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2003 North Indian Ocean cyclone season : ウィキペディア英語版
2003 North Indian Ocean cyclone season

The 2003 North Indian Ocean cyclone season was mostly focused in the Bay of Bengal, where six of the seven depressions developed. The remaining system was a tropical cyclone that developed in the Arabian Sea in November, which was also the only system that did not affect land. There were three cyclonic storms, which is below the average of 5.4. Only one storm formed before the start of the monsoon season in June, although it was also the most notable. On May 10, a depression formed in the central Bay of Bengal, and within a few days became a very severe cyclonic storm. After it stalled, it drew moisture from the southwest to produce severe flooding across Sri Lanka, killing 254 people and becoming the worst floods there since 1947. Damage on the island totaled $135 million (2003 USD). The storm eventually made landfall in Myanmar on May 19. It is possible that the storm contributed to a deadly heat wave in India due to shifting air currents.
In late July, a monsoon depression moved across much of India, and another monsoon disturbance persisted off the coast of Pakistan. The interaction between the two systems resulted in heavy rainfall across the region, flooding dozens of villages. Monsoonal rainfall killed 285 people between Pakistan and India in the summer of 2003. In late August, another monsoon depression moved across northeastern India. A depression that struck Andhra Pradesh in India killed 21 people in early October. Later that month, a tropical depression crossed Thailand from the western Pacific Ocean, contributing to ongoing flooding that killed 19. Once in the Indian Ocean, this system struck southeastern India without causing much damage. The last system of the year was a cyclonic storm that struck southeastern India in December, killing 81 people and causing $28 million in damage (2003 USD).
==Season summary==


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There were seven depressions throughout the season, of which three attained cyclonic storm status. One of the cyclonic storms formed before the start of the monsoon season, two depressions formed during the monsoon season from June to September, and the remaining systems formed after September.〔 The number of depressions was similar or greater than that of the previous three years.〔 However, the total of 3 cyclonic storms was below the average of 5.4.
In May 2004, seven of the eight members of the World Meteorological Organization panel on tropical cyclones for the North Indian Ocean met in Colombo, Sri Lanka to review the season. During the meeting, the panel announced the first list of tropical cyclone names to be used in the basin for the following season. The panel noted the increasing frequency of deadly natural disasters in the region, such as the floods that affected Sri Lanka in May 2003 from a cyclone. One of the panel's goals was increased coordination between the countries in the region. The India Meteorological Department (IMD) in New Delhi served as the official Regional Specialized Meteorological Center,〔 although the Joint Typhoon Warning Center also issued warnings for the region in an unofficial capacity. The IMD utilized satellite data from EUMETSAT to track cyclones, as well as radars from Bangladesh, Sri Lanka, and India.〔
There were several other monsoon disturbances that affected various countries in the region, including Bangladesh, Pakistan, and Oman.〔 On July 27, during the monsoon season, an area of convection exited from the coast of Pakistan. On the next day, the thunderstorms organized around the center, prompting the Pakistan Meteorological Department to classify the system as a monsoon depression. The IMD operationally classified the system as a depression on July 29, although it was dropped during the agency's annual report.〔 The system weakened into a remnant low on July 30.〔 The system drew moisture from another depression that had moved across India from the Bay of Bengal, bringing three days of heavy rainfall to Karachi, Pakistan. Badin in southeastern Pakistan recorded of rainfall in 24 hours. The rainfall extended into northwestern India, and in Gujarat, a station received more than its annual rainfall during the deluge. Flooding from the heavy rainfall destroyed widespread crops and flooded dozens of villages, and ongoing rains persisted throughout the summer, killing 285 people in the two countries.〔(【引用サイトリンク】publisher=Dartmouth Flood Observatory )

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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