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Thermal State of Permafrost and Active-layer Monitoring in the Antarctic : Advances During the International Polar Year 2007–2009

Vieira, Goncalo (author)
University of Lisbon, Institute of Geography and Territorial Planning
Bockheim, James (author)
University of Wisconsin, Soil Science
Guglielmin, Mauro (author)
Insubria University, DBSF
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Balks, Megan (author)
University of Waikato, Department of Earth and Ocean Sciences
Abramov, Andrey (author)
IPCABPSS RAS, Soil Cryology
Boelhouwers, Jan (author)
Uppsala universitet,Kulturgeografiska institutionen
Cannone, Nicoletta (author)
Department of Biology and Evolution, University of Ferrara
Ganzert, Lars (author)
Alfred Wegener Institute for Polar and Marine Research, Research Unit Potsdam
Gilichinsky, David A (author)
IPCABPSS RAS, Soil Cryology
Goryachkin, Sergey (author)
Russian Academy of Sciences, Institute of Geography
López-Martínez, Jerónimo (author)
Department of Geology and Geochemistry, Universidad Autónoma de Madrid
Meiklejohn, Ian (author)
Rhodes University, Department of Geography
Raffi, Rosanna (author)
Department of Sapienza University, Department of Earth Sciences
Ramos, Miguel (author)
University of Alcalá, Department of Physics
Schaefer, Carlos (author)
al University of Viçosa, Department of Soils
Serrano, Enrique (author)
University of Valladolid, Department of Geography
Simas, Felipe (author)
Federal University of Viçosa, Department of Soils
Sletten, Ronald (author)
University of Washington, Earth and Space Sciences; University of Washington, Earth and Space Sciences
Wagner, Dirk (author)
Alfred Wegener Institute for Polar and Marine Research, Research Unit Potsdam
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 (creator_code:org_t)
2010-06-08
2010
English.
In: Permafrost and Periglacial Processes. - : Wiley. - 1045-6740 .- 1099-1530. ; 21:2, s. 182-197
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Results obtained during the International Polar Year (IPY) on the thermal state of permafrost and the active layer in the Antarctic are presented, forming part of ANTPAS (‘Antarctic Permafrost and Soils’), which was one of the key projects developed by the International Permafrost Association and the Scientific Committee for Antarctic Research for the IPY. The number of boreholes for permafrost and active-layer monitoring was increased from 21 to 73 during the IPY, while CALM-S sites to monitor the active layer were increased from 18 to 28. Permafrost temperatures during the IPY were slightly below 0°C in the South Shetlands near sea-level, showing that this area is near the climatic boundary of permafrost and has the highest sensitivity to climate change in the region. Permafrost temperatures were much lower in continental Antarctica: from the coast to the interior and with increasing elevation they ranged between −13.3°C and −18.6°C in Northern Victoria Land, from −17.4°C to −22.5°C in the McMurdo Dry Valleys, and down to −23.6°C at high elevation on Mount Fleming (Ross Island). Other monitored regions in continental Antarctica also showed cold permafrost: Queen Maud Land exhibited values down to −17.8°C on nunataks, while in Novolazarevskaya (Schirmacher Oasis) at 80 m a.s.l. the permafrost temperature was −8.3°C. The coastal stations of Molodeznaya at Enderby Land showed permafrost temperatures of −9.8°C, Larsemann Hills – Progress Station in the Vestfold Hills region – recorded −8.5°C, and Russkaya in Marie Byrd Land, −10.4°C. This snapshot obtained during the IPY shows that the range of ground temperatures in the Antarctic is greater than in the Arctic. Copyright © 2010 John Wiley & Sons, Ltd.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

Keyword

permafrost temperature;active layer;Antarctica;IPY;ANTPAS
Physical geography
Naturgeografi
Geovetenskap med inriktning mot naturgeografi
Earth Science with specialization in Physical Geography

Publication and Content Type

ref (subject category)
art (subject category)

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