• Team

    dynamics and Earth System feedbacks Permafrost coring in the Fish Creek Delta, North Alaska (Photo: Alfred Wegener Institut) Arctic permafrost landscapes change rapidly under the influence of natural and ant [...] permafrost carbon pools and their vulnerability to mobilization Alaskan Yedoma cliff (Photo: Alfred Wegener Institut) Arctic landscapes underlain by permafrost are threatened by climate warming and may [...] Degradation of ice-rich permafrost by thermal erosion thermoerosional valley Kurungnakh (Photo: Alfred-Wegener-Institut) Thermo-erosional valleys are widely distributed in ice-rich permafrost deposits of

  • Remote Sensing

    Remote Sensing Map of Arctic sea ice thickness (April 2015) obtained from CryoSat-2 data (Graphic: Alfred Wegener Institut) Contact: Dr. Stefan Hendricks The inaccessibility and sheer size of sea ice covered [...] based on measuring the height of ice floes above the sea surface with radar altimeters (Graphic: Alfred Wegener Institut)

  • Data Assimilation

    been successfully applied to North Atlantic/Arctic Ocean Sea Ice Model (NAOSIM) developed at the Alfred Wegener Institute (AWI). We are currently working to apply the systems to Finite-volumE Sea ice-Ocean [...] simulation without data assimilation, red: model simulation with data assimilation. (Graphic: Alfred-Wegener-Institut) Spatial pattern of sea ice extent in September, from 1990 to 2010 (every 5 years). [...] simulation without data assimilation, black: model simulation with data assimilation. (Graphic: Alfred-Wegener-Institut) Spatial pattern of sea ice motion in August 2006: Left panel: model simulation without

  • Microstructure Mapping

    Example of Microstructure Mapping image (Photo: Ilka Weikusat, Alfred-Wegener-Institut) An essential part of ice core research at the AWI consists of mapping the microstructural parameters (grain size

  • West Antarctic Ice Sheet

    region and West Antarctic margin (modified from Kipf et al., Gondwana Research, 2014). (Photo: Alfred-Wegener-Institut) Geodynamic and tectonic processes played a dominant role in forming the present topographic

  • Freshwater fluxes

    content (integrated in the area in blue on the map) freFresh water content cha (Graphic: T. Kovacs, Alfred-Wegener-Institut) The Arctic Ocean receives freshwater by run-off from Asia north of the Himalaya. Large

  • Methane

    Methane Airborne measurements of atmospheric methane Methane signal over a lake. (Graphic: Alfred-Wegener-Institut) Methane (CH4) is an important greenhouse gas. Though its concentration in the atmosphere

  • Ant_Peninsula

    produce base data sets for habitat studies. Larsen A, B, and C ice shelves, Weddell Sea (Graphic: Alfred Wegener Institut) Contact Dr. Boris Dorschel Prof. Dr. Wilfried Jokat Cooperation partners Geology, AWI

  • Campaigns

    campaign performed by the Leipzig Institute for Meteorology (LIM), University of Leipzig and the Alfred-Wegener-Institute (AWI) at Kohnen Station , Antarctica (75°00’ S, 00°04’ E, 2892 m a.s.l.) in austral

  • Fabric Analyser

    c-axes measurements with the automated fabric analyser (Graphic: Alfred-Wegener-Institut) Crystal orientations (also called fabrics or lattice orientations ) represent an important subject of microstructure