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Journal of ZheJiang University (Engineering Science)  2019, Vol. 53 Issue (2): 315-324    DOI: 10.3785/j.issn.1008-973X.2019.02.015
Water Resources and Ocean Engineering     
Numerical simulation of three-dimensional characteristics of tidal current and residual current in Yangshan Harbor
Yan-ling TANG1(),Lu-di XU1,Zhi-guo HE1,2,*(),Bao-de CHEN3,Jie XU4,Li LI1,2
1. Ocean College, Zhejiang University, Zhoushan 316012, China
2. Key Laboratory of Marine Geotechnical Engineering and Materials of Zhejiang Province, Hangzhou 310058, China
3. Shanghai Typhoon Research Institute, China Meteorology Administration, Shanghai 200030, China
4. Shanghai Marine Meteorological Observatory, Shanghai 200030, China
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Abstract  

The finite-volume community ocean model (FVCOM) was used to establish a high-resolution numerical model based on the latest bathymetry data and unstructured mesh. The three-dimensional characteristics of the tidal current and residual current in Yangshan Harbor after the construction of the harbor were studied. Model results indicated that the speed of flood tide was faster than that of the ebb tide in the west of the narrow, and the performance of the east was opposite. The speed in the south of the islands was higher than that in the north. High velocity region and circulation phenomenon appeared at the narrow entrance of the tidal channel, and the peak speed reached 2.88 m/s at the surface level during flood tide. In the north and south areas of the islands, eddies were formed during the flood slack tide, with the northward current at surface and southward current at bottom. And the direction was opposite during ebb slack tide. A circulation existed with the southward current at surface and northward current at bottom during ebb tide at the deep-water channel. The directions of the M2 tidal ellipses were controlled by the coastlines under the influence of the project. The tidal choking effect increased after the construction of the harbor. The residual current was dominated by seaward in Yangshan Harbor sea area, but landward residual current existed in the channel. Separation of residual current appeared at the narrow entrance of the tidal channel. The stagnation point moved eastward.



Key wordsYangshan Harbor      tidal current      residual current      unstructured mesh      finite-volume community ocean model (FVCOM)     
Received: 20 September 2017      Published: 21 February 2019
CLC:  P 751  
Corresponding Authors: Zhi-guo HE     E-mail: yltang@zju.edu.cn;hezhiguo@zju.edu.cn
Cite this article:

Yan-ling TANG,Lu-di XU,Zhi-guo HE,Bao-de CHEN,Jie XU,Li LI. Numerical simulation of three-dimensional characteristics of tidal current and residual current in Yangshan Harbor. Journal of ZheJiang University (Engineering Science), 2019, 53(2): 315-324.

URL:

http://www.zjujournals.com/eng/10.3785/j.issn.1008-973X.2019.02.015     OR     http://www.zjujournals.com/eng/Y2019/V53/I2/315


洋山海域三维潮流和余流特征的数值模拟

基于最新的水下地形数据和非结构网格,利用有限体积海洋模型(FVCOM),建立洋山海域高分辨率水动力数值模型,研究该海域建港工程后潮流和余流的三维动力学特征. 结果表明,峡道西部涨潮流大于落潮流,东部相反. 南岛链以南海域流速均大于北岛链以北流速,峡道窄口处出现高流速区和环流现象,涨潮流表层最大流速可达2.88 m/s. 涨憩时刻,南岛链南岸和北岛链北岸都形成表层向北、底层向南的表-底层环流,落憩时刻相反. 落急时,深水航道处出现表层向南、底层向北的表-底层环流. 受围海造地工程后地形影响,峡道内M2分潮潮流椭圆主轴均沿岸线方向. 与工程前相比,峡道效应增强. 洋山海域整体以海向余流占优,但峡道内形成陆向余流. 峡道窄口处存在余流分离现象,峡道西部余流滞流点东移.


关键词: 洋山港,  潮流,  余流,  非结构网格,  有限体积海洋模型 
Fig.1 Sketch of location of computational domain, model mesh and terrain
Fig.2 Verification of tidal elevation in Yangshan Harbor and Majishan, and verification of flow velocity and flow direction in Haijiaofubiao and Kouwaifubiao
Fig.3 Surface flow field in each period during spring tide in Yangshan Harbor with red circle representing circulation position in each period
Fig.4 Vertical velocity profile in P1 to P4 cross sections in flood and ebb periods during spring tide
Fig.5 Vertical velocity profile parallel to P5 cross section in flood and ebb periods during spring tide with black line representing contour of 0 flow rate
Fig.6 Vertical velocity profiles parallel or perpendicular to P5 cross section respectively in flood and ebb periods during spring tide with black line representing contour of 0 flow rate
Fig.7 Distribution of tidal current ellipses in Yangshan Harbor with red lines representing surface layer, blue lines representing middle layer, and green lines representing bottom layer
Fig.8 Vertical distribution of semimajor, semiminor, inclination and ellipticity of M2 tidal current ellipse
Fig.9 Distribution of Euler residual current with red rectangle, circle, and triangle representing stagnation point, separation point and circulation position respectively
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