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Cyclone Martin : ウィキペディア英語版 | Cyclone Martin
Severe Tropical Cyclone Martin was the deadliest tropical cyclone of the 1997–98 South Pacific cyclone season. The system was first noted as a weak tropical disturbance on October 27, to the north of the Northern Cook Islands. Over the next few days atmospheric convection surrounding the system remained disorganized, as it moved towards the southwest and was affected by strong upper-level north-easterly winds and moderate to strong vertical wind shear. The system was subsequently named Martin during October 31, after it had rapidly developed further and shown a marked improvement organization. ==Meteorological history==
On October 27, 1997 the Fiji Meteorological Service started to monitor a weak tropical disturbance, that had developed to the north of the Northern Cook Islands. Over the next few days atmospheric convection surrounding the system remained disorganised, as the system moved to the southwest and was affected by strong upper-level north-easterly winds and moderate to strong vertical wind shear. Late on October 30, the United States Naval Pacific Meteorology and Oceanography Center (NPMOC) designated the disturbance as Tropical Cyclone 04P, as it had become a tropical depression.〔 During the next day the system started to show a marked improvement in organisation and began rapidly developing, before RSMC Nadi named it Martin at 1500 UTC after it had developed into a category 1 tropical cyclone on the Australian tropical cyclone intensity scale.〔 When it was named, Martin was located about to the west of Manihiki Atoll in the Northern Cook Islands and had started to re-curve and move towards the south-east during that day.〔 Early on November 1, RSMC Nadi reported that the system had become a category 2 tropical cyclone on the Australian scale, before the NPMOC reported that Martin had become equivalent to a category one hurricane on the Saffir-Simpson hurricane wind scale (SSHWS).〔 During that day as the cyclone season officially started, Martin continued to intensify and became a category 3 severe tropical cyclone on the Australian scale, as it passed about to the south of Manihiki.〔〔 During November 2, the system continued to intensify as it moved towards the southeast and became equivalent to a category 2 hurricane on the SSHWS, as it moved towards the French Polynesian Society Islands of Bellingshausen, Mopelia and Scilly.〔〔〔 During the next day, Martin passed near the Society Islands as it developed an eye, before RSMC Nadi reported at 06:00 UTC that the system had peaked as a category 3 severe tropical cyclone with 10-minute sustained wind speeds of 155 km/h (100 mph).〔 The NPMOC also reported at around that time that Martin had peaked with 1-minute sustained windspeeds of 185 km/h (115 mph), which made it equivalent to a category 3 hurricane on the SSHWS.〔〔 After peaking in intensity Martin started to weaken, as it interacted with a frontal system and started to accelerate towards the south-southeast.〔 During November 4, Martin passed within of Tahiti as it became a category 2 tropical cyclone and started to transition into an extratropical cyclone.〔〔 Later that day, the NPMOC issued their final advisory on system as it had become equivalent to a tropical depression, vertically sheared with its surface center dislocated about from its upper level center.〔 During November 5, Martin weakened below tropical cyclone intensity, before it was last noted on November 8 in the Southeastern Pacific ocean over to the southeast of Adamstown in the Pitcairn Islands.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Cyclone Martin」の詳細全文を読む
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