Morphodynamic Evolution(形态动力学演化)研究综述
Morphodynamic Evolution 形态动力学演化 - This chapter demonstrates the possibilities for the application of a robust modeling system to assess the morphodynamic evolution and sediment budget and pathways. [1] The study focused on the question of how the natural and human forcing has affected the morphodynamic evolution of bars in the middle Yangtze River. [2] The morphodynamic evolution of the shape of dunes and piles of granular material is largely dictated by avalanching phenomena, acting when the local slope gets steeper than a critical repose angle. [3] It is also found that storm waves can be very significant to morphodynamic evolution of this tide-dominated estuary. [4] Presently, the curvature effects are minute owned to the morphodynamic evolution of the Sand Engine. [5] In addition, the effects of morphodynamic evolution in different regions (i. [6] Results concerning the morphodynamic evolution of bed topography in the channel and in the seaward basin are discussed in sections 3 and 4. [7] This work proposes a new dredging strategy for tidal inlets and analyzes its morphodynamic evolution by means of numerical modeling. [8] The effect of vegetation in controlling the morphodynamic evolution under wave attack is greater when the sand fraction increases, thus contributing to the development of small steep scarps. [9] Quarter-diurnal tidal constituents are linked to tidal asymmetries and play a role in the morphodynamic evolution of inlets, estuaries and lagoons. [10] Morphodynamic evolution in an alluvial river is usually controlled by various boundary conditions. [11] The complex interactions between flow hydrodynamics, sediment transport, geometry, and changes in base level control the morphodynamic evolution of tidal channels, inlets, and estuaries. [12] We investigate a 250-year period of morphodynamic evolution including a 150-year hindcast and a 100-year forecast with different SLR scenarios. [13] Monitoring the bio-morphodynamic evolution of these environments is therefore a crucial task that requires a detailed and holistic scrutiny. [14] Morphodynamic evolution and adaptability of nourished beaches. [15] The current study examined the indicators of the morphodynamic evolution in the littoral system including the Oum Er-Rbia estuary and the neighboring beaches over 1970–2017. [16]本章展示了应用稳健的建模系统来评估形态动力学演变和沉积物收支和路径的可能性。 [1] 该研究的重点是自然和人为强迫如何影响长江中游坝体的形态演化。 [2] 沙丘和颗粒材料堆形状的形态动力学演变很大程度上取决于雪崩现象，当局部坡度变得比临界安息角更陡时起作用。 [3] 还发现风暴波对这个以潮汐为主的河口的形态动力学演化非常重要。 [4] 目前，曲率效应在沙机的形态动力学演变中占有一席之地。 [5] 此外，不同区域形态动力学演化的影响（i. [6] 第 3 节和第 4 节讨论了有关河道和向海盆地中河床地形形态动力学演变的结果。 [7] 本工作提出了一种新的潮汐入口疏浚策略，并通过数值模拟分析了其形态动力学演化。 [8] 当沙粒比例增加时，植被对波浪冲击下形态动力学演化的控制作用更大，从而有助于小陡峭陡坡的发育。 [9] 四分之一昼夜潮汐成分与潮汐不对称性有关，并在入口、河口和泻湖的形态动力学演变中发挥作用。 [10] 冲积河流的形态动力学演化通常受各种边界条件的控制。 [11] 流动流体动力学、泥沙运输、几何形状和基准面变化之间的复杂相互作用控制着潮道、入口和河口的形态动力学演变。 [12] 我们调查了 250 年的形态动力学演变，包括 150 年的后报和 100 年不同 SLR 情景的预测。 [13] 因此，监测这些环境的生物形态动力学演变是一项至关重要的任务，需要进行详细和全面的审查。 [14] 营养海滩的形态动力学演变和适应性。 [15] 目前的研究检查了 1970-2017 年包括 Oum Er-Rbia 河口和邻近海滩在内的沿岸系统形态动力学演变的指标。 [16]
Term Morphodynamic Evolution
The model was subsequently applied to assess the long-term morphodynamic evolution of the estuary in response to changes in various forcings, with results that are conceptually and theoretically explainable. [1] The long‐term morphodynamic evolution of estuaries depends on a combination of antecedent topography and boundary conditions, including fluvial input, sea‐level change and regional‐landscape interactions. [2]该模型随后被应用于评估河口的长期形态动力学演变，以响应各种强迫的变化，其结果在概念上和理论上都可以解释。 [1] 河口的长期形态动力学演化取决于前期地形和边界条件的组合，包括河流输入、海平面变化和区域-景观相互作用。 [2]
Consistent Morphodynamic Evolution 一致的形态动力学演化
The almost linear relationship between the cross-sectional inlet areas and the tidal prisms of the intertidal basins in the East Frisian Wadden Sea demonstrates that these bathymetric data describe a consistent morphodynamic evolutionary trend. [1] The almost linear relationship between the cross-sectional inlet areas and the tidal prisms of the intertidal basins in the East Frisian Wadden Sea demonstrates that these bathymetric data describe a consistent morphodynamic evolutionary trend. [2]东弗里斯兰瓦登海潮间带盆地的横截面入口面积与潮汐棱柱之间的几乎线性关系表明，这些测深数据描述了一致的形态动力学演化趋势。 [1] 东弗里斯兰瓦登海潮间带盆地的横截面入口面积与潮汐棱柱之间的几乎线性关系表明，这些测深数据描述了一致的形态动力学演化趋势。 [2]