland methanotrophs are taken into consideration,” Oh says. “It was even possible in our simulation that net emissions decrease because high-affinity methanotrophs survive better than methanogens in response to warming.”
While smaller net methane emissions sound good at first glance, Zhuang and Oh warn that the scenario would be dependent on higher global temperatures.
“We could see Arctic methanotrophs consume more methane than the region is producing, but that would require even more warming,” Zhuang says. “And it’s important to remember that this is only one part of the planet. It doesn’t account for greenhouse gases produced in other regions.”
Zhuang and Oh will continue to monitor Arctic methane emissions and improve their model. They believe they’ve added a critical component required to better understand net methane emissions, but they say that current models will need to adapt to provide more accurate projections.
“The model we use assumes that wetland and upland areas will not change in the future,” Oh says. “We know, however, that changes in temperature, precipitation, and other factors will impact areal dynamics of wetland vs. upland, thus methane emissions.”
Funding came from the NASA Interdisciplinary Research in Earth Science program and the NASA Earth and Space Science Fellowship program.
Source: Purdue University