#TITLE_ALTERNATIVE#
Abstract: <br /> <br /> <br /> <br /> <br /> Current simulation using 3D hydrodynamic baroclinic Princeton Ocean Model with a generating force of tides and river discharges are used to examine the distribution of temperature and salinity which are represented by th...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/5689 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Abstract: <br />
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Current simulation using 3D hydrodynamic baroclinic Princeton Ocean Model with a generating force of tides and river discharges are used to examine the distribution of temperature and salinity which are represented by three river mouths in Jakarta Bay. The data used in this model are tidal data which is applied in the open boundary using ORI Tide program, salinity and temperature data which is applied in the waters of Jakarta Bay as initial condition, and salinity, temperature and river discharges data in three river mouths namely Muara Angke, Muara Karang and Muara Ancol. Simulation was done for 21 days. <br />
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The result of the model simulation shows that during ebb tide the water turns clockwise along the center of Jakarta bay, and counter clockwise during flood tide. The difference in spring tide and neap tide is not in the current pattern but in the magnitude, it is greater in spring tide. Temperature pattern is similar to the one of salinity which spreads out towards the sea during ebb tide and pushed toward the river during flood tide. Vertical variation of temperature is only up to 3 m depth. <br />
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