Authors:
Rafael Caduff | Gamma Remote Sensing AG, Gümligen, Switzerland | Switzerland
Thomas Ingeman-Nielsen | Department of Civil Engineering, Technical University of Denmark
Johanna Scheer | Department of Civil Engineering, Technical University of Denmark
Dr. Tazio Strozzi | Gamma Remote Sensing AG, Gümligen, Switzerland
Penelope How | Geological Survey of Denmark and Greenland (GEUS)
Eva Mätzler | Government of Greenland, Ministry of Mineral Resources and Justice
Building in permafrost environments is challenging. For example, the bearing capacity of some permafrost soils may significantly decrease with warming and thawing due to increased unfrozen water content. Moreover, the seasonal freeze/thaw cycle of the active layer (AL) may lead to significant frost action and subsequently potential damage of infrastructure foundations.
Often, lack of equipment, time and financial resources hinder thorough surveys of the soil conditions (such as frost susceptibility), which should occur in the planning and design phase of construction projects. Additionally, permafrost degradation results in Active Layer thickness increase. This poses problems to currently stable situations where the foundations still lie within the permanently frozen and bearing-capable soils.
In the AALM4INFRAM ESA project satellite based remote sensing (Sentinel-1 InSAR and Sentinel-2 surface classification) was used together with geotechnical field surveys and geographic information systems (GIS) to
i. map the current amplitude of seasonal frost/thaw cycle induced ground movements,
ii. map frost susceptibility,
iii. estimate the permafrost degradation rate
As outcome of the project, maps showing the seasonal frost heave and the multi-annual permafrost degradation trend as a non-reversible motion component were produced for test sites at Ilulissat, Sisimiut, Kangerlussuaq and Qaanaaq. This gives a geographic overview of the soil parameters and the distribution of potentially difficult foundation soils in settlements in Greenland. Additionally, a combination of an AL-thickness estimation with a map of a measure of frost-susceptibility could be derived for Ilulissat. Data is distributed amongst important Greenlandic stakeholders on governmental, municipal and private level, from a web map platform that is also open for the public.
In general, the stakeholder-feedback was positive. Several critical areas with known permafrost-related damages were correctly mapped. Furthermore, unknown areas were identified and will be validated in the course of future site investigations for infrastructure projects.
In our contribution, we will present an overview on the methods used to derive the above stated map products from remote sensing perspective, discuss the resulting products in light of the current infrastructure damage problematic and give an outlook on future perspective of the presented approach in arctic infrastructure management.