• The gypsum gravity chute: A phytoplankton-elevator to the ocean floor

    sink, hereby transporting large quantities of carbon to the ocean’s depths. Experts from the Alfred Wegener Institute recently observed this phenomenon for the first time in the Arctic. As a result of

  • Sitemap

    Business Travel Health at the Workplace Sustainable Ship Operation AWI Sustainability Guideline Alfred Wegener Continental drift Seafloor spreading Logistics Schedules Proposals Advisory Board Neumayer Advisory

  • Modell Simulations

    Model Simulations What are sea ice models used for? Example of a sea ice model (Graphic: Alfred Wegener Institut) The Arctic areas - ocean even more than land - are difficult to reach, for several winter

  • SHERPA

    analyses of images from Mann et al. (2004) . Screenshot SHERPA (Photo: Alfred-Wegener-Institut) Segmented diatom valve (Photo: Alfred-Wegener-Institut)

  • Paleoclimate Research

    stable water isotope values of ice cores from Northern Greenland (Graphic: Stefanie Weißbach, Alfred-Wegener-Institut) Human activities have serious impacts on the global environmental system and will,

  • REKLIM-Max_en

    informtion can be found on the REKLIM website . Circumpolar Map of Northerm Hemisphere (Graphic: Alfred Wegener Institut) Project collaborators Lars Max Ralf Tiedemann Figure 1: Overview map of high-latitude

  • 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

  • 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

  • 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