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Geostrophic transport of Indonesian throughflow

Deep Sea Research Part I: Oceanographic Research Papers, 1995
Abstract 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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Multi-decadal timeseries of the Indonesian throughflow

Dynamics of Atmospheres and Oceans, 2018
Abstract 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 K Gruenburg, Arnold L. Gordon, Guo-qing Jiang   +2 more
exaly   +2 more sources

Impacts of the South China Sea Throughflow on seasonal and interannual variations of the Indonesian Throughflow

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, Tangdong Qu, Toshio Yamagata   +2 more
exaly   +2 more sources

Interannual variability of the Indonesian Throughflow: The salinity effect

Journal of Geophysical Research: Oceans, 2016
AbstractThe Indonesian Throughflow (ITF) region possesses strong mixing and experiences significant freshwater input, but the role of salinity variability in the Indonesian Seas remains unclear. The goal of this study is to understand how salinity variability influences the ITF transport on interannual time scales. The ITF transport is calculated using
Shijian Hu, Janet Sprintall
exaly   +2 more sources

Pacific-to-Indian Ocean connectivity: Tasman leakage, Indonesian Throughflow, and the role of ENSO [PDF]

Journal of Geophysical Research: Oceans, 2014
The upper ocean circulation of the Pacific and Indian Oceans is connected through both the Indonesian Throughflow north of Australia and the Tasman leakage around its south.
Alexander Sen Gupta, Agus Santoso, Matthew H. England   +2 more
exaly   +3 more sources

A diagnostic study of the Indonesian Throughflow

Journal of Geophysical Research: Oceans, 2000
The 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, Maxim I. Yaremchuk   +1 more
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Fifty Years of the Indonesian Throughflow*

Journal of Climate, 2009
Abstract 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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Neogene history of the Indonesian Throughflow

2004
The 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, Ann Holbourn, Robert Hall, Maja Zuvela, Rolf Käse   +4 more
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What controls the origin of the Indonesian throughflow?

Journal of Geophysical Research: Oceans, 1996
The 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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