ESA’s Gravity field and steady-state Ocean Circulation Explorer (GOCE) mapped the near-stationary structure of Earth’s gravity field and a high-precision geoid for ocean-circulation, sea-level and solid-Earth studies. Launched on March 17, 2009, the spacecraft used six accelerometers in three orthogonal gradiometer arms to measure gravity gradients. GPS tracking and laser ranging constrained its orbit, while continuously adjusted ion propulsion counteracted atmospheric drag at its very low orbital altitude. Its focus on fine spatial structure complements missions that emphasize time-varying mass redistribution. GOCE reentered the atmosphere on November 11, 2013.
Alerts are unavailable because this mission is no longer active.
ESA’s Gravity field and steady-state Ocean Circulation Explorer (GOCE) mapped the near-stationary structure of Earth’s gravity field and a high-precision geoid for ocean-circulation, sea-level and solid-Earth studies. Launched on March 17, 2009, the spacecraft used six accelerometers in three orthogonal gradiometer arms to measure gravity gradients. GPS tracking and laser ranging constrained its orbit, while continuously adjusted ion propulsion counteracted atmospheric drag at its very low orbital altitude. Its focus on fine spatial structure complements missions that emphasize time-varying mass redistribution. GOCE reentered the atmosphere on November 11, 2013.
Alerts are unavailable because this mission is no longer active.