New data from the Global Terrestrial Network for Permafrost (GTNP) reveal that a warming climate is accelerating thawing of the permafrost—the concrete-like frozen ground found mostly in the far Northern Hemisphere. The rising ground temperature could spell trouble for the vast new energy developments proposed for the high northern latitudes, experts say.
Tracking trends in the permafrost—soil that remains frozen for more than two years—is important because it is a sensitive record keeper of climate change, says Frederick Nelson, a physical geographer at the University of Delaware. New data from the Circumpolar Active Layer Monitoring Program, GTNP, and other monitoring programs, presented on December 13 at the American Geophysical Union meeting in San Francisco, clearly show that the permafrost is warming in response to rising air temperatures in the Arctic, he says.
The changes in the permafrost have important implications for the natural gas pipeline planned in Canada’s Mackenzie River Valley in the Northwest Territories, says Chris Burn, Natural Sciences and Engineering Research Council of Canada Northern Research Chair at Carleton University in Ottawa. The buried pipeline will carry pressurized gas, chilled to match the surrounding ground temperature. Because the pipe will travel through areas with and without permafrost, there is a risk that the pipe will be either cold or warm enough to freeze or thaw the soil. The resulting subsidence or frost heave could bend the pipe, requiring engineers to cut gas flow to prevent ruptures or institute costly repairs. Therefore, the project's engineers need to predict how permafrost responds to climate change so that they can minimize any thermal disturbance caused by the pipeline.
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Meanwhile, measurements taken from boreholes in the permafrost at Svalbard, Norway, suggest that ground temperatures have increased by an average of 0.4 °C in the past decade, which is roughly 4 times faster than in the previous century, says Charlie Harris, a permafrost scientist at the Cardiff University (U.K.). Climate warming has boosted soil temperatures in northern Russia by 1 °C over the past 60 years and has increased the thickness of the active layer—the upper surface of the permafrost that thaws in summer—by 20–30 centimeters since the 1950s, according to Tingjun Zhang, a geophysicist at the University of Colorado at Boulder. Since the late 1960s, the average temperature of permafrost in Canada’s Mackenzie River delta has warmed from –8 to –6.5 °C, Burn says. At the same time, the rising frequency of 10-day intense events of continuous sunshine combined with warm summer temperatures is triggering landslides in parts of Canada’s Arctic, explains Antoni Lewkowicz, a geomorphologist at the University of Ottawa. Meltwater at the bottom of the active layer buoys up slabs of soil nearly 650 meters long that slide off the lubricated surface. Landslides, some on slopes as gentle as 5º, have more than doubled on Ellesmere Island, from 6 per year before 1975 to about 14 per year for the past 25 years, he adds."
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http://pubs.acs.org/subscribe/journals/esthag-w/2005/mar/science/jp_permafrost.html