The impacts of the large-scale hydraulic structures on tidal dynamics in open-type bay: numerical study in Jakarta Bay

被引:10
作者
Rusdiansyah, Alfi [1 ,2 ]
Tang, Yanling [1 ]
He, Zhiguo [1 ,3 ]
Li, Li [1 ,3 ]
Ye, Ying [4 ]
Surya, Martin Yahya [1 ]
机构
[1] Zhejiang Univ, Inst Port Coastal & Offshore Engn, Ocean Coll, Hangzhou 310058, Zhejiang, Peoples R China
[2] Agcy Assessment & Applicat Technol BPPT, Jakarta 13410, Indonesia
[3] State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Zhejiang, Peoples R China
[4] Zhejiang Univ, Inst Marine Geol & Resources, Ocean Coll, Hangzhou 310058, Zhejiang, Peoples R China
关键词
Jakarta Bay; Tide; Current; Residual current; Giant Sea Wall; Numerical modeling; MOKPO COASTAL ZONE; MODEL; CONSTRUCTION; RECLAMATION; KOREA; OCEAN;
D O I
10.1007/s10236-018-1183-3
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The construction of a Giant Sea Wall (GSW) complex in Jakarta Bay has been proposed to protect Jakarta against flood in the Master Plan for National Capital Integrated Coastal Development (NCICD). However, these large-scale hydraulic structures could significantly change the tidal dynamics in Jakarta Bay. This research investigates the potential impacts of a GSW on the tidal dynamics, including tides, currents, and residual currents in Jakarta Bay using a validated numerical model (Finite Volume Coastal Ocean Model (FVCOM)). Results show that the bay is diurnal with a maximum tidal range of similar to 0.9 m. The flow is mainly in an east-west direction with a maximum depth-mean current speed of up to 0.3 ms(-1). The construction of a GSW would modulate the tidal dynamics by changing the bathymetry, tidal prism, wind effect, and tidal choking effect in the bay. The maximum tidal range would be slightly increased due to the reduced tidal prism of the bay and the increased tidal choking effect. The current would penetrate into the west reservoir through the gates and channels between the artificial islands, with peak speed jets appearing at the gates (similar to 0.3 ms(-1)), due to tidal choking. A similar peak current speed appears near the right wing of the GSW due to the pressure gradient would be created by the wing of the GSW. Closing the gates would mainly affect the currents inside the west reservoir. The residual current would be slightly increased after the construction of the GSW. An eddy would be formed at the bottom level near the right wing of the GSW. The direction of the residual current is landward instead of seaward at the surface level outside the GSW. The impact of wind on surface currents would be much reduced due to the decreased water surface area. Although this study is site specific, the findings may have a wider applicability to the impacts of large-scale hydraulic structures on tidal dynamics in open-type bays.
引用
收藏
页码:1141 / 1154
页数:14
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