SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE

This Study to know Subsurface Evolution of 2006 positive Indian Ocean Dipole. The data used are SST (Sea Surface Temperature), surface wind, SSH (Sea Surface Height), Zonal current, Zonal current for each dept and temperatur were obtained from Simple Ocean Data Assimilation (SODA), These data were a...

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Main Author: JOHAN (NIM: 22413011); Tim Pembimbing: Ivonne. M. Radjawane, Ph.D.; Dr. Iskhaq Iskandar M.Sc., SEPTI
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/20521
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:20521
spelling id-itb.:205212016-09-06T15:43:21ZSUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE JOHAN (NIM: 22413011); Tim Pembimbing: Ivonne. M. Radjawane, Ph.D.; Dr. Iskhaq Iskandar M.Sc., SEPTI Indonesia Theses INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/20521 This Study to know Subsurface Evolution of 2006 positive Indian Ocean Dipole. The data used are SST (Sea Surface Temperature), surface wind, SSH (Sea Surface Height), Zonal current, Zonal current for each dept and temperatur were obtained from Simple Ocean Data Assimilation (SODA), These data were analyzed using a lowpass filter with a cut-off period of 13-monthly to see the phenomenon of IOD and the cut-off period for the 3-month to see the phenomenon of the equatorial waves. The results showed that the evolution of positive IOD 2006 in subsurface occurred longer than the evolution of the surface. Evolution of positive IOD 2006 in subsurface preceding one month earlier and two months longer to ends than the evolution of IOD on the surface. The duration of the evolution of positive IOD 2006 in subsurface is affected by the zonal currents moving eastward during evolution took place. 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 This Study to know Subsurface Evolution of 2006 positive Indian Ocean Dipole. The data used are SST (Sea Surface Temperature), surface wind, SSH (Sea Surface Height), Zonal current, Zonal current for each dept and temperatur were obtained from Simple Ocean Data Assimilation (SODA), These data were analyzed using a lowpass filter with a cut-off period of 13-monthly to see the phenomenon of IOD and the cut-off period for the 3-month to see the phenomenon of the equatorial waves. The results showed that the evolution of positive IOD 2006 in subsurface occurred longer than the evolution of the surface. Evolution of positive IOD 2006 in subsurface preceding one month earlier and two months longer to ends than the evolution of IOD on the surface. The duration of the evolution of positive IOD 2006 in subsurface is affected by the zonal currents moving eastward during evolution took place.
format Theses
author JOHAN (NIM: 22413011); Tim Pembimbing: Ivonne. M. Radjawane, Ph.D.; Dr. Iskhaq Iskandar M.Sc., SEPTI
spellingShingle JOHAN (NIM: 22413011); Tim Pembimbing: Ivonne. M. Radjawane, Ph.D.; Dr. Iskhaq Iskandar M.Sc., SEPTI
SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE
author_facet JOHAN (NIM: 22413011); Tim Pembimbing: Ivonne. M. Radjawane, Ph.D.; Dr. Iskhaq Iskandar M.Sc., SEPTI
author_sort JOHAN (NIM: 22413011); Tim Pembimbing: Ivonne. M. Radjawane, Ph.D.; Dr. Iskhaq Iskandar M.Sc., SEPTI
title SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE
title_short SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE
title_full SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE
title_fullStr SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE
title_full_unstemmed SUBSURFACE EVOLUTION OF 2006 POSITIVE INDIAN OCEAN DIPOLE
title_sort subsurface evolution of 2006 positive indian ocean dipole
url https://digilib.itb.ac.id/gdl/view/20521
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