What is it about?
The surface of the Earth deforms in response of both deep solid-state mantle convection and melting of ice sheets. These processes normally occur on different spatial and time scales but it is difficult to separate these possesses from geophysical data. New satellite gravity data combined with high-resolution seismic tomography models and analysis of postglacial rebound allows for better understanding how climate-driven and solid Earth processes are linked.
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This page is a summary of: Late Cenozoic lithosphere dynamics in Svalbard: interplay of glaciation, seafloor spreading and mantle convection, Journal of Geodynamics, September 2018, Elsevier,
DOI: 10.1016/j.jog.2018.09.009.
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