Contrary to what you might expect, a recent published study unveiled by scientists shows a map of our planet’s gravity, which resembles not a sphere, but more a … potato. This is because the Earth’s gravity isn’t uniform, being affected everyday by such factors like winds, currents and tides, so because gravity is higher in Iceland than in India you get this weird looking shape. The map is actually called a geoid, the result of two years of orbital surveys by the European Space Agency (ESA) Gravity Field and Steady-State Ocean Circulation Explorer (GOCE) satellite.
Below you can see a somewhat exaggerated rending of the geoid captured by GOCE. Gravity is strongest in yellow areas; it is weakest in blue ones.
Professor Reiner Rummel, former head of the Institute for Astronomical and Physical Geodesy at Technische Universität München in Germany, says GOCE provides dynamic topography and ocean circulation patterns with unprecedented quality and resolution.
“The GOCE geoid will improve our understanding of Earth’s internal structure,” he said.
The Gravity Field and Steady-State Ocean Circulation Explorer (Goce) in orbit. (c) ESA
GOCE also offers some very interesting data which prove indeed very useful for scietists studying earthquakes. The giant jolt that struck Japan this month and Chile last year occurred because huge masses of rock suddenly moved in the tectonic movement – Goce should reveal a three-dimensional view of what was going on inside the Earth in that moment.
“Even though these quakes resulted from big movements in the Earth, at the altitude of the satellite the signals are very small. But we should still seem them in the data,” said Dr Johannes Bouman from the German Geodetic Research Institute (DGFI).
