Home Geospatial Applications Miscellaneous Jet Propulsion Laboratory’s scientists map ocean Eddies

Jet Propulsion Laboratory’s scientists map ocean Eddies

Pasadena – Sep 19, 2002 Just as sunlight glints off the ocean’s surface, so do radio signals from the constellation of global positioning system (GPS) navigation satellites orbiting Earth. Now, researchers from NASA’s Jet Propulsion Laboratory, Pasadena, Calif., have shown that although these reflected signals are very weak, they can be detected by airborne instruments and used to map ocean eddies.

Eddies are currents that run in a circular path against the main flow of current. Warm eddies have a higher surface height than the surrounding water, while cool eddies are lower.Ranging from 10 to 100 kilometers (6 to 62 miles) in size, many ocean eddies are either too small or don’t last long enough to be spotted by the current generation of satellite ocean altimeters, whose measurements of sea-surface height provide a picture of global circulation.Lowe and his colleagues’ goal is to determine whether, in the future, reflected GPS signals could be used to map small ocean circulation features such as eddies from space.n the first experiment, designed to collect reflected GPS signals from a variety of terrain, the scientists demonstrated that these signals could be detected and used to calculate ocean height.

In the second experiment, planned specifically for ocean altimetry, they showed their technique has the potential to provide ocean-height measurements precise enough to map ocean eddies. The results of the latest experiment appear in the May issue of Geophysical Research Letters.Today’s satellite ocean altimeters, including the US-French Topex/Poseiden and Jason 1 spacecraft, measure sea-surface height by sending a radar pulse to the ocean’s surface and timing its return.While they measure ocean surface topography very accurately, to within 2 centimeters (1 inch), they see only the swath of ocean directly beneath them and take 10 days to make a complete map of the global ocean. Since an ocean eddy lasts only a week or two, they may only catch a portion of an eddy’s lifespan.

In contrast, an orbiting GPS altimeter would have no radar, making it relatively inexpensive. The receiver would obtain position and timing information from the GPS constellation of satellites and would measure ocean height using the arrival time of GPS signals reflected from the surface.At any single time, it would be able to produce about 10 simultaneous measurements across an area thousands of kilometers wide. A constellation of about 10 such instruments, capable of making up to 100 simultaneous ocean-height measurements, could map ocean eddies globally.The Global Positioning System is a Department of Defense-controlled navigation system comprised of 28 Earth-orbiting satellites and a network of tracking stations.By measuring the time it takes for signals to travel directly between satellites and receivers, the positions of the satellites and receivers can be determined.In coming experiments, the JPL researchers will fly their equipment on aircraft at different altitudes and speeds.They’ll be making ocean-height measurements and comparing their results with those from other instruments. They also have plans to improve their onboard receiver so that the instrument can be flown on spacecraft.