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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Asymptotic behavior of frequency and wave number spectra of nearshore shoaling and breaking waves
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Asymptotic behavior of frequency and wave number spectra of nearshore shoaling and breaking waves

机译:近岸浅滩和破碎波的频率和波数谱的渐近行为

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Wave number spectra from shoaling and breaking waves in five laboratory tests are compared to a recently published parameterization describing the evolutionary characteristics of surf zone wave spectra. This parameterization proposes two regions in which different wave number spectral shapes are present; the Zakharov range (2.5 k p ≤ k ≤ 1/h) has a k -4/3 dependence, while the Toba range (k > 1/h) has a k -5/2 shape. Comparison to laboratory data reveals that the spectral slopes from the Zakharov range of the data trend toward increased agreement with the parameterization in the range of incipient breaking. In contrast, the spectral slopes from the Toba range evolve slowly, likely owing to nonlinear interactions with lower, more energetic wave numbers. However, in the inner surf zone the spectral shape for both parameterized ranges tend toward k -2 (or equivalently, f -2 in shallow water). The dissipation coefficient α(f) is extracted from time series of free surface elevations; it is found that α(f) has a reciprocal frequency dependence with that of the frequency spectra S(f) of the data, and that this correspondence increases as the waves enter the surf zone. Additionally α(f) ~ 1/S(f) ~ f 2 in the inner surf zone. It is concluded that the wave number spectrum parameterization, particularly in the Zakharov range, reasonably describes the spectral shape while the surf zone is still only partially saturated. However, continued breaking moves the spectral shape away from the parameterized slope toward a f -2 (or k~-2) spectral shape, representative of the sawtooth-like shape of surf zone waves. This spectral shape is a clear inner surf zone asymptote.
机译:比较了在五个实验室测试中来自浅滩和破碎波的波数谱与最近发布的描述冲浪区波谱演变特征的参数化。该参数化提出了两个区域,其中存在不同的波数频谱形状。 Zakharov范围(2.5 k p≤k≤1 / h)具有k -4/3依赖性,而Toba范围(k> 1 / h)具有k -5/2形状。与实验室数据的比较表明,从数据的Zakharov范围开始的光谱斜率与初始破裂范围中的参数化趋势趋于一致。相反,来自Toba范围的光谱斜率发展缓慢,这可能是由于与更低,更高能波数的非线性相互作用所致。但是,在内部冲浪区中,两个参数化范围的光谱形状都趋向于k -2(或等效地,在浅水中为f --2)。从自由表面标高的时间序列中提取耗散系数α(f);发现α(f)与数据的频谱S(f)具有倒数频率依赖性,并且随着波进入冲浪区,这种对应关系增加。另外,在内冲浪区中,α(f)〜1 / S(f)〜f 2。结论是,波谱频谱参数化(特别是在Zakharov范围内)合理地描述了频谱形状,而海浪区仍仅部分饱和。然而,连续的破坏使光谱形状从参数化的斜率移向f --2(或k〜-2)光谱形状,代表了波状波的锯齿状。该频谱形状是清晰的内部冲浪区渐近线。

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