The high pressure system in southern hemisphere is formed just 4300 km south of Cape Comerin and has lesser strength to form cross equatorial flow. However it induced or influenced SOUTHERLY flow winds near Comrin. The western side of southern tip is slowly heated and small extent convective clouds are formed. Similarly medium level convective clouds [CTT &Minus 40 C] are formed over Rayalaseema, NE parts of Karnataka, and adjoining place capable of producing TS with 2-3 cm rainfall
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