Abstract

The study of the thermal behavior of permafrost and active layer on the South Shetland Islands, in the western side of the Antarctic Peninsula (Antarctica), has been our research topic since 1991, especially after 2006 when we established different active layer thickness and ground thermal monitoring sites of the CALM and GTN-P international networks of the International Permafrost Association. Along this period, the snow cover thickness did not change at those sites, but since 2010, we observed an elongation on the snow cover duration, with similar snow onset, but a delay on the snow offset. Due to the important effects of snow cover on the ground thermal behavior, we started in late 2015 a new research project (PERMASNOW) focused on the accurate monitoring of the snow cover (duration, density, snow water equivalent and distribution), from very different approaches, including new instrumentation, pictures analysis and remote sensing on optical and radar bands. Also, this interdisciplinary and international research team intends to compare the snow cover and ground thermal behavior with other monitoring sites in the Eastern Antarctic Peninsula where the snow cover is minimum and remains approximately constant.

Highlights

  • Polar environments are characterized by extensive areas covered by ice and glaciers

  • Due to the changes observed in the snow cover thickness, we present the instrumentation and methods that we will apply to improve our monitoring of the snow cover in the years

  • The thermal profiles of the ground, based on the analyses of 2009-2014 maximum, minimum and mean temperatures at different depths in the boreholes, allows to characterize the ground temperature at each site, and to determine the active layer thickness and the permafrost thickness when it is completely crossed by the borehole

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Summary

Introduction

Polar environments are characterized by extensive areas covered by ice and glaciers. The mean seasonal air temperature can rise up to 2°C (Vieira et al, 2010; Bañon and Vasallo, 2015) It means that under these weather conditions, the frozen soils can thaw in summer, and any increase in the air temperatures due to global warming will contribute to increase the active layer and to degrade the permafrost, what could be detected by continuous monitoring. This sensibility makes this region adequate to monitor the permafrost and the active layer thermal and mechanical evolution (e.g., Bockheim, 1995; Vieira et al, 2010; Bockheim et al, 2013). Due to the changes observed in the snow cover thickness, we present the instrumentation and methods that we will apply to improve our monitoring of the snow cover in the years

Active layer and permafrost thermal monitoring in the South Shetland Islands
Frozen ground
Snow cover
Snow cover monitoring
Snow cover patterns
Remote sensing
Radar data
Findings
Conclusions
Full Text
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