This blog post is the first in a series to come. Our team, the Climate & Ecosystems Change research group from the Vrije Universiteit Amsterdam, is working in collaboration with the Environmental Change Research Unit from the University of Helsinki for a summer with lots of fire field work, science, and adventure. On this journey, our first stop was the Quebec province in Canada. I’m writing this post after our last day of fieldwork here.
ABoVE
“This lake wasn’t here 50 years ago.” Katey Walter Anthony, an ecologist at the University of Alaska-Fairbanks, dips her paddle into the water as her kayak glides across the lake. “Years ago, the ground was about three meters taller and it was a spruce forest,” she says. Big Trail Lake is a thermokarst lake, which means it formed due to permafrost thaw. Permafrost is ground that stays frozen year round; the permafrost in interior Alaska also has massive wedges of actual ice locked within the frozen ground.
There’s a freezer door in the mountainside outside of Fairbanks, Alaska. Tom Douglas opens it and we step inside, breathing in cold air and musky dust as we start to walk back through time. This isn’t fantasy. It’s the Permafrost Tunnel run by the U.S. Army’s Cold Regions Research and Engineering Laboratory in Alaska, where Douglas is a Senior Scientist. Recently, Douglas led a group of scientists and pilots with NASA’s Arctic Boreal Vulnerability Experiment (ABoVE) on a tour through the Tunnel to learn about permafrost.
Huntzinger, ., et al. (2020), Evaluation of simulated soil carbon dynamics in Arctic-Boreal ecosystems, Environmental Research Letters, 15, 1-14, doi:10.1088/1748-9326/ab6784.
The Arctic is one of the fastest warming places on the planet. As temperatures rise, the perpetually frozen layer of soil, called permafrost, begins to thaw, releasing methane and other greenhouse gases into the atmosphere. These methane emissions can accelerate future warming—but to understand to what extent, we need to know how much methane may be emitted, when and what environmental factors may influence its release.
Wildfires in the Arctic often burn far away from populated areas, but their impacts are felt around the globe. From field and laboratory work to airborne campaigns and satellites, NASA is studying why boreal forests and tundra fires have become more frequent and powerful and what that means for climate forecasting, ecosystems and human health.
Climate change in the Arctic and Boreal region is unfolding faster than anywhere else on Earth, resulting in reduced Arctic sea ice, thawing of permafrost soils, decomposition of long- frozen organic matter, widespread changes to lakes, rivers, coastlines, and alterations of ecosystem structure and function. NASA's Terrestrial Ecology Program is conducting a major field campaign, the Arctic-Boreal Vulnerability Experiment (ABoVE), in Alaska and western Canada, for 8 to 10 years, starting in 2015.
A NASA-led effort to advance our ability to monitor changing Arctic and boreal ecosystems has started its second season, with the first aircraft taking flight over Alaska and northwest Canada this month.
