UNDER INFLUENCE OF THE UPPER AIR CYCLONIC CIRCULATION OVER EASTCENTRAL ARABIAN SEA A LOW PRESSURE AREA HAS FORMED OVER CENTRAL ARABIAN SEA (.)
ARABIAN SEA: -
BROKEN LOW/MEDIUM CLOUDS WITH EMBEDDED INTENSE TO VERY INTENSE CONVECTION OVER SOUTH ARABIAN SEA WEST OF LONGITUDE 64.0E AND MODERATE TO INTENSE CONVECTION OVER REST ARABIAN SEA (.)