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Selected ResultsIndian
Monsoon Region The movement of
Meteosat-5 over India during the Indian Ocean Experiment (INDOEX) starting
in 1998 provided a unique opportunity to study in detail the daytime diurnal
variability of clouds and components of the radiation budget over that
region Wonsick et al., 2009). Documented is the seasonal progression of
the Asian monsoon as seen in clouds and convection in the pre-, peak-,
and post-monsoon seasons. Diurnal variation of frequency of occurrence
of low cloud (left column) and high cloud (right column) for pre-monsoon
(Mar - May; top row), peak-monsoon (Jun - Sep; middle row), and post-monsoon
(Oct - Nov; bottom row) season 2001 for the hours of 8 - 15 LST is shown
in Figure 1; monthly mean cloud amount (%)
is given in Figure 2; frequency of occurrence
of convective clouds at selected daytime hours for the peak-monsoon season
(Jun - Sep) 2001 is shown in Figure 3; cloud
amount (%, top) and type (bottom) derived from Meteosat-5 for 1 Aug 04
at 07 UTC is shown in Figure 4; surface SW
downward flux (Wm-2) at 0.125 resolution with clouds from Meteosat-5 (top)
and at 2.5 resolution with clouds from ISCCP D1 (bottom) is given in Figure
5.
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