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。
Based on the detailed observations of morphodynamics and topography of the beach cusps, a study on the beach cusp morphological evolution under the normal wave conditions is carried out.
通过对滩角地形的详细观测，研究了滩角在常浪条件下的调整和变动过程。
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