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This post will focus on delivering two main tasks within the Horizon Europe SYNCHRONY project: Using an offline particle trajectory package applied to a very high-resolution ocean model, simulate Antarctic continental shelf drift trajectories of virtual
To work out an optimal approach/workflow for the interpretation of geophysical data and mapping of the (non-eroded) top Pleistocene surface, including characterization of its attributes; To collate and analyze existing (legacy) geophysical and geological