1912 Jamaica hurricane
http://dbpedia.org/resource/1912_Jamaica_hurricane
1912年牙买加飓风(英語:1912 Jamaica hurricane)是这年11月在牙买加缓慢徘徊、降下瓢泼大雨并引发重大洪灾的一个热带气旋,也是1912年大西洋飓风季的最强风暴,于11月11日清晨经西南加勒比海的低气压区发展而成。气旋起初缓慢向西北移动,之后转向东北偏北,于11月13日达到飓风强度。接下来风暴继续缓慢增强,但转向东北移动后强化速度有所加快。11月17日清晨,气旋达到持续风速每小时185公里的最高强度,在现代萨菲尔-辛普森飓风等级下已达三级飓风标准。风暴继续向东北偏北移动,于11月18日从牙买加内格里尔附近登陆。飓风上岸后不断减弱,之后又回到加勒比海,于11月20日在牙买加北侧弱化成热带风暴。气旋向西穿越加勒比海,最终于11月22日在大开曼西南方向洋面逐渐消散。 牙买加降下暴雨,部分地区降雨量高达910毫米。该岛北部和东部多座桥梁严重受损,飓风产生的狂风将约四分之一的香蕉树摧毁,多地电报线路中断,铁轨也受到狂风暴雨的沉重打击。岛屿周边海域波涛汹涌,滨海萨凡纳几乎被完全摧毁,有42人丧生。牙买加西部约有100幢民宅被毁,5000套建筑受损或毁于一旦。整个牙买加约有100人遇难,损失数额约150万美元(1912年美元)。此外,气旋还在古巴关塔那摩湾区域引发大面积洪灾,共夺走五条人命。
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The 1912 Jamaica hurricane was a slow-moving tropical cyclone that meandered about the island of Jamaica, causing torrential rainfall and severe flooding in November 1912. The strongest hurricane in the Atlantic that year, the cyclone formed from a low pressure area in the southwestern Caribbean Sea early on November 11. Initially, the storm tracked slowly to northwest, before eventually curving north-northeastward. Late on November 13, the cyclone became a hurricane. After reaching hurricane status, further deepening was slow, though after recurving toward northeastward, the storm began to quicken its rate of intensification. Early on November 17, the system peaked as a 115 mph (185 km/h) Category 3 hurricane on the modern day Saffir–Simpson hurricane wind scale. It continued north-northe
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1912 Jamaica hurricane
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1912年牙买加飓风
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Surface weather analysis of the hurricane skirting Jamaica on November 18
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The 1912 Jamaica hurricane was a slow-moving tropical cyclone that meandered about the island of Jamaica, causing torrential rainfall and severe flooding in November 1912. The strongest hurricane in the Atlantic that year, the cyclone formed from a low pressure area in the southwestern Caribbean Sea early on November 11. Initially, the storm tracked slowly to northwest, before eventually curving north-northeastward. Late on November 13, the cyclone became a hurricane. After reaching hurricane status, further deepening was slow, though after recurving toward northeastward, the storm began to quicken its rate of intensification. Early on November 17, the system peaked as a 115 mph (185 km/h) Category 3 hurricane on the modern day Saffir–Simpson hurricane wind scale. It continued north-northeastward and made landfall near Negril, Jamaica, on November 18. The storm weakened continually after landfall and reentry into the Caribbean Sea. On November 20, the hurricane weakened to a tropical storm north of Jamaica. The system tracked westward across the Caribbean, before dissipating on November 22 to the southwest of Grand Cayman. Heavy rainfall was reported in Jamaica, with as much as 36 inches (910 mm) of precipitation recorded in some areas. Several bridges were severely damaged in the northern and eastern portions of the island. Strong winds generated by the storm destroyed approximately 25% of banana trees, while telegraph lines were downed in a number of places. Railway lines were also heavily damaged by the winds and rain. Rough seas also lashed the island, with Savanna-la-Mar suffering near complete destruction and 42 deaths in that city alone. Across western Jamaica, roughly a hundred homes were destroyed, while 5,000 buildings were damaged or demolished. About 100 fatalities and $1.5 million (1912 USD) in damage occurred in Jamaica. Extensive flooding and five fatalities occurred in Cuba in the Guantánamo Bay area.
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1912年牙买加飓风(英語:1912 Jamaica hurricane)是这年11月在牙买加缓慢徘徊、降下瓢泼大雨并引发重大洪灾的一个热带气旋,也是1912年大西洋飓风季的最强风暴,于11月11日清晨经西南加勒比海的低气压区发展而成。气旋起初缓慢向西北移动,之后转向东北偏北,于11月13日达到飓风强度。接下来风暴继续缓慢增强,但转向东北移动后强化速度有所加快。11月17日清晨,气旋达到持续风速每小时185公里的最高强度,在现代萨菲尔-辛普森飓风等级下已达三级飓风标准。风暴继续向东北偏北移动,于11月18日从牙买加内格里尔附近登陆。飓风上岸后不断减弱,之后又回到加勒比海,于11月20日在牙买加北侧弱化成热带风暴。气旋向西穿越加勒比海,最终于11月22日在大开曼西南方向洋面逐渐消散。 牙买加降下暴雨,部分地区降雨量高达910毫米。该岛北部和东部多座桥梁严重受损,飓风产生的狂风将约四分之一的香蕉树摧毁,多地电报线路中断,铁轨也受到狂风暴雨的沉重打击。岛屿周边海域波涛汹涌,滨海萨凡纳几乎被完全摧毁,有42人丧生。牙买加西部约有100幢民宅被毁,5000套建筑受损或毁于一旦。整个牙买加约有100人遇难,损失数额约150万美元(1912年美元)。此外,气旋还在古巴关塔那摩湾区域引发大面积洪灾,共夺走五条人命。
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