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Active layer temperature monitoring in two boreholes in Livingston Island, maritime Antarctic: first results for 2000–2006

机译:南极海上利文斯顿岛两个钻孔中的活动层温度监测:2000–2006年的初步结果

摘要

This paper describes the active layer thermal regimes in two shallow boreholes, Sofía 275 m a.s.l. and Incinerador 35 m a.s.l., for which the ground temperature series has been recorded continuously from 2000 to 2006. The monitoring sites are located in Livingston Island, South Shetland Archipelago, Antarctica. This is one of the most sensitive regions of Earth to climate change, with a major warming trend over the last 50 years, of ca. +2.5oC in the Mean Annual Air Temperatures (MAAT). This region is located near the climatic limit of permafrost, since MAAT at sea level is close to -2oC. Lineal fits of the ground temperatures series for the study period at different depths in these boreholes show positive slopes. An outcome from the analysis of freezing and thawing indexes is that most of the ground warming seems to concentrate in the summer.
机译:本文介绍了两个浅孔Sofi'a 275 m a.s.l.中的活性层热态。 2000年至2006年连续记录了地面温度序列。监测地点位于南极洲南设得兰群岛的利文斯顿岛。这是地球对气候变化最敏感的地区之一,在过去的50年中,气候变暖的主要趋势是大约年平均气温(MAAT)为+ 2.5oC。该区域位于多年冻土的气候极限附近,因为海平面上的MAAT接近-2oC。在这些井眼中不同深度的研究期间,地面温度序列的线性拟合显示出正斜率。冻融指数分析的结果是,大多数地面变暖似乎都集中在夏季。

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