EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC
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 (Ocea...
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id-itb.:334012019-01-22T15:16:56ZEKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC Anas, Muhammad Teknik (Rekayasa, enjinering dan kegiatan berkaitan) Indonesia Final Project Ekman pumping, SST, El Niño, La Niña, zonal wind. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/33401 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). 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. text |
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Teknik (Rekayasa, enjinering dan kegiatan berkaitan) Anas, Muhammad EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC |
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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).
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. |
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Final Project |
author |
Anas, Muhammad |
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Anas, Muhammad |
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Anas, Muhammad |
title |
EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC |
title_short |
EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC |
title_full |
EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC |
title_fullStr |
EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC |
title_full_unstemmed |
EKMAN PUMPING VARIABILITY IN THE EQUATORIAL PACIFIC |
title_sort |
ekman pumping variability in the equatorial pacific |
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https://digilib.itb.ac.id/gdl/view/33401 |
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