2012年9月1日- 2014年8月31日斯匹次卑尔根半岛西北部kaffe øyra平原地表热状态

Pub Date : 2016-06-03 DOI:10.1515/bgeo-2016-0005
A. Araźny, R. Przybylak, M. Kejna
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引用次数: 0

摘要

本文介绍了2012年9月1日至2014年8月31日在斯匹次卑尔根半岛西北部kaffe约yra平原地下1 ~ 100 cm的地温测量结果。热条件的观测是在三个地点进行的,这些地点位于典型的极地生态环境:海滩、冻土带和冰碛上。将kaffe约yra平原的地温测量结果与Ny-Ålesund附近气象站的天气条件观测结果进行了比较。分析了地温的年变率、季节变率和日变率。这反映了当时的主要气象条件。不同生态区的地表热条件存在显著差异,这主要是由于地表的形态多样性、含水率、植被和积雪以及永久冻土层的深度。
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Ground thermal regime on the Kaffiøyra Plain (NW Spitsbergen) in the period from 1 September 2012 to 31 August 2014
Abstract The article presents the results of ground temperature measurements taken at 1 cm to 100 cm below ground level on the Kaffiøyra Plain (NW Spitsbergen) from 1 September 2012 to 31 August 2014. Observations of thermal conditions were carried out at three sites located in characteristic polar ecotopes: on a beach, in tundra and on a moraine. The results of ground temperature measurements for the Kaffiøyra Plain were compared to the observations of weather conditions at the nearby meteorological station in Ny-Ålesund. The variability of ground temperature was analysed in annual, seasonal and diurnal courses. These reflected the prevailing meteorological conditions at the time. Substantial differences in ground thermal conditions were found between the ecotopes, which was due to the morphological diversity of the ground, its moisture content, vegetation and snow cover, as well as the depth of the permafrost.
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