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    冯鑫, 王刚, 张甲波, 刘会欣. 台风风暴潮灾害风险评估区划与综合防潮措施研究[J]. 中国防汛抗旱, 2022, 32(11): 37-43. DOI: 10.16867/j.issn.1673-9264.2022092
    引用本文: 冯鑫, 王刚, 张甲波, 刘会欣. 台风风暴潮灾害风险评估区划与综合防潮措施研究[J]. 中国防汛抗旱, 2022, 32(11): 37-43. DOI: 10.16867/j.issn.1673-9264.2022092
    FENG Xin, WANG Gang, ZHANG Jiabo, LIU Huixin. Research on risk assessment zoning of typhoon storm surge disaster and comprehensive tide prevention measures[J]. China Flood & Drought Management, 2022, 32(11): 37-43. DOI: 10.16867/j.issn.1673-9264.2022092
    Citation: FENG Xin, WANG Gang, ZHANG Jiabo, LIU Huixin. Research on risk assessment zoning of typhoon storm surge disaster and comprehensive tide prevention measures[J]. China Flood & Drought Management, 2022, 32(11): 37-43. DOI: 10.16867/j.issn.1673-9264.2022092

    台风风暴潮灾害风险评估区划与综合防潮措施研究

    Research on risk assessment zoning of typhoon storm surge disaster and comprehensive tide prevention measures

    • 摘要: 利用ADCIRC水动力,Jelesnianski风场和气压场耦合的风暴潮数值分析模型,研究了渤海典型台风风暴潮对曹妃甸区漫滩漫堤情况的演变过程,评估出曹妃甸区的防潮现状及隐患区域,提出解决当前隐患的综合防潮措施。研究表明:在台风风暴潮的作用下,低压台风场驱动区域潮流高速运动,致使中心气压场附近的水位发生明显增加,引起的台风增水在曹妃甸沿岸为2.754 m。曹妃甸区现存的大部分防潮设施可抵御该次风暴潮的影响,仅有纳潮河南岸等少部分区域被淹没。曹妃甸北部和东部区域整体风险较小,主要风险为Ⅲ级和Ⅳ级。Ⅰ级和Ⅱ级高风险区域主要集中在入海河道两侧。研究结果对曹妃甸区防灾减灾工作具有重要的指导意义。

       

      Abstract: The ADCIRC (an ADvanced CIRCulation model for oceanic,coastal and estuarine waters)hydrodynamics, Jelesnianski wind field and pressure field coupled storm surge numerical analysis model were used to study the evolution process of typical typhoon storm surge in the Bohai Sea on the situation of floodplain and levee overtopping in Caofeidian district. The current situation of tidal protection and hidden danger areas in Caofeidian district were evaluated, and the comprehensive tidal protection measures to solve the current hidden dangers were proposed. The study showed that: under the action of typhoon storm surge, the low-pressure typhoon field drove the regional tidal current to move at a high speed, which caused the water level near the central pressure field to increase significantly. The water increase caused by typhoon was 2.754 m along the coast of Caofeidian. Most of the existing tidal-proof facilities in Caofeidian district can resist the impact of the storm surge, and only a few areas such as the south bank of the Nachao River were flooded. The overall risk in the northern and eastern parts of Caofeidian district is relatively small, and the main risks are Level Ⅲ and Ⅳ. The highrisk areas of Level I and II are mainly concentrated on both sides of the river channel entering into the sea. The results have important references for the disaster prevention and mitigation work in Caofeidian district.

       

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