Moreover,
solid earth deformation and redistribution of ocean water influence each other, because the ocean represents a load on the Earth's surface.
Konfal, S. A., Wilson, T. J., Bevis, M. G., Kendrick, E. C., Willis, M. J., (2012), Modern Horizontal Crustal Motions in Victoria Land, Antarctica: Influence of Heterogeneous Earth Structure on
Solid Earth Deformation, Abstract T41B - 2591 presented at 2012 Fall Meeting, AGU, San Francisco, Calif., 3 - 7 Dec..
Konfal, S., Wilson, T., Bevis, M., Kendrick, E., Hall, B., GPS and paleoshoreline record of
solid earth deformation in Southern Victoria Land, Antarctica, Proc.
Not exact matches
Regional variations arise because the
Earth's gravity field is affected in multiple ways by the melt of ice, due to the direct effect of surface mass changes (the gravity field is determined by the distribution of mass), the consequent
deformation of the
Solid Earth (removing a load causes the
Earth's surface to rebound, which in turn changes the distribution of the
Earth's mass), the consequent redistribution of ocean water (the ocean surface is shaped by the gravity filed) and perturbations of the
Earth's rotation axis (because of mass redistribution).
However the
deformation of the
solid Earth by ice sheet loading is so extensive that both the elastic crust and plastic mantle are involved.