2000 North Indian Ocean cyclone season
http://dbpedia.org/resource/2000_North_Indian_Ocean_cyclone_season an entity of type: Abstraction100002137
2000年北印度洋氣旋季泛指在2000年全年內的任何時間，於北印度洋水域所產生的熱帶氣旋。雖然有關方面並沒有設下本颱風季的指定期限，但大部份北印度洋的熱帶氣旋通常都會於四月至十二月期間形成。 本條目的範圍僅侷限於北印度洋水域。在北印度洋產生的氣旋風暴是由隶属于的印度氣象局新德里颱風中心命名，而在該地區的熱帶低氣壓的編號都以 A/B 字母作結。 在香港天文台的天氣圖上也包括東北印度洋地區，若有熱帶氣旋形成，則採用世界氣象組織級別法，最高強度都稱之為「颱風」，所有風暴都是無命名的。 （以下各氣旋風暴資訊以氣旋風暴存在期間的最強形態為名稱。）
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The 2000 North Indian Ocean cyclone season was fairly quiet compared to its predecessor, with all of the activity originating in the Bay of Bengal. The basin comprises the Indian Ocean north of the equator, with warnings issued by the India Meteorological Department (IMD) in New Delhi. There were six depressions throughout the year, of which five intensified into cyclonic storms – tropical cyclones with winds of 65 mph (105 km/h) sustained over 3 minutes. Two of the storms strengthened into a Very Severe Cyclonic Storm, which has winds of at least 120 km/h (75 mph), equivalent to a minimal hurricane. The Joint Typhoon Warning Center (JTWC) also tracked storms in the basin on an unofficial basis, estimating winds sustained over 1 minute.
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2000 North Indian Ocean cyclone season
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2000年北印度洋氣旋季
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North Indian Ocean
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BOB01 2000 track.png
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BOB02 2000 track.png
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Cyclone 01B 2000 track.png
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Cyclone 02B 2000 track.png
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Cyclone 03B 2000 track.png
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Cyclone 04B 2000 track.png
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The 2000 North Indian Ocean cyclone season was fairly quiet compared to its predecessor, with all of the activity originating in the Bay of Bengal. The basin comprises the Indian Ocean north of the equator, with warnings issued by the India Meteorological Department (IMD) in New Delhi. There were six depressions throughout the year, of which five intensified into cyclonic storms – tropical cyclones with winds of 65 mph (105 km/h) sustained over 3 minutes. Two of the storms strengthened into a Very Severe Cyclonic Storm, which has winds of at least 120 km/h (75 mph), equivalent to a minimal hurricane. The Joint Typhoon Warning Center (JTWC) also tracked storms in the basin on an unofficial basis, estimating winds sustained over 1 minute. The first storm of the season originated toward the end of March in the Bay of Bengal, one of only five March storms at the time in that body of water. Strong wind shear, which plagued several storms during the season, caused the storm to rapidly dissipate over open waters. In August, a weak depression struck the Indian state of Andhra Pradesh, producing additional flooding after a deluge affected the area in July. There were 131 deaths in Andhra Pradesh, mostly by drownings or collapsed walls, while damage was estimated at ₹7.76 billion rupees (US$170 million ). There were two short-lived storms in October – one dissipated offshore India in the middle of the month, and the other struck Bangladesh toward the end of the month. The latter storm destroyed many homes and boats, killing 77 in Bangladesh including 52 fishermen, and damage in the Indian state of Meghalaya was estimated at ₹600 million rupees (US$13 million). The strongest storm of the season, 2000 South Indian cyclone, struck Tamil Nadu in November, causing damages of ₹700 million rupees (US$15 million) and 12 deaths. The final storm of the season hit eastern Sri Lanka, leaving 500,000 homeless and killing nine.
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2000年北印度洋氣旋季泛指在2000年全年內的任何時間，於北印度洋水域所產生的熱帶氣旋。雖然有關方面並沒有設下本颱風季的指定期限，但大部份北印度洋的熱帶氣旋通常都會於四月至十二月期間形成。 本條目的範圍僅侷限於北印度洋水域。在北印度洋產生的氣旋風暴是由隶属于的印度氣象局新德里颱風中心命名，而在該地區的熱帶低氣壓的編號都以 A/B 字母作結。 在香港天文台的天氣圖上也包括東北印度洋地區，若有熱帶氣旋形成，則採用世界氣象組織級別法，最高強度都稱之為「颱風」，所有風暴都是無命名的。 （以下各氣旋風暴資訊以氣旋風暴存在期間的最強形態為名稱。）
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