We would like to draw your attention to the session GM 9.1 COLD REGIONS GEOMORPHOLOGY at the forthcoming EGU General Assembly in Vienna, 7-12 April 2013 (http://meetingorganizer.copernicus.org/EGU2013/session/11705). Please note that the deadline for abstract submission is the 9th of January 2013.
Confirmed keynote speakers are Professor Mark Bateman (University of Sheffield, UK) on 'Unpicking periglacial palimpsests' and Professor Ólafur Ingólfsson (UNIS, Svalbard) on 'Surging glaciers in Iceland - research status and future challenges'
We hope this session is of interest to you and look forward to receiving your abstract. Best wishes, Sven Lukas, Matteo Spagnolo and Isabelle Gärtner-Roer
GM 9.1 Cold regions geomorphology
Present-day glacial and periglacial processes in cold regions, i.e. arctic and alpine environments, provide modern analogues to processes and climatic changes that took place during the Pleistocene, including gradual retreat or collapse of ice sheets and mountain glaciers, and melting and shrinking of low-land permafrost. Current changes in mid-latitude mountain ranges could also serve as a proxy for future changes in arctic regions within a context of climate change (e.g. speed-up of creeping permafrost features, relictification of rock glaciers).
We invite contributions that either:
1. investigate present-day glacial and/or periglacial landforms, sediments and processes to describe the current state, to reconstruct past environmental conditions and to predict future scenarios in cold regions; or 2. have a Quaternary focus and aim at enhancing our understanding of past glacial, periglacial and paraglacial processes, also through the application of dating techniques.
Case studies that use a multi-disciplinary approach (e.g. field, laboratory and modelling techniques) and/or that highlight the interaction between the glacial, periglacial and paraglacial cryospheric components in cold regions are particularly welcome.