current team of the Permafrost Research Section Head of Section Prof. Dr. Guido Grosse Deputy Head of Section Prof. Dr. Hugues Lantuit Dr. Claire Treat Assistant Melanie Reinhardt Senior Scientists Prof
the research project PermaSAR and the main focus is on landsurface subsidence or heave caused by permafrost processes such as thawing and freezing. Field campaigns are conducted in collaboration with the
like what we now see in eastern Siberia. Today’s Arctic, with ice-covered Greenland, Siberian permafrost and sea ice at the North Pole, is a holdover of that glacial world. But for how much longer? As
sediments, documenting a former high stand of Lake Heihai. The fossil lake marls are affected by permafrost and disrupted by segregation ice. In the background, the glaciated peaks of the Kunlun Mountain
processes observed in the coastal and shelf regions are of particular interest, because ice retreat, permafrost thawing and an increase in temperature and volume of river runoff influence local ocean circulation
Geosciences Prof. Dr. G. Mollenhauer Geophysics Dr. V. Schlindwein Glaciology Prof. Dr. I. Weikusat Permafrost Research Prof. Dr. G. Grosse Marine Geology and Palaeontology Prof. Dr. R. Tiedemann Marine Ge
framework of the International Continental Scientific Drilling Program ( ICDP ). In autumn 2008, a permafrost borehole was drilled next to the western shore of the lake, and in spring 2009, we drilled from
and refreezes there, for example as a ice vein in a frost crack. When we take samples from the permafrost today and analyse the isotope ratio of the ground ice in our laboratory, we also make this fingerprint [...] Environmental Systems Past Climate Change ISOLAB Facility - Stable Isotope Laboratory Potsdam Permafrost research at the AWI Glaciological research at the AWI Sample preparation: it couldn't be cleaner
(Atmosphere, Ocean, Ice and Land) Coastal and Shelf Sea Systems Terrestrial Arctic Ecosystems and Permafrost Marine and Polar Life Aquaculture Online applications are open until 14 August 2023 (23:59 CEST)
as part of Polar CORDEX . HIRHAM-CLM atmosphere-land model Simulated active layer thickness and permafrost extent from HIRHAM5 and HIRHAM5-CLM4 (Graphic: Alfred-Wegener-Institut) The original ECHAM5’s [...] soil processes than ECHAM5’s inbuilt land component. CLM4.5 have been widely used in modelling permafrost-related processes. It significantly reduces the simulated bias in active layer thickness and winter