海滩均衡剖面是海洋动力和海滩泥沙充分作用下的一个具有统计意义上的相对均衡的海滩形态。
The equilibrium beach profile is a statistically relative equilibrium beach shape under the interaction between Marine dynamics and beach sediments.
结果表明滩角的形成过程具有自组织特征，因此滩角可以通过海滩泥沙、地形与波、流的自组织过程形成。
The results show that the self-organized processes between the sediment, topography and swash can induce the formation of beach cusps.
结果表明，在常波况条件下海滩沿岸泥沙向偏南方向运移，在高能条件下可能出现与常波况条件下相反运动的趋势。
It is shown from the analysis results that the alongshore beach sediment was transported southward under normal wave conditions and could be transported northward under high wave energy conditions.
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