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不同海浪主导条件下的一维风涌分离方法研究

魏永亮 庞邓连 高志一 唐泽艳

魏永亮,庞邓连,高志一,等. 不同海浪主导条件下的一维风涌分离方法研究[J]. 海洋学报,2025,47(x):1–12
引用本文: 魏永亮,庞邓连,高志一,等. 不同海浪主导条件下的一维风涌分离方法研究[J]. 海洋学报,2025,47(x):1–12
Wei Yongliang,Pang Denglian,Gao zhiyi, et al. Study on Separation Method for One-Dimensional Wind-Sea and Swell under Different Dominant Wave Conditions[J]. Haiyang Xuebao,2025, 47(x):1–12
Citation: Wei Yongliang,Pang Denglian,Gao zhiyi, et al. Study on Separation Method for One-Dimensional Wind-Sea and Swell under Different Dominant Wave Conditions[J]. Haiyang Xuebao,2025, 47(x):1–12

不同海浪主导条件下的一维风涌分离方法研究

基金项目: 国家自然科学基金项目(41976174;41606196);农业农村部全球渔业资源调查监测评估项目(D-8025-24-5002)。
详细信息
    作者简介:

    魏永亮(1983—),男,山东潍坊人,副教授,主要从事海洋微波遥感研究。E-mail:yl-wei@shou.edu.cn

    通讯作者:

    高志一,男,高级工程师,研究方向为海浪理论与小尺度海气相互作用。E-mail: gaozy@nmefc.cn

Study on Separation Method for One-Dimensional Wind-Sea and Swell under Different Dominant Wave Conditions

  • 摘要: 海洋中的混合浪通常由风浪和涌浪以一定比例组成,因研究和应用等需求经常需要分离其中的风浪和涌浪。本文针对现有四种代表性一维谱风涌分离方法(1D法):PM法(Pierson-Moskowitz)、改进的PM法、JP法(Jesús-Portilla)和频谱积分法,利用中法海洋卫星上搭载的波谱仪提供的二维海浪谱数据,对比分析了纯风浪、风浪为主、涌浪为主和纯涌浪四种海浪主导情况下的分离结果,结果表明:(1)PM法和改进的PM法分别在风浪为主和涌浪为主时各有更好的分离效果;(2)JP法整体表现较差,对不同海浪主导条件的响应不敏感;频谱积分法在风浪占比较大时效果更佳;(3)随着混合浪中涌浪比例的增加,适当增大PM法中分离频率的比例系数可提升分离精度。在此基础上结合波龄提出了一种分段PM法,通过调整分离频率的比例系数,在风浪主导和涌浪主导的条件下分别取1.03和1.1时,得到的分离结果更为精确。
  • 图  1  2022年11月1日04时37分SWIM二维谱及分离的三个波分量

    (a) 第一波分量;(b) 第二波分量;(c) 第三波分量;(d) 三个波分量组成的总海浪谱

    Fig.  1  The 2D SWIM spectrum and three separated wave components at 04:37 on November 1, 2022

    (a)First wave component; (b) Second wave component; (c) Third wave component; (d) Combined spectrum of three components

    图  2  2022年11月1日04时37分SWIM一维谱风涌组成情况

    (a) 各波分量一维谱;(b) 各频率的峰值波向和风向的余弦值分布

    Fig.  2  Wind-sea and swell composition of the 1D SWIM spectrum at 04:37 on November 1, 2022

    (a) 1D spectra of wave components; (b) Distribution of the cosine of the angle between peak wave direction and wind direction across frequencies

    图  3  四种1D法与2D法风涌分离结果对比

    (a)(e) PM法分离结果;(b)(f) 改进的PM法分离结果;(c)(g) JP法分离结果;(d)(h) 频谱积分法分离结果;下同

    Fig.  3  Comparison of wind-sea and swell separation results using four 1D methods and 2D method

    (a)(e) Separation results using PM method; (b)(f) Separation results using improved PM method; (c)(g) Separation results using JP method; (d)(h) Separation results using spectral integral method. Similar explanation for the following figures

    图  4  风浪为主时的风涌分离结果

    Fig.  4  Separation results of wind-sea and swell when wind-sea dominates

    图  5  纯风浪时的风涌分离结果

    Fig.  5  Separation results of wind-sea and swell under pure wind-sea conditions

    图  6  涌浪为主时的风涌分离结果

    Fig.  6  Separation results of wind-sea and swell when wind-sea dominates

    图  7  纯涌浪下的风涌分离结果

    Fig.  7  Separation results of wind-sea and swell under swell dominates

    图  8  四种海浪情况下分离结果的统计指标随比例系数变化的变化情况

    (a)(e) 纯风浪时的分离结果;(b)(f) 风浪为主时的分离结果;(c)(g) 涌浪为主时的分离结果;(d)(h) 纯涌浪时的分离结果

    Fig.  8  The variation of statistical indicators of separation results under four different wave conditions as the ratio coefficient changes

    (a)(e) Separation results under pure wind-sea conditions; (b)(f) Separation results when wind-sea dominates; (c)(g) Separation results when swell dominates; (d)(h) Separation results under pure swell conditions

    图  9  分段调整比例系数后的PM法风涌分离结果

    (a): 分离的风浪结果对比;(b): 分离的涌浪结果对比,下同

    Fig.  9  Separation results of the PM method with piecewise-adjusted ratio coefficients

    (a): Comparison of Separated Wind-Sea Results; (b): Comparison of Separated Swell Results; similar for the following figures.

    图  10  分段PM法的风涌分离结果

    Fig.  10  Separation results of wind-sea and swell using the piecewise PM method

    表  1  分段调整比例系数后的PM法与其他PM法的风涌分离结果比较

    Tab.  1  Comparison of separation results between the piecewise-adjusted PM method and other PM methods

    rRMSE/mBias/m
    原始的PM法(风/涌)0.87/0.780.72/0.60−0.45/0.26
    改进的PM法(风/涌)0.88/0.850.50/0.490.12/−0.13
    分段调整PM法后(风/涌)0.94/0.930.36/0.32−0.06/0.02
    下载: 导出CSV

    表  2  分段PM法与其他PM法的风涌分离结果比较

    Tab.  2  Comparison of separation results between Piecewise PM Method and other PM Methods

    rRMSE/mBias/m
    原始的PM法(风/涌)0.87/0.780.72/0.60−0.45/0.26
    改进的PM法(风/涌)0.88/0.850.50/0.490.12/−0.13
    分段PM法(风/涌)0.90/0.880.46/0.42−0.03/−0.04
    下载: 导出CSV
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  • 收稿日期:  2024-09-23
  • 修回日期:  2025-04-22
  • 网络出版日期:  2025-05-26

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