Jet Propulsion Laboratory Home Page
Jet Propulsion Laboratory Website National Aeronatics and Space Administration CalTech Home Page
JPL Home Page Earth Solar System Stars and Galaxies Technology Search
Images and Videos News Missions Events Kids Education Scientists and Engineers About JPL
Upper-left corner   Upper-right corner
  NEWS
Dot PRESS RELEASES

  Dot2001 RELEASES

  Dot2000 RELEASES

  Dot1999 RELEASES

  Dot1998 RELEASES

  Dot1997 RELEASES

  Dot1996 RELEASES

Dot PRESS KITS

Dot FACT SHEETS

Dot FEATURES

Dot PROFILES

Dot IMAGES / VIDEOS

Dot MEDIA VISITS

Dot MEDIA CONTACTS

Dot EMPLOYEE NEWSPAPER

 
2002 News Releases

From Satellites to Sea: JPL Scientists Map Ocean Eddies
September 13, 2002

airborne instruments aboard plane have demonstrated the ability to use signals from GPS to map ocean eddies
JPL researchers, using airborne instruments aboard this aircraft, have demonstrated the ability to use signals from the global positioning system to map ocean eddies
Image courtesy: I.K. Curtis Services
Browse image

       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, which affect shoreline weather and the fishing industry, represent "one of the largest unknowns in Earth's climate models," said JPL physicist Dr. Stephen Lowe. Lowe led two aircraft experiments to test how well GPS could be used for altimetry, or measuring sea-surface height.

       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.

eddy off California, October 2001
Eddy off coast of California, October 2001
Caption page
More information on coastal eddy research

       "Eddies are small features with a big impact," said co-author Dr. Yi Chao, a JPL oceanographer. "They're where a lot of ocean physics happens and are an integral part of our climate system. But we don't have enough information about them to include in our models. Coastal eddies also have a major role in regulating the weather near the shore, and they are important for fisheries because they're where fish go to feed. In the open ocean, eddies bring nutrient-rich cold water up to the surface and are an important part of the global carbon cycle."

       In 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 U.S.-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.

       "Our plan is not to replicate the very precise measurements that Topex/Poseidon and Jason 1 make," said Chao, "but rather to help fill in some of the gaps in time and in coverage by looking between the satellites' ground tracks and close to the shore. We would like to provide a new data set to push the next generation of climate models."

       JPL is a division of the California Institute of Technology in Pasadena.


Contacts: JPL/Alan Buis (818) 354-0474

2002-175

Bottom-left corner   Bottom-right corner  

Privacy / Copyright FAQ Feedback Site Map