Abstract
The first observations from meteorological satellites were cloud pictures. These wee put to use immediately and are still used daily for locating storms over ocean areas (see Chapters VII-7 and VII-10). To use cloud imagery successfully for analysis of synoptic-scale storms, two criteria must be met: (1) entire storms and their surroundings must be viewed approximately simultaneously, and (2) the frequency of observations must be no less than once every 12 hours and preferably once every 6 hours. The first criterion was met in 1966 with data from the Environmental Science Services Administration (ESSA) polar orbiters. In 1972, the NOAA series of polar orbiters provided images twice a day. In 1974 the GOES satellites increased the frequency of observations to every 30 min, permitting the producting of time lapse animation of synoptic-scale weather systems.
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© 1990 American Meteorological Society
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Rao, P.K., Holmes, S.J., Anderson, R.K., Winston, J.S., Lehr, P.E. (1990). Use of Satellite Imagery in Synoptic-Scale Weather Analysis and Forecasting. In: Rao, P.K., Holmes, S.J., Anderson, R.K., Winston, J.S., Lehr, P.E. (eds) Weather Satellites: Systems, Data, and Environmental Applications. American Meteorological Society, Boston, MA. https://doi.org/10.1007/978-1-944970-16-1_29
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DOI: https://doi.org/10.1007/978-1-944970-16-1_29
Publisher Name: American Meteorological Society, Boston, MA
Online ISBN: 978-1-944970-16-1
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