Under the influence of an upper air cyclonic circulation, a low pressure area formed over Andaman Sea on October 6.[20] The system drifted westward and intensified into a depression and subsequently into a deep depression the next day, followed by the Joint Typhoon Warning Center (JTWC) issuing a Troipical cyclone formation alert (TCFA).[21] Owing to favorable environmental conditions, the storm intensified into a cyclonic storm on October 8 and was named Hudhud.[22][23] Its convection consolidated in the following hours, and Hudhud became a Severe Cyclonic Storm on October 9. Hudhud underwent rapid deepening in the following days, intensified into a Very severe cyclonic storm and developed a well-defined eye feature. Shortly before landfall near Visakhapatnam, Andhra Pradesh on October 12, Hudhud reached its peak strength with three minute wind speeds of 175 km/h (109 mph) and a minimum central pressure of 960 hPa (28.35 inHg).[24] The system drifted northwards over land and was last noted as a well-marked low pressure area over east Uttar Pradesh on October 14.[25]
Hudhud brought extensive damage to the coastal districts of Andhra Pradesh. At least 84 deaths were reported due to the storm, and the damage cost was amounted to $9.7 billion, making Hudhud the first storm in the basin to cause at least $9 billion in damage since Nargis in 2008.
Hudhud brought extensive damage to the coastal districts of Andhra Pradesh. At least 84 deaths were reported due to the storm, and the damage cost was amounted to $9.7 billion, making Hudhud the first storm in the basin to cause at least $9 billion in damage since Nargis in 2008.
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