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<palign="justify">The territorial waters of western Sumatra affected by phenomenon in the Indian Ocean, as Indian Ocean Dipole (IOD), upwelling, and monsoon winds. In this research, water mass identified based on the distribution of water mass in eastern Indian Ocean, especially in w...

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Main Author: Hamidi Hasibuan (NIM : 12911005), Fazlur
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/27245
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:27245
spelling id-itb.:272452018-09-06T09:32:26Z#TITLE_ALTERNATIVE# Hamidi Hasibuan (NIM : 12911005), Fazlur Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/27245 <palign="justify">The territorial waters of western Sumatra affected by phenomenon in the Indian Ocean, as Indian Ocean Dipole (IOD), upwelling, and monsoon winds. In this research, water mass identified based on the distribution of water mass in eastern Indian Ocean, especially in western Sumatra. Water mass analysis in this research using Optimum Multi Parameter (OMP) method with the source of water mass is Bengal Bay Water (BBW), South Indian Central Water (SICW), dan Indian Equatorial Water (IEW). Parameter used is temperature and salinity were obtained from Kaiyo and Mirai Cruise, and World Ocean Database (WOD).Based on the result of research note that BBW with percentage more than 90% generally identified at the surface to a depth of 160 m. SICW having a maximum percentage 60-80% at a depth of 80 – 280 m. While IEW with percentage more than 90% at the depth of 480 – 1130 m. IEW in northern Indian Ocean more deeper than southern, due to BBW in the north has a lighter density, so that IEW with heavier density is deeper in the northern Indian Ocean.<palign="justify"> 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 <palign="justify">The territorial waters of western Sumatra affected by phenomenon in the Indian Ocean, as Indian Ocean Dipole (IOD), upwelling, and monsoon winds. In this research, water mass identified based on the distribution of water mass in eastern Indian Ocean, especially in western Sumatra. Water mass analysis in this research using Optimum Multi Parameter (OMP) method with the source of water mass is Bengal Bay Water (BBW), South Indian Central Water (SICW), dan Indian Equatorial Water (IEW). Parameter used is temperature and salinity were obtained from Kaiyo and Mirai Cruise, and World Ocean Database (WOD).Based on the result of research note that BBW with percentage more than 90% generally identified at the surface to a depth of 160 m. SICW having a maximum percentage 60-80% at a depth of 80 – 280 m. While IEW with percentage more than 90% at the depth of 480 – 1130 m. IEW in northern Indian Ocean more deeper than southern, due to BBW in the north has a lighter density, so that IEW with heavier density is deeper in the northern Indian Ocean.<palign="justify">
format Final Project
author Hamidi Hasibuan (NIM : 12911005), Fazlur
spellingShingle Hamidi Hasibuan (NIM : 12911005), Fazlur
#TITLE_ALTERNATIVE#
author_facet Hamidi Hasibuan (NIM : 12911005), Fazlur
author_sort Hamidi Hasibuan (NIM : 12911005), Fazlur
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/27245
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