Geomorphological Observations of Permafrost and Ground-Ice Degradation on Deception and Livingston Islands, Maritime Antarctica

The Antarctic Peninsula is experiencing one of the fastest increases in mean annual air temperatures (ca. 2.5ºC in the last 50 years) on Earth. If the observed warming trend continues as indicated by climate models, the region could suffer widespread permafrost degradation. This paper presents field...

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Bibliographic Details
Main Authors: Gonçalo Vieira, Enrique Serrano, Miguel Ramos, Stephan Gruber, Christian Hauck, Juan José Blanco
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
active layer
Antarctic
debris flow
permafrost
thermokarst
Antarctic Peninsula
Deception Island
Hurd
Hurd peninsula
Livingston Island
The Antarctic
Antarc*
Antarctica
Ice
Thermokarst
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.6378
http://www.geo.unizh.ch/~stgruber/pubs/vieira_2008-nicop.pdf
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Summary:The Antarctic Peninsula is experiencing one of the fastest increases in mean annual air temperatures (ca. 2.5ºC in the last 50 years) on Earth. If the observed warming trend continues as indicated by climate models, the region could suffer widespread permafrost degradation. This paper presents field observations of geomorphological features linked to permafrost and ground-ice degradation at two study areas: northwest Hurd Peninsula (Livingston Island) and Deception Island along the Antarctic Peninsula. These observations include thermokarst features, debris flows, active-layer detachment slides, and rockfalls. The processes observed may be linked not only to an increase in temperature, but also to increased rainfall, which can trigger debris flows and other processes. On Deception Island some thermokarst features may be related to anomalous geothermal heat flux from volcanic activity.

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