Der Effekt der globalen Erwärmung auf die submarinen Kontinentalhänge der Arktis

• Antragstellerin: Dr. Rieka Karoline Harders
• Fachliche Zuordnung: Paläontologie ; Hydrogeologie, Hydrologie, Limnologie, Siedlungswasserwirtschaft, Wasserchemie, Integrierte Wasserressourcen-Bewirtschaftung
• Förderung: Förderung von 2013 bis 2014
• Projektkennung: Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 234805511

This project aims at investigating a scientific and societal pressing subject which requires urgent attention: the geo-hazards associated with the imminent use of the Arctic Ocean under the changing conditions forced by Global Change. Due to the increasing temperatures, the Arctic region is experiencing a decline of glaciers and sea-ice. Sea-ice reduction will soon expose to exploration yet unknown seafloor and sub-seafloor geology. Given todays interest in natural resources exploitation, the Arctic regions will experience an increase in seafloor and sub-seafloor use and an accelerated development of infrastructures, especially in coastal and continental margin areas. The glacial environment of the Arctic land masses causes that physical processes along continental margins differ substantially from those at lower latitudes, where continental slopes are built with river-fed sediments and glacial influence is comparatively unimportant. Continental margins at lower latitudes are better studied because industrialized nations have previously focused their activities there. The response of the Arctic seafloor and sub-seafloor system to upcoming changes in physical oceanography and glacial conditions, and the resultant sedimentary processes are yet not understood. To evaluate the future response of the Arctic geological system to Global Change is necessary to further understand the interplay among past climate change, continental margin geology, and submarine slope stability. This project aims at filling that critical gap in understanding. The overarching goal of this project is to evaluate how the increase of temperature, within the bounds of current predictions, may change the behavior of the Arctic geological system and alter slope stability. To achieve the goal we will estimate the volume and rate of gas release into the atmosphere that might affect climate, and evaluate the potential feed back of climate change to gas-hydrate dissociation. We will analyze potential future scenarios of slope in-stability in the context of the combined effect of the removal of past ice loading, ongoing temperature change, and stability of the geological elements of the continental margin system.

• DFG-Verfahren: Forschungsstipendien
• Internationaler Bezug: Spanien
• Gastgeber: Professor Dr. Angelo Camerlenghi; Dr. Roger Urgeles