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Reconstruction of the track and a simulation of the storm surge associated with the calamitous typhoon affecting the Pearl River Estuary in September 1874

机译:与影响珠江河口的灾害台风相关轨道的重建及其风暴潮的模拟,影响珠江河口9月1874年

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A typhoon struck the Pearl River Estuary in September 1874 (“Typhoon 1874”), causing extensive damage and claiming thousands of lives in the region during its passage. Like many other historical typhoons, the deadliest impact of the typhoon was its associated storm surge. In this paper, a possible track of the typhoon was reconstructed through an analysis of the historical qualitative and quantitative weather observations in the Philippines, the northern part of the South China Sea, Hong Kong, Macao, and Guangdong recorded in various historical documents. The magnitudes of the associated storm surges and storm tides in Hong Kong and Macao were also quantitatively estimated using storm surge model and analogue astronomical tides based on the reconstructed track. The results indicated that the typhoon could have crossed the Luzon Strait from the western North Pacific and moved across the northeastern part of the South China Sea to strike the Pearl River Estuary more or less as a super typhoon in the early morning on 23?September 1874. The typhoon passed about 60 km south–southwest of Hong Kong and made landfall in Macao, bringing maximum storm tides of around 4.9 m above the Hong Kong Chart Datum (http://www.geodetic.gov.hk/smo/gsi/Data/pdf/explanatorynotes.pdf, last access: 3?January 2020) at the Victoria Harbour in Hong Kong and around 5.4 m above the Macao Chart Datum (https://mosref.dscc.gov.mo/Help/ref/Macaucoord_2009_web_EN_v201702.pdf, last access: 3?January 2020) at Porto Interior (inner harbour) in Macao. Both the maximum storm tide (4.88 m above the Hong Kong Chart Datum) and maximum storm surge (2.83 m) brought by Typhoon 1874 at the Victoria Harbour estimated in this study are higher than all the existing records since the establishment of the Hong Kong Observatory in 1883, including the recent records set by super typhoon Mangkhut on 16?September 2018.
机译:一台台风在1874年9月袭击了珠江口(“台风1874”),造成广泛的伤害,并在该地区造成了成千上万的生活。像许多其他历史的台风一样,台风的最致命的影响是其相关的风暴浪涌。在本文中,通过分析菲律宾的历史定性和定量天气观测,南海,澳门北部,广东省在各种历史文件中进行了分析,重建了台风的可能轨道。利用风暴浪涌模型和基于重建轨道的模拟天文潮汐量也定量估计了港澳风暴浪涌和澳门风暴潮汐的大小。结果表明,台风可以从西北太平洋西部的吕宋海峡越过吕宋海峡,迁移南海东北部门,在清晨在23岁的时候更少地击中珠江河口的珠江口袭击了珠江口,于23岁的超级台风赛中。台风通过香港西南部约60公里,在澳门登陆,使最大的风暴潮汐约为4.9米在香港图表基准(http://www.geodetic.gov.hk/smo/gsi/数据/ pdf / deparderynotes.pdf,上次访问:3?1月2020年1月2020年)在香港的维多利亚港和澳门图表基准(https://mosref.dscc.gov.mo/help/ref/macaucoord_2009_web_en_v201702)上方约为5.4米.pdf,最后一次访问:3?1月2020年1月)在澳门的波尔图内部(内港)。 Typhoon 1874年在本研究中估计的维多利亚港口的最大风暴潮(4.88米)和最大的风暴浪涌(2.83米)估计自香港天文台以来的维多利亚港为维多利亚港的维多利亚港1883年,包括最近由Super Typhoon Mangkhut设置的纪录,2018年9月。

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