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![](https://webarchive.library.unt.edu/eot2008/20090118072402im_/http://topex-www.jpl.nasa.gov/images/l2-main-content-top.gif) |
Altimeter(s)
OSTM/Jason-2
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The Poseidon-3 radar altimeter is the main instrument on the Jason-2 mission. Derived from the Poseidon-1 altimeter on Topex/Poseidon and the Poseidon-2 on Jason-1, it measures sea level, wave heights and wind speed.
The Poseidon-3 altimeter emits pulses at two frequencies 13.6 and 5.3 GHz to measure the distance from the satellite to the surface (range). Free electrons in the atmosphere can delay the signal's return, affecting the measurement accuracy. The delay is directly related to the radar frequency, so the difference between the two measurements can be used to determine atmospheric
electron content. Poseidon-3 is coupled with Doris/Diode, to improve measurements over coastal areas, inland waters and ice.
Additional information on the Poseidon-3 instrument is available on the AVISO site.
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Jason-1
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The POSEIDON-2 altimeter is the main instrument on the Jason-1 mission. Derived from
the POSEIDON-1 altimeter on TOPEX/Poseidon, it measures sea level, wave heights
and wind speed. It operates at two frequencies and is also able to estimate atmospheric
electron content.
The altimeter emits a radar beam that is reflected back
to the antenna from the Earth's surface. POSEIDON-2 operates
at two frequencies (13.6 GHz in the Ku-band,
5.3 GHz in the C-band)
to determine atmospheric electron content, which affects the
radar signal path delay. These two frequencies also serve
to measure the amount of rain in the atmosphere.
Additional information on the Poseidon-2 instrument is available on the AVISO site.
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TOPEX/Poseidon
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The dual-frequency NASA radar
altimeter, NRA, is
the primary instrument aboard the spacecraft. It works by sending
radio pulses at 13.6 GHz and 5.3 GHz toward the earth and measuring
the characteristics of the echo. By combining this measurement
with data from the microwave
radiometer and with other information from the spacecraft and
the ground, scientists can calculate the height of the sea surface
to within 4.3 centimeters.
The single-frequency CNES altimeter, POSEIDON-1, like the GPS receiver, is classified as an experimental
sensor because TOPEX/Poseidon is the first flight to utilize this technology. The CNES
altimeter is a solid-state, low-power, low-mass sensor which works in much the same
way as the NASA altimeter. It shares the same antenna as the NRA; thus only one altimeter operates
at any given time. It operates about 10% of the time, or one cycle over ten. Its precision
is also comparable with that of the NASA altimeter.
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Altimeter(s) |
Radiometer |
DORIS |
LRA |
GPS/TRSR
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