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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.

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    A close up of a snow covered slope.
  2. Our Research

    The study of the last interglacial sea ice requires a cross-disciplinary team of scientists in the fields of climate modelling, sea ice dynamics, and ice/marine sediment cores.   The “Retreat […]

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    A star in the middle of the night sky.