自由长波产生:断点强迫与束缚波释放

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Stephanie Contardo, Ryan J. Lowe, Francois Dufois, Jeff E. Hansen, Graham Symonds
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引用次数: 0

摘要

当风浪在近岸破碎时,通过断点强迫和束缚波释放两种机制产生自由长(次重力)波。先前的研究强调,在陡坡上较低频率群的断裂有利于断点强迫产生长波,而在温和斜坡上较高频率群的断裂有利于束缚波的释放。然而,没有研究建立并证明了每种机制何时占主导地位的定量阈值。在本文中,我们使用一维线性数值模型来量化每种机制,并评估它们在自由长波产生中的相对优势,作为波浪和测深参数的函数。结果表明,由于每种机制产生的自由长波之间的相位差,断点强迫和束缚波释放的单独贡献与两种机制产生的总长波能量并不线性相加。这些机制的组合总是导致净长波振幅较小。归一化的床坡参数在区分断点强迫释放机制和束缚波释放机制的优势方面是有效的。发现断点强迫的效率与河床坡度、波群频率和短波周期无关。因此,每种机制对长波产生的相对重要性主要取决于束缚波释放的效率,而束缚波释放的效率随这些参数的变化而变化。总的来说,在大多数情况下,束缚波释放机制往往占主导地位,除了发生在陡坡上的低次重力频率的情况(例如,典型的珊瑚礁环境)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Free Long Wave Generation: Breakpoint Forcing Versus Bound Wave Release

Free Long Wave Generation: Breakpoint Forcing Versus Bound Wave Release

When wind waves break in the nearshore, free long (infragravity) waves are generated through two mechanisms: breakpoint forcing and bound wave release. Previous studies have highlighted that lower frequency groups breaking on steep slopes favor long wave generation by breakpoint forcing, whereas higher frequency groups breaking on mild slopes favor bound wave release. However, no study has established and demonstrated quantitative thresholds for when each mechanism will dominate. In this paper, we use a one-dimensional linear numerical model to quantify each mechanism and assess their relative dominance in free long wave generation, as a function of wave and bathymetry parameters. The results show that the individual contributions of breakpoint forcing and bound wave release do not add up linearly to the total long wave energy generated from both mechanisms due to the phase differences between free long waves generated from each mechanism. The combination of mechanisms always results in a net smaller long wave amplitude. The normalized bed slope parameter is shown to be effective in differentiating between the dominance of the breakpoint-forced and bound wave release mechanisms. The efficiency of breakpoint forcing is found to be independent of bed slope, wave group frequency and short-wave period. Therefore, the relative importance of each mechanism to long wave generation depends mainly on the efficiency of the bound wave release, which varies with these parameters. Overall, the bound wave release mechanism tends to dominate under most conditions, except for cases with low infragravity frequencies that occur on steep slopes (e.g., typical of reef environments).

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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