Earth System Modelling, Department Geodesy, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Earth System Modelling, Department Geodesy, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Earth System Modelling, Department Geodesy, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Earth System Modelling, Department Geodesy, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Maik Thomas
Earth System Modelling, Department Geodesy, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Institute for Meteorology, Freie Universität Berlin, Kaiserswerther Str. 16–18, 14195 Berlin, Germany
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Total article views: 3,411 (including HTML, PDF, and XML)
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2,819
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BibTeX: 78
EndNote: 134
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Viewed (geographical distribution)
Total article views: 4,850 (including HTML, PDF, and XML)
Thereof 4,437 with geography defined
and 413 with unknown origin.
Total article views: 3,411 (including HTML, PDF, and XML)
Thereof 3,069 with geography defined
and 342 with unknown origin.
Total article views: 1,439 (including HTML, PDF, and XML)
Thereof 1,368 with geography defined
and 71 with unknown origin.
Glacial isostatic adjustment is the delayed reaction of the Earth's lithosphere and mantle to changing mass loads of ice sheets or water. The deformation behaviour of the Earth's surface depends on the ability of the Earth's mantle to flow, i.e. its viscosity. It can be estimated from sea level observations, and in our study, we estimate mantle viscosity using sea level observations from the past. This knowledge is essential for understanding current sea level changes due to melting ice.
Glacial isostatic adjustment is the delayed reaction of the Earth's lithosphere and mantle to...
