首页> 外文会议>International Conference on Estuaries and Coasts(ICEC-2003) I; 20031109-11; Hangzhou(CN) >FIELD STUDIES AND MODELLING OF INTERACTION BETWEEN NEARSHORE CURRENTS AND BARRED COAST
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FIELD STUDIES AND MODELLING OF INTERACTION BETWEEN NEARSHORE CURRENTS AND BARRED COAST

机译:近岸电流与禁止海岸相互作用的现场研究与建模。

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摘要

The study is aimed at on the description of longshore and cross-shore currents at a bar crest and at an adjacent trough. Field measurements and theoretical modelling tested against and driven by the field data were carried out. The field data were collected during several field campaigns comprising a multi-bar coastal zone. The recent field investigations revealed some specific features of nearshore hydrodynamics, e.g. significant longshore current velocities not only in the surf zone but beyond its offshore boundary as well. These velocities occurred even during almost perpendicular wave incidence. On a second front, the cross-shore currents were found to be much depth-variable, with the velocities sometimes directed seawards at the bar crest and landwards at the bar trough. The phase-resolving sediment transport computations incorporated a three-layer model with the bedload layer based on the water-soil mixture theory and two sub-layers of suspended load. This sediment transport model was nested in the phase-averaged modelling framework of hydrodynamics. Sea bed changes were calculated from spatial variability of the net sand transport rate. The records of nearshore topography were investigated with Extended Empirical Orthogonal Functions (EEOF) to seek large scale, long-term morphodynamic patterns.
机译:该研究的目的是描述条形波峰和相邻波谷处的长岸和跨岸海流。针对现场数据并由现场数据驱动进行了现场测量和理论建模。现场数据是在包括多条沿海地区在内的几次现场运动中收集的。最近的现场调查揭示了近岸水动力的一些特定特征,例如不仅在冲浪区而且在其海上边界以外的重要近岸流速。这些速度甚至发生在几乎垂直的波入射期间。在第二个方面,发现跨岸水流的深度变化很大,有时速度有时会指向海,直指在海浪的顶部,而海浪则直指在海槽的陆地。相分辨的泥沙运移计算将三层模型与基于水土混合理论的床层和两层子层的悬浮物结合起来。该泥沙运移模型嵌套在水动力学的相平均建模框架中。海床变化是根据净沙传输速率的空间变异性计算的。利用扩展经验正交函数(EEOF)对近岸地形记录进行了研究,以寻求大规模的长期形态动力学模式。

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