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Ninth International Conference on Permafrost ... - IARC Research

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First Results of Ground Surface Temperature Modeling in Finnmark,Northern NorwayHerman FarbrotDepartment of Geosciences, University of Oslo, Norway and Norwegian Meteorological Institute, Oslo, NorwayBernd EtzelmüllerDepartment of Geosciences, University of Oslo, NorwayKetil IsaksenNorwegian Meteorological Institute, Oslo, NorwayThomas V. SchulerNorwegian Water Resources and Energy Directorate, Oslo, NorwayOle Einar TveitoNorwegian Meteorological Institute, Oslo, NorwayHanne H. ChristiansenThe University Centre in Svalbard, L<strong>on</strong>gyearbyen, NorwayIntroducti<strong>on</strong>The main objective of the Norwegian IPY project“<strong>Permafrost</strong> Observatory Project: A C<strong>on</strong>tributi<strong>on</strong> to theThermal State of <strong>Permafrost</strong> in Norway and Svalbard” (TSPNORWAY) (http://www.tspnorway.com) is to measure andmodel the distributi<strong>on</strong> of permafrost in northern Norway andSvalbard, as well as to assess its thermal state, thickness, andinfluence <strong>on</strong> periglacial landscape-forming processes.The inner part of Finnmark (Fig. 1), the northernmostcounty of mainland Norway, is a plain, having str<strong>on</strong>gFigure 1. Locati<strong>on</strong> map showing three classes of mean annual air temperature (MAAT, 1961–1990) in Finnmark (based <strong>on</strong> Tveito et al. 2000).The dark grey shows areas where MAAT is lower than -3°C, light grey shows areas where MAAT is between -3°C, and -1°C, and white isMAAT higher than -1°C.73

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