Statistics – Computation
Scientist
Statistics
Computation
Scientist
Dublin Institute for Advanced Studies, Dublin, Ireland
GeoForschungsZentrum Potsdam, Telegrafenberg, D-14473 Potsdam, Germany; Charles University, V Holešovičkách 2, 18000 Prague 8, Czech Republic
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, Praha, Czech Republic; School of Theoretical Physics, Dublin Institute for Advanced Studies, 10 Burlington Road, Dublin 4, Ireland
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, 18000, Praha, Czech Republic
Karlova Università, Prague, Czechoslovakia
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holesõovicõkách 2, 180 00 Prague 8, Czech Republic.
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkach 2, Praha 8, Czech Republic
GeoForschungsZentrum Potsdam, Telegrafenberg, D-14473, Potsdam, Germany
GeoForschungsZentrum Potsdam, Division 1: Kinematics and Dynamics of the Earth, Telegrafenberg, D-14473, Potsdam, Germany
GeoForschungsZentrum Potsdam, Department 1: Geodesy and Remote Sensing. Potsdam, Germany of Geodesy and Remote Sensing, GeoForschungsZentrum Potsdam, Telegrafenberg A17, D-14473, Potsdam, Germany; Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, Praha, Czech Republic
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, 18000 Prague 8, Czech Republic.
Department of Geophysics, Faculty of Mathematics and Physics, Charles University, V Holešlovičkách 2, 180 00 Prague 8, Czech Republic.
A benchmark study for glacial isostatic adjustment codes
A determination of the parameters of the level surface of lunar gravity
Can the 1D viscosity profiles inferred from postglacial rebound data be affected by lateral viscosity variations in the tectosphere?
Comparison between Newtonian and non-Newtonian flow driven by internal loads.
Detectability of geoid displacements arising from: changes in global continental-ice volumes by the GRACE gravity space mission
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