Wir freuen uns über jede Rückmeldung. Ihre Botschaft geht vollkommen anonym nur an das Administrator Team. Danke fürs Mitmachen, das zur Verbesserung des Systems oder der Inhalte beitragen kann. ACHTUNG: Wir können an Sie nur eine Antwort senden, wenn Sie ihre Mail Adresse mitschicken, die wir sonst nicht kennen!
unbekannter Gast

Cutting-edge glacier and climate study in the Eastern Alps #

Sandra Braumann was awarded the DOC fellowship by the Austrian Academy of Science that provides 36 months of funding for her PhD to realize this research at the Institute of Applied Geology (IAG) in collaboration with the Lamont-Doherty Earth Observatory (Columbia University), the University of Utah and with the Austrian Geological Survey.#

Glacier and climate study in the Eastern Alps
Glacier and climate study in the Eastern Alps
Photo: BOKU

Alpine glaciers react highly sensitive to climate variations and cause – due to fluctuations – geomorphological imprints in glacial and periglacial areas, e.g. glacial polish because of detersion, and distinct moraine sequences. Moraines at elevations below the modern ice margin mark stable glacier positions in the past and indicate wetter and colder climate conditions. Detailed mapping of these landforms allows putting spatial constraints on paleo-glacier positions. In addition, numerical ages, generated by applying cosmogenic surface exposure dating using 10Be, provide information with respect to depositional ages of moraines. With a combination of both approaches, geomorphological mapping and moraine dating, ice margins will be reconstructed, thereby establishing a comprehensive geochronology of glacier advances and retreats at the Silvretta region covering the past 11.700 years, the Holocene. Results will then be implemented in a glacier model. The aim is to complement the traditional model calibration period, which is largely based on instrumental observations, with geological age data, in this way including the geological time scale in the model. In a next step, past glacier fluctuations will be reconstructed and interpreted towards a paleo-climatological context. This allows answering the question of environmental and climatological conditions necessary to produce mapped and dated moraines in the Silvretta region. If paleo-glacier positions can be modelled successfully, there are good chances to robustly estimate future glacier change implied by predicted climate scenarios, and to provide a framework to assess effects of glacier and climate change in the Silvretta region.

Sandra Braumann is conducting her research as a member of BOKU’s Quaternary group and will be supervised by Prof. Markus Fiebig, Dr. Stephanie Neuhuber and Ass. Prof. Dr. Christopher Lüthgens. Prof. Dr. Joerg M. Schaefer (Lamont-Doherty Earth Observatory), Ass. Prof. Dr. Summer Rupper (University of Utah), and Dr. Juergen Reitner (Geological Survey Austria) will be engaged in the project as external supervisor. Inatura Erlebnis Naturschau GmbH at Dornbirn provides funding to cover project costs in coordination with the provincial government (Amt der Vorarlberger Landesregierung, AbT. IVe).