Results 131 to 140 of about 419 (169)
South China Sea throughflow impact on the Indonesian throughflow [PDF]
Geophysical Research Letters, 2012 In 2008–2009 the Makassar throughflow profile changed dramatically: the characteristic thermocline velocity maximum increased from 0.7 to 0.9 m/sec and shifted from 140 m to 70 m, amounting to a 47% increase in the transport of warmer water between 50 and 150 m during the boreal summer. HYCOM output indicates that ENSO induced change of the South China
Bruce Huber +2 more
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Multi-decadal timeseries of the Indonesian throughflow
Dynamics of Atmospheres and Oceans, 2018Abstract NCEP reanalysis wind data from 1948 to 2016 and Makassar Strait transport from 2004 to 2011 are used to construct a multi-decadal timeseries of 0–300 m Makassar Throughflow using a back-propagation (BP) neural network. Based on the 2004–2015 Makassar timeseries, 0–300 m transport accounts for 75% (±8%) of the total Makassar throughflow ...
Laura Gruenburg +2 more
exaly +2 more sources
Geostrophic transport of Indonesian throughflow
Deep Sea Research Part I: Oceanographic Research Papers, 1995Abstract The Indonesian throughflow was measured during a six year period, permitting estimates of the mean and mean annual cycle of volume transport. The measurements are based on regularly repeated XBT sections, which were used with the climatological T/S relationship to calculate geostrophic currents relative to 400 m.
G. Meyers, R.J. Bailey, A.P. Worby
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Fifty Years of the Indonesian Throughflow*
Journal of Climate, 2009Abstract Simple Ocean Data Assimilation (SODA) reanalysis data are used to produce a 50-yr record of flow through the Makassar Strait, the primary conduit for the Indonesian Throughflow (ITF). Two time series are constructed for comparison to the flow through the Makassar Strait as observed during 1997–98 and 2004–06: SODA along-channel ...
Arnold L. Gordon, Debra Tillinger
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Dynamics of Atmospheres and Oceans, 2009
Impacts of the South China Sea Throughflow (SCST) on seasonal and interannual variations of the Indonesian Throughflow are studied by comparing outputs from ocean general circulation model (OGCM) experiments with and without the SCST. The observed subsurface maximum in the southward flow through the Makassar Strait is simulated only when the SCST ...
Tomoki Tozuka +2 more
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Impacts of the South China Sea Throughflow (SCST) on seasonal and interannual variations of the Indonesian Throughflow are studied by comparing outputs from ocean general circulation model (OGCM) experiments with and without the SCST. The observed subsurface maximum in the southward flow through the Makassar Strait is simulated only when the SCST ...
Tomoki Tozuka +2 more
exaly +2 more sources
A diagnostic study of the Indonesian Throughflow
Journal of Geophysical Research: Oceans, 2000The objective of this study is to derive estimates of the mean seasonal variations in the Pacific to Indian Ocean throughflow transport using climatological data of the temperature/salinity fields and surface wind stress. A variable grid global general circulation model (GCM) with 1/6° resolution in Indonesian seas configured with ETOP05 bottom ...
Konstantin V. Lebedev +1 more
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Neogene history of the Indonesian Throughflow
2004The Indonesian Throughflow acts as a major switchboard in the global thermohaline circulation, and its variability is strongly related to tropical climate dynamics on shorter and longer timescales. During the Holocene and Pleistocene, fluctuating sea surface temperature and salinity patterns in the Western Pacific Warm Water Pool and Indonesian Seas ...
Wolfgang Kuhnt +4 more
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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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What controls the origin of the Indonesian throughflow?
Journal of Geophysical Research: Oceans, 1996The question of which water enters the Indonesian passages is a subject of outstanding debate. This article represents another attempt to address this issue using a new nonlinear model. The new model illustrates that the origin and composition of the Indonesian throughflow are determined by the structure of the opposing and retroflecting currents ...
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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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