摘要
珠江口伶仃洋汇集了虎门、蕉门、洪奇沥、横门的来水来沙 ,这些水、沙进入伶仃洋后 ,在各种因素的综合作用下 ,不断地运移 ,造成今天的伶仃洋三滩两槽复杂的水下地形。
The Lingdingyang Bay receives the silt and water of Humen,Jiaomen,Hongqili and Henmen at Zhujiang Estuary. These water and silt move continually by the integrated action of various factors,which results in the modern varied underwater topography of 'Three Shoals and Two Troughs'.
出处
《台湾海峡》
CAS
CSCD
2000年第1期119-124,共6页
Journal of Oceanography In Taiwan Strait
关键词
珠江口
伶仃洋
滩槽发育
演变
影响因素
Zhujiang Estuary, Lingdingyang Bay, shoal and though development, factor analysis