Ninth International Conference on Permafrost ... - IARC Research
Ninth International Conference on Permafrost ... - IARC Research
Ninth International Conference on Permafrost ... - IARC Research
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TSP NORWAY – Thermal M<strong>on</strong>itoring of Mountain <strong>Permafrost</strong> in Northern NorwayKetil IsaksenNorwegian Meteorological Institute, Oslo, NorwayHerman FarbrotDepartment of Geosciences, University of Oslo, NorwayBernd EtzelmüllerDepartment of Geosciences, University of Oslo, NorwayHanne H. ChristiansenThe University Centre in Svalbard, L<strong>on</strong>gyearbyen, NorwayLars Harald Blikra<str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> Centre for Geohazards, Oslo, NorwayKirsti MidttømmeGeological Survey of Norway, Tr<strong>on</strong>dheim, NorwayJan Steinar RønningGeological Survey of Norway, Tr<strong>on</strong>dheim, NorwayIntroducti<strong>on</strong><strong>Permafrost</strong> is widespread in the higher mountains ofNorway. Extensive studies in southern Norway show thatthe lower regi<strong>on</strong>al altitudinal limit of mountain permafrostis str<strong>on</strong>gly correlated with the mean annual air temperature(MAAT) and decreases eastward with increasingc<strong>on</strong>tinentality (e.g., Etzelmüller et al. 2008). However, lessinformati<strong>on</strong> is available <strong>on</strong> the distributi<strong>on</strong> of permafrost innorthern Norway, where most investigati<strong>on</strong>s have focused<strong>on</strong> periglacial geomorphology and, in particular, palsas(Isaksen et al. 2008 and references therein).In 2002 a permafrost m<strong>on</strong>itoring program was initiated inTroms and Finnmark, which are the two northernmost countiesof mainland Norway. A series of miniature temperaturedataloggers (MTDs) were installed for m<strong>on</strong>itoring groundsurface and air temperatures (Isaksen et al. 2008). A griddedmean annual air temperature map indicates a altitudinalgradient for disc<strong>on</strong>tinuous permafrost in northern Norway,decreasing from over 1000 m a.s.l. in coastal sites down tobelow 400 m a.s.l. in the interior and more c<strong>on</strong>tinental areas(Etzelmüller et al. 2008).In March 2007, the Norwegian-founded 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) was started. In the following, the project isbriefly described, and the first results from borehole thermalprofiles are presented.The TSP Norway ProjectThe Norwegian-funded IPY project “<strong>Permafrost</strong>Observatory Project: A C<strong>on</strong>tributi<strong>on</strong> to the Thermal Stateof <strong>Permafrost</strong> in Norway and Svalbard” (TSP NORWAY;Christiansen et al. 2007) is a part of the internati<strong>on</strong>al IPYfull project “<strong>Permafrost</strong> Observatory Project: A C<strong>on</strong>tributi<strong>on</strong>to the Thermal State of <strong>Permafrost</strong> (TSP).” TSP will obtain a“snapshot” of the permafrost envir<strong>on</strong>ments as a benchmarkagainst which to assess past and future changes by makingstandardized temperature measurements in existing and newboreholes throughout the World’s permafrost regi<strong>on</strong>s. Theultimate payoff is l<strong>on</strong>g-term and will serve as validati<strong>on</strong>of current models and understanding of how permafrostc<strong>on</strong>diti<strong>on</strong>s are reacting to climate change. Thawing ofpermafrost in Norway may lead to subsidence of the groundsurface, having a substantial impact, for example, <strong>on</strong>infrastructure and <strong>on</strong> the stability of mountain slopes.The main objective of TSP NORWAY is to measure andmodel the permafrost distributi<strong>on</strong> in northern Norway andSvalbard, including its thermal state, thickness, and influence<strong>on</strong> periglacial landscape-forming processes.Establishment of High Altitude BoreholesNine 7–31 m deep boreholes were drilled in bedrock inTroms and Finnmark in August and September 2007. In twoof the boreholes, a measurement setup with 15–20 thermistorsc<strong>on</strong>nected to dataloggers and snow depth sensors, with datarecording every six hours, was installed. In <strong>on</strong>e of theseboreholes (Kistefjellet) the data are transferred by a modemenabling <strong>on</strong>line presentati<strong>on</strong>. The other seven and twoexisting boreholes were instrumented with MTDs at selecteddepths. All boreholes were cased. Periodic recalibrati<strong>on</strong> ofthe installed thermistors is possible, and the holes remainaccessible for other probes in the future. Furthermore, aseries of MTDs were installed for m<strong>on</strong>itoring surface and airtemperatures at selected sites.ResultsThe first estimate of mean ground temperature (MGT)near the bottom of the boreholes is presented in Table 1.<strong>Permafrost</strong> is presumably present in <strong>on</strong>e of the boreholes(Guolasjavri 1, Fig. 1). In the remaining boreholes, MGT isnear or slightly above 0°C. Snow cover c<strong>on</strong>diti<strong>on</strong>s seem tobe decisive for the permafrost distributi<strong>on</strong> in the investigatedaltitude ranges. In additi<strong>on</strong> sediment-covered ground may insome cases experience permafrost c<strong>on</strong>diti<strong>on</strong>s due to thermal111