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多向不规则波浪的确定性模拟

罗丽 柳淑学 李金宣 王磊

罗丽,柳淑学,李金宣,等. 多向不规则波浪的确定性模拟[J]. 海洋学报,2020,42(9):79–86 doi: 10.3969/j.issn.0253-4193.2020.09.009
引用本文: 罗丽,柳淑学,李金宣,等. 多向不规则波浪的确定性模拟[J]. 海洋学报,2020,42(9):79–86 doi: 10.3969/j.issn.0253-4193.2020.09.009
Luo Li,Liu Shuxue,Li Jinxuan, et al. Deterministic simulation of multidirectional irregular waves[J]. Haiyang Xuebao,2020, 42(9):79–86 doi: 10.3969/j.issn.0253-4193.2020.09.009
Citation: Luo Li,Liu Shuxue,Li Jinxuan, et al. Deterministic simulation of multidirectional irregular waves[J]. Haiyang Xuebao,2020, 42(9):79–86 doi: 10.3969/j.issn.0253-4193.2020.09.009

多向不规则波浪的确定性模拟

doi: 10.3969/j.issn.0253-4193.2020.09.009
基金项目: 国家自然科学基金(51879037,51739010)。
详细信息
    作者简介:

    罗丽(1988-),女,陕西省渭南市人,博士生,从事港口、海岸和近海工程研究。E-mail:luoli881206@163.com

    通讯作者:

    柳淑学(1965-),男,河北省唐县人,研究员。E-mail:liusx@dlut.edu.cn

  • 中图分类号: P731.22

Deterministic simulation of multidirectional irregular waves

  • 摘要: 波浪波动时间过程及波列的模拟,对于开展实际波浪对于工程建筑物的作用具有重要的意义。本文采用线性叠加的单叠加模型,建立了多向不规则波浪的确定性模拟方法。基于理论模拟的规则波、单向不规则波和多向不规则波,验证了波浪确定性模拟方法的有效性。定性地对比分析了模拟波列和已知波列的一致性;定量地研究了模拟波浪在空间范围rr/Ls的误差分布情况(rr表示指定位置与给定位置的空间距离,Ls为有效波长)。并且建议,采用本文方法进行波浪确定性模拟时,最佳的浪高仪间距应小于0.12Ls
  • 图  1  波浪浪高仪的布置形式

    Fig.  1  Sketch of the wave gauges

    图  2  2号(a)和5号(b)浪高仪在T0=250/256 s,H0=0.04 m,θ=π/6时的波浪过程线

    Fig.  2  Comparison of the wave surface elevation histories for T0= 250/256 s, H0=0.04 m, θ=π/6 of No.2 (a) and No.5 (b) gauges

    图  3  理论波浪频谱(Ts=1.5 s,Hs=0.04 m)

    Fig.  3  Theoretical wave frequency spectrum (Ts=1.5 s,Hs=0.04 m)

    图  4  R/Ls为0.06和0.12时,average-θi和max-Energy-θiθEr沿fi的分布(Ts=1.5 s, Hs=0.04 m)

    Fig.  4  Variation of the θEr for average-θi and max-Energy-θi with fi for R/Ls=0.06 and R/Ls=0.12 (Ts=1.5 s, Hs=0.04 m)

    图  5  单向不规则波已知波列和模拟波列在不同rr/Ls时的对比(Ts=1.5 s,Hs=0.04 m)

    Fig.  5  Comparison of the original and simulated uni-directional irregular wave surface elevation histories (Ts=1.5 s,Hs=0.04 m)

    图  6  采用average-θi和max-Energy-θi模拟所得波浪的Ermaxrr/Ls的变化(Ts=1.5 s,Hs=0.04 m)

    Fig.  6  Variation of Ermax for simulated waves with rr/Ls using average-θi and max-Energy-θi respectively (Ts=1.5 s, Hs=0.04 m)

    图  7  R/Ls不同时,采用average-θi方法计算的θEr沿fi的分布(Ts=1.5 s,Hs=0.04 m,s=25)

    Fig.  7  Variation of θEr with fi for average-θi method with different R/Ls (Ts=1.5 s, Hs=0.04 m, s=25)

    图  8  rr/Ls=0.35,R/Ls不同时,3号浪高仪位置理论波列和确定性模拟波列的对比(Ts=1.5 s,Hs=0.04 m,s=25)

    Fig.  8  Comparison of theoretical and simulated wave surface elevation histories for different R/Ls with rr/Ls=0.35 at No.3 gauge (Ts=1.5 s, Hs=0.04 m, s=25)

    图  9  R/Ls=0.06,rr/Ls不同时,3号浪高仪位置处理论波列和确定性模拟波列的对比(Ts=1.5 s,Hs=0.04 m,s=25)

    Fig.  9  Comparison of theoretical and simulated wave surface elevation histories for different rr/Ls with R/Ls=0.06 at No.3 gauge (Ts=1.5 s, Hs=0.04 m, s=25)

    图  10  R/Ls=0.06时采用计算的average-θi和max-Energy-θi模拟所得波浪的Ermaxrr/Ls的变化(Ts=1.5 s, Hs=0.04 m, s=25)

    Fig.  10  Variation of Ermax for simulated waves with rr/Ls using average-θi and max-Energy-θi of R/Ls=0.06 (Ts=1.5 s, Hs=0.04 m, s=25)

    图  11  不同的R/Ls采用average-θi模拟所得波浪的Ermaxrr/Ls的变化(Ts=1.5 s, Hs=0.04 m, s=25)

    Fig.  11  Variation of Ermax for simulated waves with rr/Ls using average-θi with different R/Ls (Ts=1.5 s, Hs=0.04 m, s=25)

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出版历程
  • 收稿日期:  2019-08-29
  • 修回日期:  2020-06-05
  • 网络出版日期:  2021-04-21
  • 刊出日期:  2020-09-25

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