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<p align="justify">Variation of Ekman pumping in Equatorial Pacific has been studied using surface wind velocity from NCEP/NCAR (National Centers for Environmental Prediction/National Centers for Atmospheric Research). It’s also used temperature from NOAA (National Oceanic and Atm...

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Main Author: Anas (NIM : 12910023), Muhammad
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/29124
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:29124
spelling id-itb.:291242018-09-06T09:15:49Z#TITLE_ALTERNATIVE# Anas (NIM : 12910023), Muhammad Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/29124 <p align="justify">Variation of Ekman pumping in Equatorial Pacific has been studied using surface wind velocity from NCEP/NCAR (National Centers for Environmental Prediction/National Centers for Atmospheric Research). It’s also used temperature from NOAA (National Oceanic and Atmospheric Administration) and ONI (Ocean Nino Index) in the period of 1996 – 2015 (20 years). <br /> <br /> <br /> <br /> Data processing result show that Ekman pumping in the Equatorial Pacific (0.5°N – 0.5°S and 170°E – 110°W) varies by seasonal and interannual (El Niño and La Niña). The mean Ekman pumping has positive value between July to December with the intensity varies between 4.4x10-7 – 1.3x10-6 m s-1, corresponding with SST (Sea Surface Temperature) in the north and cause negative value in south. During El Niño and La Niña evidences, there is a time lag of one to three months between Ekman Pumping and SST anomalies. When trade wind becomes stronger, Ekman Pumping become stronger and there is a time lag of one to two months with zonal wind.<p align="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 <p align="justify">Variation of Ekman pumping in Equatorial Pacific has been studied using surface wind velocity from NCEP/NCAR (National Centers for Environmental Prediction/National Centers for Atmospheric Research). It’s also used temperature from NOAA (National Oceanic and Atmospheric Administration) and ONI (Ocean Nino Index) in the period of 1996 – 2015 (20 years). <br /> <br /> <br /> <br /> Data processing result show that Ekman pumping in the Equatorial Pacific (0.5°N – 0.5°S and 170°E – 110°W) varies by seasonal and interannual (El Niño and La Niña). The mean Ekman pumping has positive value between July to December with the intensity varies between 4.4x10-7 – 1.3x10-6 m s-1, corresponding with SST (Sea Surface Temperature) in the north and cause negative value in south. During El Niño and La Niña evidences, there is a time lag of one to three months between Ekman Pumping and SST anomalies. When trade wind becomes stronger, Ekman Pumping become stronger and there is a time lag of one to two months with zonal wind.<p align="justify">
format Final Project
author Anas (NIM : 12910023), Muhammad
spellingShingle Anas (NIM : 12910023), Muhammad
#TITLE_ALTERNATIVE#
author_facet Anas (NIM : 12910023), Muhammad
author_sort Anas (NIM : 12910023), Muhammad
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/29124
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