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Past and Present Permafrost Temperatures in the Abisko Area: Redrilling of Boreholes

机译:阿比斯库地区过去和现在的多年冻土温度:重新钻孔

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摘要

Monitoring of permafrost has been ongoing since 1978 in the Abisko area, northernmost Sweden, when measurements of active layer thickness started. In 1980, boreholes were drilled in three mires in the area to record permafrost temperatures. Recordings were made twice per year, and the last data were obtained in 2002. During the International Polar Year (2007–2008), new boreholes were drilled within the ‘Back to the Future’ (BTF) and ‘Thermal State of Permafrost’ (TSP) projects that enabled year-round temperature monitoring. Mean annual ground temperatures (MAGT) in the mires are close to 0℃, ranging from -0.16 to -0.47℃ at 5 m depth. Data from the boreholes show increasing ground temperatures in the upper and lower part by 0.4 to 1℃ between 1980 and 2002. At one mire, permafrost thickness has decreased from 15 m in 1980 to ca. 9 m in 2009, with an accelerating thawing trend during the last decade.
机译:自1978年以来,在瑞典最北端的阿比斯库地区开始进行永久冻土的监测,当时开始进行活性层厚度的测量。 1980年,在该地区的三个矿井中钻孔,以记录多年冻土温度。每年进行两次记录,最后一次数据是2002年获得的。在国际极地年(2007-2008)期间,在“回到未来”(BTF)和“多年冻土热状态”( TSP)项目可实现全年温度监控。泥潭中的平均年地面温度(MAGT)在5 m深度处接近-0,从-0.16至-0.47。钻孔数据显示,1980年至2002年之间,上部和下部的地温升高了0.4至1℃。在一个泥潭中,多年冻土层的厚度从1980年的15 m减小到了大约1 m。 2009年为900万,过去十年间解冻趋势呈加速趋势。

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