"Under the influence of upper air cyclonic circulation over northwest Bay of Bengal, a low pressure area has formed over northwest Bay of Bengal and associated cyclonic circulation extends upto mid tropospheric levels tilting southwestwards with height."
Source
Comment by Praful Rao
STH stormwatch is a procedure started many years ago where we use broadband internet to keep a close watch on the adverse weather activities in the Bay of Bengal with a view to forewarn communities on the formation of any adverse weather in the Bay and its movement.
