Ice-sheet modelling

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  1. Geological History Constraints on the Magnitude of Grounding Line Retreat in the Thwaites Glacier System

    GHC will gather information about past ice sheet behaviour and relative sea level change in the Thwaites Glacier system. Determining the timing and magniture of past episodes of thinning and retreat and subsequent re-advance is important to provide a context for the current and future behaviour of Thwaites Glacier.

    Read more of: Geological History Constraints on the Magnitude of Grounding Line Retreat in the Thwaites Glacier System
    A close up of a snow covered slope.