Study Finds Permafrost Warming, Monitoring Improving
Permafrost
warming continues throughout a wide swath of the Northern Hemisphere, according
to a team of scientists assembled during the recent International Polar Year.
Their findings, recently published in Permafrost and Periglacial Processes, describe the thermal state of high-latitude permafrost during the International Polar Year, 2007-2009. Vladimir Romanovsky, a professor with the snow, ice and permafrost group at the University of Alaska Fairbanks Geophysical Institute, is the lead author of the paper, which also details the significant expansion of Northern Hemisphere permafrost monitoring.
"This paper is actually pretty unique," Romanovsky says, "because it's the first time such a large geographical area has been involved in one paper."
During the International Polar Year, Romanovsky and his colleagues launched a field campaign to improve the existing permafrost-monitoring network. The permafrost thermal state is monitored with borehole sensors, which gather data from holes drilled deep into the permafrost. The researchers established nearly 300 borehole sites that serve as permafrost observatories across the polar and sub-polar regions in the Northern Hemisphere. Their work more than doubled the size of the previously existing network.
"The heart of monitoring is the measuring of temperatures in boreholes," Romanovsky says. "For permafrost temperatures, you have to be there. You have to establish boreholes."
Having data from across the circumpolar North allows scientists to analyze trends affecting permafrost. The article notes that permafrost temperatures have warmed as much as 2 degrees Celsius – about 36 degree F – from 20 to 30 years ago. They also found that permafrost near zero degrees Celsius warmed more slowly than colder permafrost. According to Romanovsky, this trend is an example of the large-scale analysis possible using data from the expanded network.
The enlarged and revamped observatory network is meant to be a building block for further research. It also has the potential to foster better modeling of future conditions, and act as an early warning system of the negative consequences of climate change in permafrost regions. That could, in turn, help policymakers and the public plan for a future with warmer permafrost.
Romanovsky, whose specialty is Russian and North American permafrost conditions, plans to keep building on the legacy of the International Polar Year. With help from a 5-year National Science Foundation grant, he continues his collaboration with American and international colleagues, establishing new borehole sites in under-sampled areas and analyzing trends evidenced by the newly available data.
The Fourth International Polar Year was a 2-year event that began in March of 2007, and focused the attention of the international research community on the Earth's polar regions.
Their findings, recently published in Permafrost and Periglacial Processes, describe the thermal state of high-latitude permafrost during the International Polar Year, 2007-2009. Vladimir Romanovsky, a professor with the snow, ice and permafrost group at the University of Alaska Fairbanks Geophysical Institute, is the lead author of the paper, which also details the significant expansion of Northern Hemisphere permafrost monitoring.
"This paper is actually pretty unique," Romanovsky says, "because it's the first time such a large geographical area has been involved in one paper."
During the International Polar Year, Romanovsky and his colleagues launched a field campaign to improve the existing permafrost-monitoring network. The permafrost thermal state is monitored with borehole sensors, which gather data from holes drilled deep into the permafrost. The researchers established nearly 300 borehole sites that serve as permafrost observatories across the polar and sub-polar regions in the Northern Hemisphere. Their work more than doubled the size of the previously existing network.
"The heart of monitoring is the measuring of temperatures in boreholes," Romanovsky says. "For permafrost temperatures, you have to be there. You have to establish boreholes."
Having data from across the circumpolar North allows scientists to analyze trends affecting permafrost. The article notes that permafrost temperatures have warmed as much as 2 degrees Celsius – about 36 degree F – from 20 to 30 years ago. They also found that permafrost near zero degrees Celsius warmed more slowly than colder permafrost. According to Romanovsky, this trend is an example of the large-scale analysis possible using data from the expanded network.
The enlarged and revamped observatory network is meant to be a building block for further research. It also has the potential to foster better modeling of future conditions, and act as an early warning system of the negative consequences of climate change in permafrost regions. That could, in turn, help policymakers and the public plan for a future with warmer permafrost.
Romanovsky, whose specialty is Russian and North American permafrost conditions, plans to keep building on the legacy of the International Polar Year. With help from a 5-year National Science Foundation grant, he continues his collaboration with American and international colleagues, establishing new borehole sites in under-sampled areas and analyzing trends evidenced by the newly available data.
The Fourth International Polar Year was a 2-year event that began in March of 2007, and focused the attention of the international research community on the Earth's polar regions.
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