Physics
Scientist
Japan Marine Science and Technology Center, Yokosuka 237-0061, Japan
Institut für Meteorologie und Geophysik, Johann Wolfgang Goethe-Universität, Feldbergstr. 47, 60323, Frankfurt am Main, Germany
Centre for Geodynamics, NGU, Leiv Eiriksonsvei 39, Trondheim, 7491, Norway
Centre for Geodynamics, NGU, Leiv Eirisksonsvei 39, Trondheim, 7491, Norway
Geological Survey of Norway, Leiv Eirikssons vei 39, Trondheim, 7491 Norway
Institut für Meteorologie und Geophysik, Johann Wolfgang Goethe-Universität, 60323, Frankfurt am Main, Germany
Centre for Geodynamics, Geological Survey of Norway, Leiv Eirikssons vei 39, N-7491 Trondheim, Norway
Helmholtz Centre Potsdam, German Research Centre for Geosciences, Potsdam, Germany; Physics of Geological Processes and Geosciences, University of Oslo, Norway
IFREE, JAMSTEC, 2-25 Natsushima-cho, Yokosuka 237-0061 Japan
Centre for Geodynamics, NGU, Leiv Eirikssons vei 39, N-7491 Trondheim, Norway
Centre for Geodynamics, Geological Survey of Norway, NO-7491 Trondheim, Norway
Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany; Center for Geodynamics, NGU, N-7491 Trondheim, Norway
Center for Geodynamics, NGU, N-7491 Trondheim, Norway.
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany; Physics of Geological Processes and Geosciences, University of Oslo, Oslo, Norway
Center for Geodynamics, N.G.U., 7491 Trondheim, Norway
Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany. After 1: Norges geologiske undersøkelse, N-7491 Trondheim, Norway
Center for Geodynamics, Norges Geologiske Undersøkelse, Leiv Eirikssons vei 39, N-7491 Trondheim, Norway
Center for Geodynamics, Geological Survey of Norway, NO-7491 Trondheim, Norway; Helmholtz Centre Potsdam, German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Advection of plumes in mantle flow: implications for hotspot motion, mantle viscosity and plume distribution
An explanation for the shape of Earth's gravity spectrum based on viscous mantle flow models
Changes of the Earth's rotation axis owing to advection of mantle density heterogeneities
Constraining rheology and water content in the upper mantle by modeling plate tectonics
Deep versus shallow origin of gravity anomalies, topography and volcanism on Earth, Venus and Mars
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