Physical oceanography of the present day Indonesian Throughflow
Abstract: The Indonesian Throughflow (ITF) transfers c. 15 Sv (1 Sv 106 m3s21) of relatively cool, fresh water from the tropical Pacific Ocean to the tropical Indian Ocean. Additionally, the ITF is a key interocean component of the global ocean warm water route, which returns water from the Pacific...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1027.6747 2023-05-15T17:33:22+02:00 Physical oceanography of the present day Indonesian Throughflow Debra Tillinger The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6747 http://sp.lyellcollection.org/content/355/1/267.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6747 http://sp.lyellcollection.org/content/355/1/267.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://sp.lyellcollection.org/content/355/1/267.full.pdf text ftciteseerx 2016-10-30T00:05:02Z Abstract: The Indonesian Throughflow (ITF) transfers c. 15 Sv (1 Sv 106 m3s21) of relatively cool, fresh water from the tropical Pacific Ocean to the tropical Indian Ocean. Additionally, the ITF is a key interocean component of the global ocean warm water route, which returns water from the Pacific Ocean to the Atlantic Ocean to close the loop of the thermohaline overturning circulation associated with North Atlantic DeepWater. That flow consequently freshens the Indian Ocean and transports heat between basins. The ITF can also be described by the island rule, which relates the winds over the entire South Pacific Ocean to the magnitude of the ITF. El Niño-Southern Oscil-lation (ENSO) dominates the regional variability in the Pacific Ocean and exerts a strong control over the variability of ITF transport. The Indian Ocean responds to the ENSO signal as well, but is also influenced by the Indian Ocean Dipole, a climate phenomenon that may act inde-pendently of ENSO to affect the ITF. On a local scale, the surface layer of the ITF is controlled by local winds, which are primarily mon-soonal, but at depth the ITF responds to the pressure gradient between the Pacific Ocean and the Indian Text North Atlantic Unknown Indian Pacific |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
Abstract: The Indonesian Throughflow (ITF) transfers c. 15 Sv (1 Sv 106 m3s21) of relatively cool, fresh water from the tropical Pacific Ocean to the tropical Indian Ocean. Additionally, the ITF is a key interocean component of the global ocean warm water route, which returns water from the Pacific Ocean to the Atlantic Ocean to close the loop of the thermohaline overturning circulation associated with North Atlantic DeepWater. That flow consequently freshens the Indian Ocean and transports heat between basins. The ITF can also be described by the island rule, which relates the winds over the entire South Pacific Ocean to the magnitude of the ITF. El Niño-Southern Oscil-lation (ENSO) dominates the regional variability in the Pacific Ocean and exerts a strong control over the variability of ITF transport. The Indian Ocean responds to the ENSO signal as well, but is also influenced by the Indian Ocean Dipole, a climate phenomenon that may act inde-pendently of ENSO to affect the ITF. On a local scale, the surface layer of the ITF is controlled by local winds, which are primarily mon-soonal, but at depth the ITF responds to the pressure gradient between the Pacific Ocean and the Indian |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Debra Tillinger |
spellingShingle |
Debra Tillinger Physical oceanography of the present day Indonesian Throughflow |
author_facet |
Debra Tillinger |
author_sort |
Debra Tillinger |
title |
Physical oceanography of the present day Indonesian Throughflow |
title_short |
Physical oceanography of the present day Indonesian Throughflow |
title_full |
Physical oceanography of the present day Indonesian Throughflow |
title_fullStr |
Physical oceanography of the present day Indonesian Throughflow |
title_full_unstemmed |
Physical oceanography of the present day Indonesian Throughflow |
title_sort |
physical oceanography of the present day indonesian throughflow |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6747 http://sp.lyellcollection.org/content/355/1/267.full.pdf |
geographic |
Indian Pacific |
geographic_facet |
Indian Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://sp.lyellcollection.org/content/355/1/267.full.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1027.6747 http://sp.lyellcollection.org/content/355/1/267.full.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766131858391695360 |