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南渡江三角洲海岸泥沙纵向运移与岸滩演变的响应
引用本文:陈沈良,龚文平.南渡江三角洲海岸泥沙纵向运移与岸滩演变的响应[J].海洋湖沼通报,1998(1):23-32.
作者姓名:陈沈良  龚文平
作者单位:[1]华东师范大学河大口海岸国家重点实验室 [2]海南省海洋局
基金项目:国家自然科学基金!49671007
摘    要:南渡三角洲沿岸在盛行NNE向波浪等动力条件的作用下,泥沙产生纵向运移,岸滩遭受侵蚀或堆积,岸滩演变剧烈。本文利用基于网格的波注折射绕射模型,分析南渡江三角洲海岸波浪动力过程、破波带波能与辐射应力分布及其引起的沿岸泥沙纵向运称。浴海岸动力学地貌的角度,通过三角洲沿岸波浪动力特征、泥沙运动的分析,探讨沙质岸滩的动态与地貌演变。

关 键 词:南渡江  三角液  海岸  泥沙运移  岸滩演变

LONGSHORE SEDIMENT TRANSPORT AND NEARSHORE EVOLUTION RESPONSE FOR THE NANDUJIANG DELTA,HAINAN LSLAND
Chen Shenliang.LONGSHORE SEDIMENT TRANSPORT AND NEARSHORE EVOLUTION RESPONSE FOR THE NANDUJIANG DELTA,HAINAN LSLAND[J].Transaction of Oceanology and Limnology,1998(1):23-32.
Authors:Chen Shenliang
Abstract:The grid-based regional coastal process wave numerical model (RCPWAVE) is used for predicting wave attack and consequent sediment transport patterns along the coastline of the Nandujiang Delta. The beach and nearshore evolution is described from the view of coastal morphodynamics, based on the analysis of wave dynamics and longshore sediment transport. The result shows that the prevailing NNE wind wave and westward longshore transport are the main causes of beach and nearshore evolution along the Nandujiang Delta.
Keywords:Wave force  radiation stress  longshore sediment transport  nearshore evolution  dynamic landform  
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