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| earth observation satellites | |
| gravimetry | |
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GRACE is intended to enable precise measurement of Earth's shifting water masses by detecting their effects on our planet's gravity field, allowing the study of global climatic issues by enabling a better understanding of ocean surface currents and heat transport, measuring changes in sea-floor pressure, watching the mass of the oceans change, and by monitoring changes in the storage of water and snow on the continents. Also data on Ocean and deep sea currents as well on tectonics are derived from the data. EXPLANATION GRACE maps variations in the Earth's gravity field over its five-year spacetime (extended to eight years in 2005) with its two identical spacecraft flying about 220 kilometers apart in a Polar Orbit 500 kilometers above the Earth. The twin GRACE satellites were launched from Plesetsk Cosmodrome , Russia on a Rockot (SS-19 + Breeze upper stage) launch vehicle, on March 17 , 2002 . OPERATION The two satellites constantly maintain a two-way microwave-ranging link between them, as well as measuring their own movements using Accelerometer s and Star Camera s and by listening to GPS satellite broadcasts. All of this information is then downloaded to ground stations. The GRACE vehicles also have optical Corner Reflector s to enable Laser Ranging from ground stations. SPACECRAFT MANUFACTURE The spacecraft were manufactured by Astrium of Germany . The microwave RF systems, and attitude determination and control system algorithms were provided by Space Systems/Loral . The star cameras used to measure the spacecraft attitude were provided by Technical University Of Denmark . The instrument computer along with a highly precise GPS and digital signal processing system has been provided by JPL in Pasadena. The highly precise accelerometer that is needed to separate atmospheric and solar wind effects from the gravitation data has been manufactured by ONERA . JPL is responsible for the overall mission management under the NASA ESSP program. DISCOVERIES The data so far obtained by GRACE is the most precise experiment to try to measure the relativistic Frame-dragging effect. In 2006 a team of researchers led by Ralph Von Frese and Laramie Potts used GRACE data to discover the 480 km (300 miles) wide Wilkes Land Crater in Antarctica, which probably formed about 250 million years ago.1 OTHER DEPLOYMENT GRACE data has also been used to analyze the shifts in the Earth's crust caused by the earthquake that created the 2004 Indian Ocean Tsunami . 2 REFERENCES EXTERNAL LINKS
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