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南沙群岛礁概化地形上拍岸浪数值模拟与统计分析

曹广颂 朱首贤 张文静 聂屿

曹广颂,朱首贤,张文静,等. 南沙群岛礁概化地形上拍岸浪数值模拟与统计分析[J]. 海洋学报,2020,42(1):22–30,doi:10.3969/j.issn.0253−4193.2020.01.003
引用本文: 曹广颂,朱首贤,张文静,等. 南沙群岛礁概化地形上拍岸浪数值模拟与统计分析[J]. 海洋学报,2020,42(1):22–30,doi:10.3969/j.issn. 0253−4193.2020.01.003
Cao Guangsong,Zhu Shouxian,Zhang Wenjing, et al. Numerical simulations and statistical analysis of surf on the generalized topography of the Nansha Islands[J]. Haiyang Xuebao,2020, 42(1):22–30,doi:10.3969/j.issn.0253−4193.2020.01.003
Citation: Cao Guangsong,Zhu Shouxian,Zhang Wenjing, et al. Numerical simulations and statistical analysis of surf on the generalized topography of the Nansha Islands[J]. Haiyang Xuebao,2020, 42(1):22–30,doi:10.3969/j.issn.0253−4193.2020.01.003

南沙群岛礁概化地形上拍岸浪数值模拟与统计分析

doi: 10.3969/j.issn.0253-4193.2020.01.003
基金项目: 国家自然科学基金(41076048,41376012);中央高校基本科研业务费项目(2018B46914)。
详细信息
    作者简介:

    曹广颂(1992—),男,江苏省连云港市人,主要从事海洋动力学与数值模拟研究。E-mail:824708267@qq.com

    通讯作者:

    朱首贤,男,副教授,研究方向为海洋动力学与数值模式、河口海岸水沙运动及遥感。E-mail:zhushouxian@vip.sina.com

  • 中图分类号: P731.2

Numerical simulations and statistical analysis of surf on the generalized topography of the Nansha Islands

  • 摘要: 南沙群岛珊瑚岛礁众多,大多数岛礁具有向海坡陡峭、外礁坪比较平缓的特征。将南沙群岛岛礁的迎浪向地形概化为陡坡和缓坡组成的双斜坡,采用FUNWAVE-TVD模式数值模拟概化地形上的波浪,根据模拟的破碎波高分析其拍岸浪特征。对拍岸浪数值模拟结果进行比较分析,向海坡的坡度对拍岸浪影响不大,外礁坪上拍岸浪高随地形坡度增大而略有增大;向海坡和外礁坪交界位置(即坡折点)水深对拍岸浪有比较明显的影响,拍岸浪高随坡折点水深增大而减小;拍岸浪高随入射波高和波周期增大而增大。利用大量的拍岸浪数值模拟数据对国内外5种统计模型进行检验,并且基于拍岸浪数值模拟数据建立了3种南沙群岛岛礁拍岸浪统计模型,计算结果显示这些模型适用性较好。
  • 图  1  南沙群岛珊瑚礁体类型[16]

    Fig.  1  Types of the coral reefs of the Nansha Islands

    图  2  环礁地貌单元划分[16]

    Fig.  2  The landsacpe of the coral atoll[16]

    图  3  波浪水槽实验设置

    Fig.  3  The sketch of the wave flume experiment

    图  4  数值模拟与水槽实验的波高比较

    Fig.  4  The wave heights from the wave flume experiment and numerical simulation

    图  5  南沙群岛岛礁波浪数值模拟的概化地形

    Fig.  5  The generalized topography for the numerical simulations of wave on the Nansha Islands reefs

    图  6  不同入射波高和波周期的波浪模拟结果

    Fig.  6  The simulated wave heights impacted by the incident wave heights and periods

    图  7  向海坡坡度对破碎波高影响的数值模拟结果

    Fig.  7  The simulated breaking wave heights impacted by the slopes of seaward reef slopes

    图  8  外礁坪坡度对破碎波高影响的数值模拟结果

    Fig.  8  The simulated breaking wave heights impacted by the slopes of outer reef flats

    图  9  坡折点水深对破碎波高影响的数值模拟结果

    Fig.  9  The simulated breaking wave heights impacted by the depths at slope turnings

    图  10  统计模型与数值模拟的破碎波高

    Fig.  10  The breaking wave heights from the statistical models and the numerical simulations

    图  11  A模型、B模型、C模型和数值模拟的破碎波高

    Fig.  11  The breaking wave heights from the A, B, C models and the numerical simulations

    表  1  720个波浪数值模拟算例的参数设置

    Tab.  1  The 720 cases of wave numerical simulations

    外礁坪坡度s2坡折点水深hr/m入射波周期T0/s入射波高H0/m
    1∶30
    1∶40
    1∶50
    1∶601.00.5
    1∶701.551.0
    1∶802.081.5
    1∶1002.510 2.0
    1∶1503.0
    1∶300
    1∶500
    1∶700
    1∶1 000
    下载: 导出CSV
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出版历程
  • 收稿日期:  2019-04-28
  • 修回日期:  2019-09-04
  • 网络出版日期:  2021-04-21
  • 刊出日期:  2020-01-25

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