Thawing permafrost can release nitrous oxide, also known as laughing gas, a contributor to climate change that has been largely overlooked in the Arctic, a study from B. Eberling, H. H. Christiansen and B. U. Hansen showed in Nature Geoscience.
The report in the journal Nature Geoscience indicated that emissions of the gas surged under certain conditions from thawing permafrost that underlies about 25 percent of land in the Northern Hemisphere.
Emissions of the gas measured from thawing wetlands in Zackenberg in eastern Greenland leapt 20 times to levels found in tropical forests under thawing conditions.
The scientists, from Denmark and Norway, studied sites in Canada and Svalbard off northern Norway alongside their main focus on Zackenberg. The releases would be a small addition to known impacts of global warming.
Nitrous oxide is the third most important greenhouse gas from human activities, dominated by carbon dioxide ahead of methane.
The scientists said that past studies had reckoned that carbon dioxide and methane were released by a thaw of permafrost while nitrous oxide stayed locked up.
“Thawing and drainage of the soils had little impact on nitrous oxide production,” Nature said in a statement of the study led by Bo Elberling of Copenhagen University.
“However, re-saturation of the drained soils with meltwater from the frozen soils — as would happen following thawing — increased nitrous oxide production by over 20 times,” it said.
“Nearly a third of the nitrous oxide produced in this process escaped into the atmosphere,” it added.
Text from REUTERS. Link to the paper