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Variation of Zonal Winds in the Upper Troposphere and Lower Stratosphere in Association with Deficient and Excess Indian Summer Monsoon Scenario

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Figure

Table 1. Indian summer Monsoon Rainfall in mm (ISMR) from 1960 to 1998 and their departure from long-term normal (852.4 mm) in terms of the standard deviation (84.5 mm)
Figure 1. Monthly zonal wind (m·s−1) climatology averaged over the Indian region (65˚E - 90˚E & 0˚ - 25˚N) from surface (1000 hPa) to stratospheric level (10 hPa) for the period 1960-1998
Figure 2. Wind anomaly vector in (m·s−1) over the region (0˚ - 25˚N and 65˚E - 90˚E) for the levels 70 hPa, 100 hPa and 200 hPa for DRY (figures a1), b1), and c1)) and WET (figures a2), b2), and c2)) year’s composites
Figure 3. Vertical variation of zonal wind (m·s−1) for the pressure levels 1000 hPa to10 hPa averaged over the Indian longi-tude belt (65˚E - 90˚E) during monsoon period
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