An algorithm to detect tropical deep convective clouds through AMSU-B water vapor channels |
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Authors: | Xu Xu Heygster Georg Suping Zhang |
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Institution: | 1. Ocean-Atmosphere Interaction and Climate Laboratory, Ocean University of China, Qingdao 266003, P. R. China 2. Institute of Environmental Physics, University of Bremen, Germany |
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Abstract: | An algorithm to detect tropical deep convective clouds and deep convective overshootings based on the measurements from the
three water vapor channels (183.3 GHz±1 GHz, 183.3 GHz±3 GHz and 183.3 GHz±7 GHz) of the Advanced Microwave Sounding Unit-B
(AMSU-B) is presented. This algorithm is an improved version of the method of Hong et al. (2005). The proposed procedure is based on the statistical analysis of seven years’ (2001–2007) measurements from AMSU-B
on NOAA-16. From the 1-d histograms of the brightness temperature of the three water vapor channels and the 2-d histograms
of the brightness temperature difference between these channels, new thresholds for brightness temperature differences and
the brightness temperature of channel 18 (183.3 GHz±1 GHz) are suggested. The new algorithm is employed to investigate the
mean distribution of tropical deep convective clouds and convective overshootings from 30°S to 30°N for the years 2001 to
2007. The major concentration of deep convective clouds and convective overshootings is found over the Intertropical Convergence
Zone (ITCZ), the South Pacific Convergence Zone (SPCZ), tropical Africa, South America, the Indian Ocean and Indonesia with
an average fraction of 0.4%. In terms of these clouds we identify the secondary Intertropical Convergence Zone located in
the eastern South Pacific and parallel to the main ITCZ in the North Pacific. The convective overshooting is more frequently
observed over land than over the ocean. |
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Keywords: | microwave remote sensing AMSU-B deep convective clouds tropics |
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