红树林存在时的波浪衰减:对不同底坡的敏感性研究

P. K. G., P. Bhaskaran
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引用次数: 39

摘要

红树林生长在热带和副热带的潮间带(海陆界面),对近岸波的整体衰减起着重要作用。波浪与红树林树干和树根的多重相互作用和底部摩擦是红树林波浪衰减的两个主要机制。早期的研究,包括分析和实验,报告了波在具有理想底部地形的植被上传播的波高呈指数衰减。但是几乎没有研究试图描述不同海底斜坡上植被对波浪衰减的特征,因为红树林通常生长在潮汐振幅大的平缓地形上。目前,正在进行若干研究,以发展人工红树林,以减少海岸灾害的风险;因此,迫切需要研究红树林在不同海底斜坡上的波浪阻尼特性。因此,本研究利用第三代波浪模型对不同海底坡度的红树林进行了波浪衰减敏感性实验。本研究揭示了在红树林存在的情况下,波浪衰减特性对不同滩坡的敏感性,旨在了解红树林的波浪衰减特性在不同底坡下的差异。在平缓坡度(1:80、1:40)下,波浪通过红树林传播到达海岸线的总能量减少百分比为93%-98%,在坡度为1:20时减少近84%,在陡坡(1:10)时减少67%。研究发现,在缓坡处,波高呈指数衰减,与前期研究结果一致,但随着底部陡度的增加,波高衰减逐渐减小,这可能与红树林存在时不同坡度的水深变化、浅滩化、破碎和反射特征有关。
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Wave attenuation in presence of mangroves: A sensitivity study for varying bottom slopes
Mangroves thrive in the intertidal areas (interface between land and sea) of tropical and sub-tropical belt and play an important role in overall attenuation of nearshore waves. Multiple interactions of waves with mangrove trunks and roots and bottom friction are the two primary mechanisms responsible for wave attenuation in mangrove forests. Earlier studies, comprising both analytical and experimental, reported an exponential decay in wave height for waves propagating over vegetation with idealized bottom topography and a few on sloping bottom. But hardly studies have attempted to characterize the wave attenuation by vegetation over varying seabed slopes since mangroves generally grow luxuriantly on gradual topography having large tidal amplitudes. Nowadays, several studies are being carried out on development of artificial mangroves to reduce the coastal hazard risks; thenceforth, there is an imperative requirement to study the wave damping characteristics of mangroves on varying seabed slopes. Consequently, this study performs sensitivity experiments to analyze the wave attenuation over mangroves with different sea-bottom slopes using a third-generation wave model. The study exposes sensitivity of wave attenuation characteristics to different beach slopes in the presence of mangroves and aims at understanding how the wave attenuation characteristics by mangroves differ with varying bottom slopes. The total percentage energy reduction for waves reaching the shoreline after propagating through mangroves on mild slope (1:80, 1:40) is observed to be 93%–98%, nearly 84% for 1:20 slope, and 67% for steep slope (1:10). The study reveals that the wave height decays exponentially for the mild slope and found to be consistent with the earlier studies, but as the degree of bottom steepness increases, the wave height reduction becomes gradual, and this can be attributed to the water depth variation, shoaling, breaking, and reflection characteristics associated with different slopes, in the presence of mangroves.
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