Its primary mission was to measure the surface wind speed and direction over the ice-free global oceans via its effect on water waves.QuikSCAT was a "quick recovery" mission replacing the NASA Scatterometer (NSCAT), which failed prematurely in June 1997 after just 9.5 months in operation.Because of its wide swath and lack of in-swath gaps, QuikSCAT was able to collect at least one vector wind measurement over 93% of the World's Oceans each day.QuikSCAT provided measurements of the wind speed and direction referenced to 10 meters above the sea surface at a spatial resolution of 25 km.Scatterometers such as QuikSCAT emit pulses of low-power microwave radiation and measure the power reflected back to its receiving antenna from the wind-roughened sea surface.Gravity and capillary waves on the sea surface caused by the wind reflect or backscatter power emitted from the scatterometer radar primarily by means of a Bragg resonance condition.σ0 varies with surface wind speed and direction relative to the antenna azimuth, incidence angle, polarization, and radar frequency.[6] The QuikSCAT project was originally budgeted at $93 million, including the physical satellite, the launch rocket, and ongoing support for its science mission.It recorded roughly four hundred thousand wind measurements daily, each covering an area 1,800 kilometers (1,100 mi) in width.[6] Jet Propulsion Laboratory and the NSCAT team jointly managed the project of construction of the satellite at the Goddard Space Flight Center.[8] The newly constructed satellite was set to launch on a Titan II rocket from Vandenberg Air Force Base in California.Shortly after, the solar arrays were deployed and connection was established with the satellite at 8:32 pm PDT with a tracking station in Norway.On July 7, eighteen days after take-off, the scatterometer was turned on and a team of 12 personnel made detailed reviews of function of QuikSCAT.[9] Many operational numerical weather prediction centers began assimilating QuikSCAT data in early 2002, with preliminary assessments indicating a positive impact.[16] This followed a battery anomaly in which the spacecraft was temporarily unable to perform nominal science observations due to limited power.
Image of Antarctica produced by the SeaWinds instrument on May 24, 2000
The last image produced from QuikSCAT data (placed on top of two GOES images) shortly before the antenna stopped spinning. Note the small area where wind data is present in comparison the area covered by the image.
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