 In late August , the monsoon trough spawned a series of disturbances in the Bay of Bengal , including one that developed on August 19 off the Odisha coast . It persisted and gradually organized , becoming a well @-@ marked low pressure area on August 22 . On the following day , the system became a depression , located about 150 km ( 90 mi ) south @-@ southeast of Visakhapatnam , Andhra Pradesh . Moving westward , the system soon moved ashore near Kakinada without intensifying beyond winds of 45 km / h ( 30 mph ) , and quickly weakened into a remnant low on August 24 . The low continued westward , eventually dissipating over Gujarat on August 28 . 
