Results 171 to 180 of about 389,376 (197)
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Current variability at the Pacific entrance of the Indonesian Throughflow
Journal of Geophysical Research: Oceans, 1999Current variability at the Pacific entrance of the Indonesian Throughflow is investigated using direct current and hydrographic measurements. Two moorings with three current meters (depths of 350, 550, and 1050 m) and one conductivity‐temperature‐depth profiler (260 m) were deployed at 4°1′N, 127°31′E and 3°11′N, 128°27′E between Talaud Islands and ...
Yuji Kashino +4 more
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Coral radiocarbon constraints on the source of the Indonesian throughflow
Journal of Geophysical Research: Oceans, 1997Radiocarbon variability in Porites spp. corals from Guam and the Makassar Strait (Indonesian Seaway) was used to identify the source waters contributing to the Indonesian throughflow. Time series with bimonthly resolution were constructed using accelerator mass spectrometry.
M. D. Moore, D. P. Schrag, M. Kashgarian
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Journal of Climate Change Society
Journal references provide an overview of the current between the Pacific and Indian Oceans, referred to as the Indonesian Throughflow (Arlindo), which is part of the global thermohaline circulation that impacts the dynamics of the atmosphere and oceans by changing the circulation and characteristics of the sea water masses of the two oceans ...
Andi Sulistiyono, Budi Iman Samiaji
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Journal references provide an overview of the current between the Pacific and Indian Oceans, referred to as the Indonesian Throughflow (Arlindo), which is part of the global thermohaline circulation that impacts the dynamics of the atmosphere and oceans by changing the circulation and characteristics of the sea water masses of the two oceans ...
Andi Sulistiyono, Budi Iman Samiaji
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The Role of Indonesian Throughflow in a Global Ocean GCM
Journal of Physical Oceanography, 1993Abstract The effect of the Indonesian Throughflow on the World Ocean circulation is examined by a series of experiments with a global ocean GCM. The principal objective is to gain an understanding of how ocean flows respond to the throughflow, and how these changes result in changes in the pattern of surface heat flux and sea surface temperature.
Anthony C. Hirst, J. S. Godfrey
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Intrinsic interannual variability of the Indonesian Throughflow
The Indonesian Throughflow (ITF) carries an annual average of about 15 Sv of water from the Pacific through the Indonesian Seas Into the Indian Ocean, and its year-to-year variation ranges from 1 to 4 Sv. A 10-member ensemble of 41-year integrations of a semi-global eddy-resolving oceanic general circulation model is examined to explore the intrinsic ...Ryo Furue +2 more
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Physical oceanography of the present day Indonesian Throughflow
Geological Society, London, Special Publications, 2011Abstract The Indonesian Throughflow (ITF) transfers c . 15 Sv (1 Sv=10 6 m 3 s −1 ) of relatively cool, fresh water from the tropical Pacific Ocean to the tropical Indian Ocean.
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A Simple Model of the Indonesian Throughflow and Its Composition
Journal of Physical Oceanography, 1993Abstract A simple analytical model of the closure of the wind-driven gyres in the tropical west Pacific is developed to illustrate the role of Halmahera and variations in the Pacific wind stress on the water mass composition of the flow from the Pacific to the Indian Ocean through the Indonesian archipelago—that is, the Indonesian Throughflow.
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Effects of High-Frequency Flow Variability on the Pathways of the Indonesian Throughflow
Journal of Geophysical Research: Oceans, 2023Yanli Jia, Shinichiro Kida, Ryo Furue
exaly