Sea level change since the Pliocene – a new formalism for predicting sea level in the presence of dynamic topography and isostasy. Austermann, J., Rovere, A., Moucha, R., Mitrovica, J., X., Rowley, D., B., Forte, A., M., & Raymo, M., E. In Geophysical Research Abstracts,EGU General Assembly 2014, volume 16, 2014.
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