Permafrost threatened by rapid retreat of Arctic sea ice, study finds

Jun 10, 2008

The rate of climate warming over northern Alaska, Canada, and Russia could more than triple during periods of rapid sea ice loss, according to a new study led by the National Center for Atmospheric Research (NCAR). The findings raise concerns about the thawing of permafrost, or permanently frozen soil, and the potential consequences for sensitive ecosystems, human infrastructure, and the release of additional greenhouse gases.

"Our study suggests that, if sea-ice continues to contract rapidly over the next several years, Arctic land warming and permafrost thaw are likely to accelerate," says lead author David Lawrence of NCAR.

The study, by scientists from NCAR and the National Snow and Ice Data Center, will be published Friday in Geophysical Research Letters. It was funded by the U.S. Department of Energy and by the National Science Foundation.

The research was spurred in part by events last summer, when the extent of Arctic sea ice shrank to more than 30 percent below average, setting a modern-day record. From August to October last year, air temperatures over land in the western Arctic were also unusually warm, reaching more than 4 degrees Fahrenheit (2 degrees Celsius) above the 1978-2006 average and raising the question of whether or not the unusually low sea-ice extent and warm land temperatures were related.

To investigate this question, Lawrence and his colleagues analyzed climate change simulations generated by the NCAR-based Community Climate System Model. Previous analysis of these simulations suggested that a sustained period of rapid ice loss lasting roughly 5 to 10 years can occur when the ice thins enough. During such an event, the model revealed, the minimum sea-ice extent can drop by an area greater than the size of Alaska and Colorado combined.

The team found that during episodes of rapid sea-ice loss, the rate of Arctic land warming is 3.5 times greater than the average 21st century warming rates predicted in global climate models. While this warming is largest over the ocean, the simulations suggest that it can penetrate as far as 900 miles inland. The simulations also indicate that the warming acceleration during such events is especially pronounced in autumn. The decade during which a rapid sea-ice loss event occurs could see autumn temperatures warm by as much as 9 degrees F (5 degrees C) along the Arctic coasts of Russia, Alaska, and Canada.

Lawrence and his colleagues then used the model to study the influence of accelerated warming on permafrost and found that in areas where permafrost is already at risk, such as central Alaska, a period of abrupt sea-ice loss could lead to rapid soil thaw. This situation, when summer thaw extends more deeply than the next winter's freeze, can lead to a talik, which is a layer of permanently unfrozen soil sandwiched between the seasonally frozen layer above and the perennially frozen layer below. A talik allows heat to build more quickly in the soil, hastening the long-term thaw of permafrost.

Potential impacts on greenhouse gases

Arctic soils are believed to hold 30 percent or more of all the carbon stored in soils worldwide. Although researchers are uncertain what will happen to this carbon as soils warm and permafrost thaws, one possibility is that the thaw will initiate significant additional emissions of carbon dioxide or the more potent greenhouse gas, methane.

About a quarter of the Northern Hemisphere's land contains permafrost, defined as soil that remains below 32 degrees F (0 degrees C) for at least two years. Recent warming has degraded large sections of permafrost, with pockets of soil collapsing as the ice within it melts. The results include buckled highways, destabilized houses, and "drunken forests" of trees that lean at wild angles.

"An important unresolved question is how the delicate balance of life in the Arctic will respond to such a rapid warming," Lawrence says. "Will we see, for example, accelerated coastal erosion, or increased methane emissions, or faster shrub encroachment into tundra regions if sea ice continues to retreat rapidly?"

The study sheds light on how interconnected the Arctic system is, says co-author Andrew Slater, a scientist at the National Snow and Ice Data Center (NSIDC). "The loss of sea ice can trigger widespread changes that would be felt across the region."

Source: National Center for Atmospheric Research

Explore further: New, tighter timeline confirms ancient volcanism aligned with dinosaurs' extinction

add to favorites email to friend print save as pdf

Related Stories

$58 million effort to study potential new energy source

Oct 22, 2014

A research team led by The University of Texas at Austin has been awarded approximately $58 million to analyze deposits of frozen methane under the Gulf of Mexico that hold enormous potential to increase ...

NASA air campaigns focus on Arctic climate impacts

Sep 17, 2014

Over the past few decades, average global temperatures have been on the rise, and this warming is happening two to three times faster in the Arctic. As the region's summer comes to a close, NASA is hard at ...

Recommended for you

Improving forecasts for rain-on-snow flooding

6 hours ago

Many of the worst West Coast winter floods pack a double punch. Heavy rains and melting snow wash down the mountains together to breach riverbanks, wash out roads and flood buildings.

The Greenland Ice Sheet: Now in HD

7 hours ago

The Greenland Ice Sheet is ready for its close-up. The highest-resolution satellite images ever taken of that region are making their debut. And while each individual pixel represents only one moment in time, ...

User comments : 4

Adjust slider to filter visible comments by rank

Display comments: newest first

googleplex
3.7 / 5 (7) Jun 10, 2008
What I find the most interesting is the rise in sea levels (20feet ) if greenland melts, or part of antarctica melt. In addition the release of methane is a huge unkown. I have heard of vast quatities in the sea bed that will be released as the sea temperature increases.
Having seen some ice shelfs completely disappear in antarctica in a matter of months one has to say that change can be almost chaotic in nature.
Do the rainforrest act as a sponge buffer for water. As they disappear more water is free to run off, instead of being soaked up by plants and organic material.
aufever
1.8 / 5 (5) Jun 11, 2008
I recently watched something on either the Discovery Channel or History Channel and this female Scientist was holding up a sample of Permafrost that had melted in on area of Alaska and it had roots in it, so apparently it had not always been frozen and she was trying to portray this as a sign that it was man caused Global Warming, so how did the roots get there if this was truly Permanent Permafrost? I believe there is enough historical evidence that is was warmer before 1300 than it is now.
malky
5 / 5 (2) Jun 11, 2008
Sorry you've got me there. If the female scientist was holding a sample of melted permafrost then it is highly likely it has roots because they grew AFTER it melted? Now we have a wonderful thing called carbon dating for organic material. If the permafrost was not permafrost pre 1300 then any organic material can be dated to prove this.....has it? Surely the skeptics would be desperatly trying to do this to prove their point, why aren't they? The same method is used to prove that the excess CO2 is is due to fossil fuels by the way.....think about it carefully.
jeffsaunders
not rated yet Jul 08, 2008
I think it is pretty obvious that if the ice melts on the water then the ice will melt on the land faster.

Probably take a primary school kid 10 m inutes to work it out given the obvious statement the research is based on.

I have seen plenty of studies that have stated the exact same thing so I am bemused as to what is actually new in the research.

Please sign in to add a comment. Registration is free, and takes less than a minute. Read more

Click here to reset your password.
Sign in to get notified via email when new comments are made.