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dc.contributor.authorVieira, Goncalo
dc.contributor.authorBockheim, James
dc.contributor.authorGuglielmin, Mauro
dc.contributor.authorBalks, Megan R.
dc.contributor.authorAbramov, Jan
dc.contributor.authorCannone, Nicoletta
dc.contributor.authorGanzert, Lars
dc.contributor.authorGilichinsky, David A.
dc.contributor.authorGoryachkin, Sergey
dc.contributor.authorLópez-Martínez, Jerónimo
dc.contributor.authorMeiklejohn, Ian
dc.contributor.authorRaffi, Rossana
dc.contributor.authorRamos, Miguel
dc.contributor.authorSchaefer, Carlos
dc.contributor.authorSerrano, Enrique
dc.contributor.authorSimas, Felipe
dc.contributor.authorSletten, Ronald
dc.contributor.authorWagner, Dirk
dc.date.accessioned2010-06-16T02:50:48Z
dc.date.available2010-06-16T02:50:48Z
dc.date.issued2010
dc.identifier.citationVieira, G., Bockheim, J., Guglielmin, M., Balks, M., Abramov, J.,…, Wagner, D. (2010). Thermal state of permafrost and active-layer monitoring in the antarctic: Advances during the international polar year 2007-2009. Permafrost and Periglacial Processes, 21(2), 182-197.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/4003
dc.description.abstractResults 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.en_NZ
dc.language.isoen
dc.publisherJohn Wiley & Sons Ltden_NZ
dc.relation.urihttp://www3.interscience.wiley.com/journal/123501973/abstract?CRETRY=1&SRETRY=0
dc.subjectpermafrost temperatureen_NZ
dc.subjectactive layeren_NZ
dc.subjectAntarcticaen_NZ
dc.subjectIPYen_NZ
dc.subjectANTPASen_NZ
dc.titleThermal state of permafrost and active-layer monitoring in the antarctic: Advances during the international polar year 2007-2009en_NZ
dc.typeJournal Articleen_NZ
dc.identifier.doi10.1002/ppp.685en_NZ
dc.relation.isPartOfPermafrost and Periglacial Processesen_NZ
pubs.begin-page182en_NZ
pubs.elements-id34986
pubs.end-page197en_NZ
pubs.issue2en_NZ
pubs.volume21en_NZ


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