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

• 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

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.