Satellite Remote Sensing
(a) SEASAT operated between
June and November 1978.
(b) GEOSAT monitored the oceans between 1985 and 1990.
(c) TOPEX-POSEIDON is a joint program of NASA and the French space agency
CNES. It began a three year ocean observation program in 1993.
(d) ERS-2, a European satellite, carries radar and microwave systems to
take measurements through clouds and darkness.
(e) SEASTAR carries a sensor to study the distribution of ocean plant
life.
With satellites, oceanographers can study the oceans as a global system.
NASA's NIMBUS-7 satellite, launched in 1978, monitored back radiation and
reflection from the earth's surface and carried a sensor package called
the Coastal Zone Color Scanner that detected multi-band radiant energy
reflecting from Chlorophyll a in sea and land plants. Data from NIMBUS-7
were used to make the images of the world's production of marine plant
life.
SEASAT (a) was a specialized oceanographic satellite that was launched in
June of 1978. It was capable of measuring the distance between the
satellite and the sea surface with accuracy of about 5 cm over a narrow
observational width. Radar echoes returning to multiple receiving
antennas on the satellite measured the scattering patterns caused by
surface waves. Theses patterns gave information on wave height related to
wind speed and scattering direction related to wind direction. The
altimeter detected elevation changes in the sea surface that were used to
measure tides, currents, sea-floor topography, and changes in sea level.
GEOSAT (b) was launched in 1985 to replace SEASAT. It monitored sea-level
topography, surface winds and waves, local gravity changes, and abrupt
boundaries between water types.
The SEASTAR launched in 1996, carrying a system called SeaWiFS (Sea Wide
Field). SeaWiFS returns the ability to study the distribution of
chlorophyll and plant life in the oceans. NASA's Earth Observing System
(EOS) series of satellites, and the Total
Ozone Mapping Spectrometer (TOMS) was launched on July 2, 1996. These
satellites will complement on-going programs by monitoring the roles of
clouds, radiation, water vapor, and precipitation in our weather systems;
the gas exchange between the oceans and the atmosphere; and the role of
polar ice.