Severe Cyclonic Storm Jal was the fifth named cyclonic storm and the fourth Severe Cyclonic Storm of the 2010 North Indian Ocean cyclone season. Jal developed from a low-pressure area in the South China Sea that organized into a Tropical Depression on . Jal is a Sanskrit word, meaning water. At least 54 people are known to have been killed in India. As a tropical depression, Jal produced torrential rains over parts of Thailand and Malaysia, triggering severe flooding which killed 59 and four people in the two countries respectively. In Sri Lanka, heavy rainfall with strong winds have caused flooding affecting around 80,000 people. In Thailand, Jal was responsible for 78 deaths, being the 4th deadliest tropical cyclone in the country. Meteorological history On October 12, a weak tropical disturbance formed within a monsoonal trough of low pressure in the South China Sea, just off the eastern coast of Borneo. For the next few weeks, the system stalled on the eastern coast of Bormeo, remaining disorganized, while the system barely affected the island of Borneo at all. During the last week of October, the storm detached from the moonsonal trough, and began slowly moving east. On , the Japan Meteorological Agency (JMA) and the Joint Typhoon Warning Center (JTWC) both reported that the system had begun to develop, already beginning to organize itself, about 550 km (340 mi), to the southeast of Ho Chi Minh City, Vietnam. During the next few days, the tropical depression strengthened slowly as it slowly moved towards the eastern border of the Indian Ocean. During this time, convection around the disturbance increased, but failed to organize around the storm's low level circulation center. Despite these unfavorable conditions, the storm managed to develop convection around its area of low pressure, and organized itself significantly. On , the Thai and Malaysian meteorological departments (TMD) reported that the disturbance had developed into a tropical depression, and initiated advisories on the system. From continuing into , the storm strengthened slightly as it continued moving towards the Indian Ocean, but not enough for it to become a tropical storm. Late on , the tropical depression crossed the Malay Peninsula, and entered the extreme eastern part of the Indian Ocean, causing the west Pacific agencies to cancel all their advisories on the storm, as it was no longer in the west Pacific Ocean. As soon as the system entered the