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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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Main Author: WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/12298
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:12298
spelling 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
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description 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.
format Final Project
author WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS
spellingShingle WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS
#TITLE_ALTERNATIVE#
author_facet WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS
author_sort WELLY RADIANTA GINTING (NIM 12904025), JUVENTUS
title #TITLE_ALTERNATIVE#
title_short #TITLE_ALTERNATIVE#
title_full #TITLE_ALTERNATIVE#
title_fullStr #TITLE_ALTERNATIVE#
title_full_unstemmed #TITLE_ALTERNATIVE#
title_sort #title_alternative#
url https://digilib.itb.ac.id/gdl/view/12298
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