Observations on permafrost ground thermal regimes from Antarctica and the Italian Alps, and their relevance to global climate change
Active-layer monitoring and the permafrost thermal regime are key indicators of climate change. The results of 3 years (1997-1999) of active-layer monitoring at one high-mountain site (La Foppa, 46degrees28' 42" N; 10degrees11' 18" E, 2670 m a.s.l.) and at one Antarctic site (Bou...
| Published in: | Global and Planetary Change |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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2004
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| Online Access: | http://hdl.handle.net/11383/1707910 https://doi.org/10.1016/S0921-8181(03)00106-1 |
| Summary: | Active-layer monitoring and the permafrost thermal regime are key indicators of climate change. The results of 3 years (1997-1999) of active-layer monitoring at one high-mountain site (La Foppa, 46degrees28' 42" N; 10degrees11' 18" E, 2670 m a.s.l.) and at one Antarctic site (Boulder Clay, 74degrees44' 45" S; 164degrees01' 17" E, 205 m a.s.l) are presented. The initial analysis of a thermal profile in a borehole (100.3 m deep) within mountain permafrost at Stelvio (3000 m a.s.l., 46degrees30' 59"N; 10degrees28' 35" E) is also presented. At the alpine site, the active-layer thickness variations (between 193 and 229 cm) relate to both the snow cover and to the air temperature changes. By contrast, at the Antarctic site, there is a strong direct linkage only between air temperature fluctuations and active-layer variations. At the alpine (La Foppa) site, the relationship between climate and active-layer thickness is complicated by thermal offset that is almost negligible at both the Stelvio and Antarctic sites. The permafrost temperature profile at Stelvio site contains a climate signal suitable for paleoclimate reconstruction. The permafrost at this site has a mean annual ground surface temperature (MAGST) of - 1.9degreesC (during 1998/1999), an active layer of about 2.5 in thick and a total thickness of - 200 m. Analysis of the MAGST history, obtained by applying a simple heat conduction one-dimensional model, revealed the occurrence of a cold period from 1820 to 1940 followed by a warming period until 1978. Since the beginning of the 1980s, temperature dropped (less than 2degreesC) until the middle 1990s, when a new period of warming started. All these climatic changes fit well with the glacial fluctuations in the area and with other paleoclimatic information derived from different proxy data |
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