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energy imbalance (EEI) and ocean heat content (OHC), in order to close an existing knowledge gap and im-prove near-term predictions. Other partners in the project are University of Ber-gen and Nansen
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the planet and across its surface. Density variations in Earth’s interior, generated by processes such as subduction and mantle convection, as well as the redistribution of water, ice, and rock at the surface
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. Depending on the deformation direction with respect to the mean orientation of crystals in both ice and mantle rock, the bulk viscosity can vary by a few orders of magnitude. Such variations in viscosity can
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