黄世昌,谢亚力,严聿晗,等. 舟山本岛海域“烟花”台风风暴高潮位研究[J]. 水利水运工程学报,2021(6):1-8. doi: 10.12170/20210915002
引用本文: 黄世昌,谢亚力,严聿晗,等. 舟山本岛海域“烟花”台风风暴高潮位研究[J]. 水利水运工程学报,2021(6):1-8. doi: 10.12170/20210915002
(HUANG Shichang, XIE Yali, YAN Yuhan, et al. Study of high water level during Typhoon In-Fa in the sea area of Zhoushan island[J]. Hydro-Science and Engineering, 2021(6): 1-8. (in Chinese)). doi: 10.12170/20210915002
Citation: (HUANG Shichang, XIE Yali, YAN Yuhan, et al. Study of high water level during Typhoon In-Fa in the sea area of Zhoushan island[J]. Hydro-Science and Engineering, 2021(6): 1-8. (in Chinese)). doi: 10.12170/20210915002

舟山本岛海域“烟花”台风风暴高潮位研究

Study of high water level during Typhoon In-Fa in the sea area of Zhoushan island

  • 摘要: 近年来登陆或严重影响浙江的强台风频率上升,北移次数增多,对舟山本岛及邻近岛屿经济活动威胁越来越大,开展舟山本岛风暴高潮位研究十分必要。分析了"烟花"台风在舟山本岛造成的风暴高潮位分布,基于海区的实测潮位资料及构建的风暴潮模型计算的风暴高潮位,揭示了本次风暴高潮位总体东部低、西部高、中部局部低值区的特征,中部局部低值区与天文高潮位的分布有关。本岛海域“烟花”台风风暴高潮位差异可达0.5 m以上;“烟花”台风若在本岛天文大潮高潮位登陆,定海至岱山风暴高潮位会继续抬高0.1~0.4 m;若南移至大目涂位置且在高潮位登陆则会造成本岛周边更高的风暴高潮位,超过本次风暴高潮位0.2~0.8 m。应高度重视风暴潮高潮位的区域差异性和变化特征,进一步提高区域风暴潮灾害防御能力。。

     

    Abstract: The frequency of strong typhoons landing or seriously affecting Zhejiang has increased, and the number of northward shifts has increased in recent years. Typhoons threaten the economic activities of Zhoushan Island and neighboring islands more and more, so it is necessary to carry out researches on storm high tidal level around the coast of Zhoushan island. We have analyzed the distribution of the storm high tidal level caused by the Typhoon In-Fa that has the greatest impact on the sea zone of Zhoushan since the beginning of this century. The measured tidal data and the simulated result of storm surge by the model constructed reveal that the storm high tidal level caused by the Typhoon In-Fa overall is low in the east and high in the west of the sea zone, accompanied by the characteristics of the central low-value area, which is related to the central low-value area of the astronomical high tide level. The difference of storm high tide level during the Typhoon In-Fa in the sea area of the island can reach more than 0.5 m. If the Typhoon In-Fa lands at astronomical high tidal level, the storm high tidal level at Dinhai and Daishan will increase by 0.1~0.4 m. If it moves southward to the Damutu location and lands at the high tide level, it will cause a higher storm high tide level around the island, which exceeds the actual storm high tide level by 0.2 to 0.8 m. Great attention should be paid to the regional variability and changing characteristics of storm surge high tide levels, which is conducive to improving regional defense capabilities of storm surge disasters.

     

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