Thawing permafrost can release nitrous oxide, also known as laughing gas, a contributor to climate change that has been largely overlooked in the Arctic
The report in the journal Nature Geoscience indicated that emissions of the gas surged under certain conditions from melting 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, which are among the main natural sources of the heat-trapping gas.
"Measurements of nitrous oxide production permafrost samples from five additional wetland sites in the high Arctic indicate that the rates of nitrous oxide production observed in the Zackenberg soils may be in the low range," the study said.
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.
It is among the gases regulated by the U.N.'s Kyoto Protocol for limiting global warming that could spur more sandstorms, floods, heatwaves and rising sea levels.
Nitrous oxide comes from human sources including agriculture, especially nitrogen-based fertilizers, and use of fossil fuels as well as natural sources in soil and water, such as microbes in wet tropical forests.
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