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Geostationary Satellites

We switch now to consideration of the second general class of metsats: those in geosynchronous orbit (refer to p.14-5). Most imagery today shown on TV News Weather segments come from such satellites. Launched on December 7, 1966, the first such satellite was ATS-1 (Applications Technology Satellite) which employed the SSCC (Spin Scan Cloud Camera) to obtain visible images of the western hemisphere. The value of synoptic coverage over short time spans was quickly proven by images such as this:

Rapid improvement in vidicon technology led to the first color system, the MSSCC (Multicolor Spin Scan Cloud Camera), on ATS-3 (launched November 5, 1967, producing striking portraits of entire continents such as this view of South America:

The beginning of an operational system dates to May 17, 1974 with the launch of the first of two SMS's (Synchronous Meteorological Satellite). Each carried as its principal sensor the VISSR (Visible Infrared Spin Scan Radiometer). These were predecessors to NOAA's GOES (Geostationary Operational Environomental Satellite) series - the kingpin of present day geosynchronous systems covering the western hemisphere. Here is an artist's drawing of the GOES-8 spacecraft:

GOES-1 was placed in an orbit that fixed it at 135° W soon after launch on October 16, 1975. Others were launched at two to three year intervals (coincidentally, GOES-10 was emplaced on April 25, 1997, the same day this paragraph was written). Those covering the Atlantic Ocean and the eastern U.S. are referred to as GOES-East; those in the Pacific are known as GOES-West). Again, VISSR is the chief sensor, but sounding (VAS is the VISSR Atmospheric Sounder) capabilities are also onboard. Starting with GOES-8 (April 13, 1994), the VISSR is operated 100% of the time rather than providing periodic views.

To exemplify GOES imagery, we now show the first visible image (top) made from GOES-1 on October 26, 1975 and the first IR image (bottom) from GOES-9 on June 19, 1995:



These hemispherical images can be subsetted to concentrate on specific areas. Here are two GOES-8 (East) images: the top one focuses on a large continental storm on March 20, 1994 whereas the bottom one indicates the passage of a front off the Atlantic coast on November 27, 1996:



The GOES-8 sounder has a visible band and 18 thermal bands, chosen to be sensitive to temperature variations related to CO2, ozone, and water vapor at different levels in the atmosphere. Each band can be converted into an image to which colors are assigned to single out thermal differences, as demonstrated in this panel of images taken on May 5, 1997.

Unusual color composites can be made from different channel images. On the top is a colorized rendition of the 6.7 µm channel image from GOES-8, sensitive to water vapor distribution, which highlights a big U.S. storm on March 20, 1994. On the bottom is a false color image made from the 6.7 µm = blue; 11 µm = green; visible = red; this GOES image displays Hurricane Hugo as seen on September 21, 1989.




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Code 935, Goddard Space Flight Center, NASA
Written by: Nicholas M. Short, Sr. email: nmshort@epix.net
and
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Updated: 1999.03.15.