Numerical modeling of tide and tidal current in the kangjin bay, south sea, Korea

2007 ◽  
Vol 42 (3) ◽  
pp. 153-163 ◽  
Author(s):  
Young Jae Ro ◽  
Kwang Young Jung ◽  
Woong Sik Jun ◽  
Hyun Min Eom
Keyword(s):  
Numerical Modeling ◽  
Tidal Current ◽  
South Sea ◽  
Tide And Tidal Current

scholarly journals TIDE AND TIDAL CURRENT IN THE BALI STRAIT, INDONESIA

2015 ◽  
Vol 36 (2) ◽  
pp. 25-36 ◽  
Author(s):  
Dessy Berlianty ◽  
Tetsuo Yanagi
Keyword(s):  
Tidal Current ◽  
Ecological Model ◽  
Current Model ◽  
Spring Tide ◽  
Residual Flow ◽  
Tidal Front ◽  
Shelf Seas ◽  
Shallow Area ◽  
Tidal Constituents ◽  
Tide And Tidal Current

Tide and tidal current model of the Bali Strait in Indonesia is produced by using a Coupled Hydrodynamical-Ecological Model for Regional and Shelf Seas (COHERENS). With its resolutions in the horizontal (500meters) and the vertical (4layers), the model well reproduces the four major tidal constituents, namely M2, S2, K1, and O1 tides, and their currents. Furthermore the model is used to investigate the tide-induced residual flow and tidal front in the Bali Strait. As a results, the tide-induced residual flow in the Bali Strait during the spring tide on May 16th in 2010 can be attributed to the variation of the strength of two eddies. The first one is the clockwise circulation in the shallow area at the wide part of the strait, while the second one is the small clockwise circulation in the south of the narrow strait. On the other hand, as suggestion from Simpson and Hunter (1974), the tidal front is determined by the value of log(H/U3) (where is the water depth in meters and the amplitude oftidal current amplitude in ms-1). The front detected by the image of sea surface temperature distribution from the satellite corresponds with the contour log(H/U3) of 6.5.

Numerical Modeling of the Tidal Current Movement of the Baima Port, China

2014 ◽  
Vol 675-677 ◽  
pp. 806-810 ◽  
Author(s):  
Xin Li ◽  
Ming Xiao Xie
Keyword(s):  
Numerical Modeling ◽  
Water Depth ◽  
Hydrodynamic Model ◽  
Tidal Current ◽  
Software Package ◽  
Current Field ◽  
Sediment Transportation ◽  
Current Coupling ◽  
Current Movement ◽  
D Wave

The Sanduao Bay is the bay with many of islands where the coastline is very winding with complex hydrodynamics and sediment transportation. Using a 2-D wave-current coupling hydrodynamic model of the Mike21 software package, the hydrodynamics condition on the Pingang Operation Area of Baima Port in the Sanduao Bay is simulatated. The results show that the current field in the berth is smooth that is beneficial to maintenance of water depth and reduction of siltation in berth. And the velocity in reclamation and dredging area is reduced less than 0.05m/s. the reclamation near the coastline and dredging in the berth make the velocity varied and the varying range is between 0.3m/s and 0.4m/s.

SAR observation and numerical modeling of tidal current wakes at the East China Sea offshore wind farm

2014 ◽  
Vol 119 (8) ◽  
pp. 4958-4971 ◽  
Author(s):  
XiaoMing Li ◽  
Lequan Chi ◽  
Xueen Chen ◽  
YongZheng Ren ◽  
Susanne Lehner
Keyword(s):  
Numerical Modeling ◽  
East China Sea ◽  
Tidal Current ◽  
Wind Farm ◽  
Offshore Wind ◽  
East China ◽  
Offshore Wind Farm ◽  
The East China Sea ◽  
China Sea

Can gray seals maintain heading within areas of high tidal current? Preliminary results from numerical modeling and GPS observations

2013 ◽  
Vol 30 (1) ◽  
pp. 374-380 ◽  
Author(s):  
Damien Chevaillier ◽  
Mikhail Karpytchev ◽  
Bernie J. Mcconnell ◽  
Simon Moss ◽  
Cecile Vincent
Keyword(s):  
Numerical Modeling ◽  
Tidal Current ◽  
Preliminary Results ◽  
Gps Observations ◽  
Gray Seals

scholarly journals Decrease in Tide and Tidal Current in Ariake Bay

2004 ◽  
Vol 13 (4) ◽  
pp. 403-411 ◽  
Author(s):  
Takamichi Fujiwara ◽  
Yusaku Kyozuka ◽  
Takaharu Hamada
Keyword(s):  
Tidal Current ◽  
Ariake Bay ◽  
Tide And Tidal Current
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