The tropical disturbance ,that became TC09B was fwst identified on the 011800Z November
Significant Tropical Weather Ad~isory by JTWC as a broad area of convection in the Bay of Bengal.
As the tropical disturbance tracked north-northwestward, its convection increased in amount and organization.
JTWC issued a Tropical Cyclone Formation Alert at 0221002, and the first warning at
0300002. Intensification continued until the tropical cyclone stalled on 5 November. With increasing
wind sheer aloft over the cyclone, a weakening trend set in on 6 November which continued until
TC09B dissipated over water two days later. The final warning was issued by JTWC at 0718002.
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