Methane in Arctic Lake Traced to Groundwater from Seasonal Thawing, UA Co-authored Research Shows

Toolik Lake is an Arctic lake located in the continuous permafrost zone in the northern foothills of the Brooks Range. It is the site of the University of Alaska's Toolik Field Station (Adina Paytan).
Toolik Lake is an Arctic lake located in the continuous permafrost zone in the northern foothills of the Brooks Range. It is the site of the University of Alaska’s Toolik Field Station (Adina Paytan).

SANTA CRUZ, Calif. — Global warming may ramp up the flow of methane from groundwater into Arctic lakes, allowing more of the potent greenhouse gas to bubble out into the atmosphere, according to a new study co-authored by a University of Alabama researcher.

Scientists have long known that Arctic lakes emit methane, which comes primarily from the action of microbes in the water and lake sediments. Although numerous studies have monitored and documented these emissions, few have examined the effects of seasonally thawed groundwater, which also contains methane and flows into the lakes.

Dr. Adina Paytan, a research scientist at the University of California, Santa Cruz, led a team of researchers, including Dr. Natasha Dimova, a UA assistant professor of Geological Sciences, to study methane concentrations at Toolik Lake, Alaska.

The group’s findings, published March 9 in Proceedings of the National Academy of Sciences, show that groundwater from the seasonal thawing of the “active layer” of soil above the permafrost adds significantly to the overall concentration of methane in the lake and thus influences the emission of this powerful greenhouse gas to the atmosphere.

“Methane transport from the active layer to Toolik Lake can account for a large fraction of methane emissions from this lake,” Paytan said. “This is important because warming in the Arctic may expand the active layer and increase the discharge, leading to increased emissions from Arctic lakes and driving additional global warming.”

Although carbon dioxide accounts for the vast majority of greenhouse gas emissions from human activities, methane emissions are also an important factor driving climate change. Methane doesn’t last as long in the atmosphere, but it is much more efficient than carbon dioxide at trapping heat. Pound for pound, the effect of methane on climate change is more than 20 times greater than carbon dioxide over a 100-year period, according to the Environmental Protection Agency.

“Accurate climate change predictions for the Arctic partially depend, as our paper points out, on gaining a better understanding of methane sources in this region,” said UA’s Dimova. “This research is another step in expanding our understanding of the role of groundwater in the big picture of global greenhouse budgets.”

At Toolik Lake, the researchers tracked methane concentrations concurrently with two naturally occurring elements (radon and radium) that serve as tracers for groundwater. Based on their measurements, they concluded that methane-rich groundwater may be an important and currently unrecognized contributor to methane emissions from Arctic lakes.

The study suggests that future warming in the Arctic could expand the active layer and increase methane transport to lakes, and from lakes into the atmosphere, exacerbating global warming.

In addition to Paytan and Dimova, coauthors of the paper include Alanna Lecher, Joseph Murray, and Slawek Tulaczyk at UC Santa Cruz; Katy Sparrow, Fenix Kodovska, and John Kessler at the University of Rochester.

This research was funded by the National Science Foundation.

UA’s department of geological sciences is part of the College of Arts and Sciences, the University’s largest division and the largest liberal arts college in the state. Students from the College have won numerous national awards including Rhodes Scholarships and Goldwater Scholarships.


Chris Bryant, UA media relations, 205/348-8323,; Tim Stephens, Office of Public Affairs, UC Santa Cruz,, 831-459-4352


Source: Dr. Natasha Dimova,  205/348-0256,