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In this study, tidal currents simulation at Larantuka Strait was carried out by using a 2D hydrodynamic model and the potential energy of those currents were also estimated. Hydrodynamic simulation results were validated with observation data. Validation results show that root mean square error (RMS...
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id-itb.:122982017-09-27T11:47:23Z#TITLE_ALTERNATIVE# WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/12298 In this study, tidal currents simulation at Larantuka Strait was carried out by using a 2D hydrodynamic model and the potential energy of those currents were also estimated. Hydrodynamic simulation results were validated with observation data. Validation results show that root mean square error (RMS) between simulated currents and observation is 0.61 m/s for v (component north and south) and 1.34 m/s for u (component west and east). Simulated sea surface elevation is also verified with observation and RMS error of this comparison is 0.151 m. Further, potential current energy was estimated from the simulation and the application of Fraenkel's formula. Estimation results show that high current potential energy is located in 123.010 E, -8.325 N. Current potential energy during spring ebb tide to spring flood, spring flood to spring ebb tide, spring ebb tide to spring flood, spring flood to spring ebb tide are11.103 KWh, 29.789 KWh, 16.610 KWh and 23.399 KWh respectively. text |
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In this study, tidal currents simulation at Larantuka Strait was carried out by using a 2D hydrodynamic model and the potential energy of those currents were also estimated. Hydrodynamic simulation results were validated with observation data. Validation results show that root mean square error (RMS) between simulated currents and observation is 0.61 m/s for v (component north and south) and 1.34 m/s for u (component west and east). Simulated sea surface elevation is also verified with observation and RMS error of this comparison is 0.151 m. Further, potential current energy was estimated from the simulation and the application of Fraenkel's formula. Estimation results show that high current potential energy is located in 123.010 E, -8.325 N. Current potential energy during spring ebb tide to spring flood, spring flood to spring ebb tide, spring ebb tide to spring flood, spring flood to spring ebb tide are11.103 KWh, 29.789 KWh, 16.610 KWh and 23.399 KWh respectively. |
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WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS |
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WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS #TITLE_ALTERNATIVE# |
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WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS |
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WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS |
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https://digilib.itb.ac.id/gdl/view/12298 |
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