by ZAMG and DHMZ
Two kinds of front delays are discussed:
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03 November 2003/03.00 UTC - Meteosat IR image
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03 November 2003/03.00 UTC - Meteosat WV image
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05 May 2003/00.00 UTC - Meteosat IR image
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05 May 2003/00.00 UTC - Meteosat WV image
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14 November 2003/15.00 UTC - Meteosat IR image
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14 November 2003/15.00 UTC - Meteosat WV image
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The 24 hours Microphysics RGB is an RGB composite based upon the data from infrared channels and differences as follows: IR12.0 - IR10.8 on red colour, IR10.8 - IR8.7 on green and IR10.8 on blue. As the name declares, it can be used day and night. It is designed and tuned to monitor the evolution of fog and low stratus on one hand, and dust and volcanic ash on the other. Secondary applications of this RGB are the detection of fires and low-level moisture boundaries. However, this RGB makes thick high level ice clouds distinctive in its dark red colour, fog or low stratus in ochre and cloud free areas in pinkish (bluish) colour (worth for Mediterranean region and differs quite a lot depending on the time of the year as can be noticed in the two images below).
Front Delay as it appears in Microphysics RGB Image
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17 July 2009/12.00 UTC - Meteosat 9 Microphysics RGB image
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The following 1 hourly loop shows decoupling of clouds at different heights when the front passes the Alps. The first, high cirrus clouds cross the mountain chain (dark blue, almost black colour) and after that, a part of frontal cloudiness (red or dark red colour) moves over the Alps and low level cloudiness (orange to ochre colour) stay behind.
Front Decoupling as it appears in Microphysics RGB Image
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08 March 2009/03.00 UTC - Meteosat 9 Microphysics RGB image
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