| 南黄海辐射沙脊群西洋水道质点示踪数值模拟 |
| |
| 引用本文： | 徐凡,陶建峰,张长宽,康彦彦.南黄海辐射沙脊群西洋水道质点示踪数值模拟[J].水道港口,2013(2):93-98. |
| |
| 作者姓名： | 徐凡 陶建峰 张长宽 康彦彦 |
| |
| 作者单位： | 1. 河海大学水文水资源与水利工程科学国家重点实验室,南京210098
2. 河海大学港口海岸与近海工程学院,南京210098 |
| |
| 基金项目： | 国家自然科学基金(51179067,51109074);高等学校博士学科点专项科研基金(20090094120005) |
| |
| 摘 要： | 基于二维水动力数学模型和现有西洋垂线流速分布公式,运用Lagrange质点示踪法计算分析了南黄海辐射沙脊群北部西洋水域的质点运动轨迹,并与投放到该海域的GPS漂流浮标运动轨迹作比较,计算结果与实测浮标漂流轨迹吻合良好。模拟结果表明,西洋水域的涨潮表层流速最大可达3.5 m/s,落潮流速最大可达2.0 m/s,水质点运动主要沿着主槽方向,当质点运动到潮流沙脊区域,其运动会发生偏移,Lagrange余流方向指向南面。
|
| 关 键 词： | Lagrange法 质点示踪 辐射沙脊群 西洋水道 |
Numerical simulation of water particle motion in Xiyang tidal inlet on radial sand ridges of south Yellow Sea |
| |
| XU Fan,TAO Jian-feng,ZHANG Chang-kuan,KANG Yan-yan.Numerical simulation of water particle motion in Xiyang tidal inlet on radial sand ridges of south Yellow Sea[J].Journal of Waterway and Harbour,2013(2):93-98. |
| |
| Authors: | XU Fan TAO Jian-feng ZHANG Chang-kuan KANG Yan-yan |
| |
| Institution: | 1.State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai University,Nanjing 210098,China;2.College of Harbor,Coastal and Offshore Engineering,Hohai University,Nanjing 210098,China) |
| |
| Abstract: | Based on the 2D flow model and velocity distribution equation applied in Xiyang,the particle trajectory of Xiyang,located in the region of radial sand ridges in the south Yellow Sea,was obtained by using the Lagrange particle tracer method,which was consistent with the trajectory of a GPS buoy thrown into this area.The results show that the maximal surface velocities are 3.5 m/s and 2.0 m/s at the flood and ebb tide respectively.The water particles move along the main channel primarily and shift in sand ridge zone,with the Lagrange residual current moving towards south. |
| |
| Keywords: | Lagrange methods particle tracer radial sand ridges Xiyang tidal inlet |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
