Permafrost Distribution Modeling in the Semi-arid Chilean Andes

• Main Authors: Azócar, Guillermo, Brenning, Alexander, Bodin, Xavier
• Other Authors: Department of Geography and Environmental Management Waterloo, University of Waterloo Waterloo, Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), International Permafrost Association
• Format: Conference Object
• Language: English
• Published: HAL CCSD 2016
• Subjects: [SDE]Environmental Sciences; Ice; permafrost
• Online Access: https://sde.hal.science/hal-01887949

International audience lMountain permafrost and rock glaciers in the Andes are of growing interest due to the increase in human activities in this remote area and new environmental regulations. Empirical models of mountain permafrost distribution based on the spatial analysis of intact and relict rock glaciers and Mean Annual Air Temperature (MAAT) have been established as a tool for regional-scale assessments of permafrost favorability across entire mountain ranges. In this approach, bias adjustments are made to account for differences in permafrost presence within rock glaciers and in general debris-covered high-mountain terrain (Boeckli et al., 2012). This method allows for a rapid initial assessment of favorability for the presence of mountain permafrost in data-scarce vast mountain regions. In the present study, this methodology is applied to map a Permafrost Favorability Index (PFI) throughout the semi-arid Andes of central Chile (29° S-32°S), excluding areas of exposed bedrock. For this purpose, an inventory of relict and intact rock glaciers was compiled for the study region, MAAT was regionalized based on scarce meteorological data available in the study region, especially for high altitude area, and permafrost favorability was spatially modeled empirically based on MAAT and potential incoming solar radiation (PISR). The compiled inventory includes 3575 rock glaciers in the, Huasco, Elqui, Limarí and Choapa watersheds in Central Chile (total area: 38651 km 2 , including low elevation areas), 1664 of which were classified as relict and therefore as indicative of permafrost absence; 51 rock glaciers were removed before modeling due to their exceptional locations. Glaciers in the study region are limited to the highest parts of the Elqui and Huasco catchments. The estimated total ice volume of rock glaciers in the study region is about 2.5 times as large as the total glacier ice volume (Azócar and Brenning, 2010). MAAT for the 1981-2010 period was regionalized based on 116 station-years of annual air ...