首页> 外文期刊>Journal of geophysical research. Earth Surface: JGR >Growth of river mouth bars in sheltered bays in the presence of frontal waves
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Growth of river mouth bars in sheltered bays in the presence of frontal waves

机译:正面波存在下庇护海湾河口坝的生长

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摘要

One of the key processes for the formation of deltas and their fluvial networks is the deposition of mouth bars in front of prograding distributaries. Waves influence mouth bar growth, but it is not clear how and to what extent. Toward this end, we conduct a modeling study on deltas forming in sheltered bays, where waves are locally generated and both longshore currents and surf zone are absent. We focus on the simplified case of a homopycnal river plume subject to frontal wave attack, and we begin by isolating the effects of waves on jet spreading. An analytical model for the hydrodynamic interaction between incoming waves and a turbulent expanding jet is developed and tested with the numerical model Delft3D coupled to the wave model SWAN. Both the analytical model and Delft3D predict that incoming surface gravity waves increase the spreading of the jet and the interaction between wave and current boundary layers causes an increase in bottom friction. To investigate how waves influence mouth bar morphodynamics, a set of numerical simulations is run with Delft3D-SWAN utilizing a geometry and wave characteristics typical of sheltered bays. Our numerical results show that in the presence of waves, mouth bars form up to 35% closer to the river mouth and 40% faster when compared to cases without waves. The distance from the river mouth to the stagnated mouth bar decreases with increasing wave height and wave period. The timescale of bar formation is inversely proportional to wave height and directly proportional to wave period. Our modeling study suggests that wave influence on mouth bar growth is complex. Small waves, like the ones modeled here, promote mouth bar formation via increased jet spreading and faster formation time, which in turn should create deltas with more distributary channels. On the other hand, large waves suppress mouth bar formation, as seen in other studies, leading to fewer distributary channels. Key Points Waves increase the expansion of the river-mouth jet by enhancing bed friction In presence of waves the bar forms at a shorter distance from river mouth Mouth bars form faster when waves are present
机译:三角洲及其河流网络形成的关键过程之一是在逐渐增加的分流点之前沉积口条。波浪会影响口巴的生长,但尚不清楚如何以及在何种程度上。为此,我们对避难海湾中形成的三角洲进行了建模研究,在避难海湾中,波浪是局部产生的,而没有近岸水流和冲浪区。我们将重点放在遭受前波攻击的同向河羽状流的简化情况上,并从隔离波对射流扩展的影响开始。使用耦合到波浪模型SWAN的数值模型Delft3D,开发并测试了入射波和湍流膨胀射流之间的水动力相互作用的解析模型。分析模型和Delft3D均预测,进入的表面重力波会增加射流的散布,并且波与电流边界层之间的相互作用会导致底部摩擦增大。为了研究波浪如何影响口栏的形态动力学,使用Delft3D-SWAN进行了一组数值模拟,利用了庇护湾的典型几何形状和波浪特征。我们的数值结果表明,在有波浪的情况下,与没有波浪的情况相比,口条的形成最接近河口35%,而速度则快40%。从河口到停滞的口岸杆的距离随着波高和波周期的增加而减小。条形形成的时间尺度与波高成反比,与波周期成正比。我们的模型研究表明,波浪对口巴生长的影响非常复杂。像此处建模的小波一样,小波通过增加射流散布和更快的形成时间来促进口形条的形成,而这反过来又应该创建具有更多分布通道的三角洲。另一方面,如其他研究所示,大浪会抑制口巴的形成,从而导致分配通道减少。要点波浪通过增强河床摩擦力来增加河口射流的膨胀。波浪存在时,条形物与河口的距离较短。

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