This image shows
the variations in the gravity field near the buried impact crater.
Over its lifetime of about 20 months, GOCE will map these global
variations in the gravity field with extreme detail and accuracy.
Not exact matches
As proof, the researchers cite tiny
variations in the earth's rotation and
gravity field, as well as deflections of continental regions like southern Africanow one kilometer higher than northern Africa.
The largest «bulges» are due to
variations in Earth's
gravity field.
Small changes
in the planet's
gravity field can push the satellites together, ever so slightly, or pull them apart —
variations that scientists use to interpret the terrain below.
Focus of Study The long - term
variation of the Earth's
gravity field due to post-glacial rebound and present - day ice melting
in the polar regions.
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).