The Indonesian Throughflow circulation under solar geoengineering [PDF]
The Indonesia Throughflow (ITF) is the only low-latitude channel between the Pacific and Indian oceans, and its variability has important effects on global climate and biogeochemical cycles.
C. Shen +4 more
doaj +3 more sources
Change in Salinity of Indonesian Upper Water in the Southeastern Indian Ocean during Argo Period [PDF]
The change in salinity of Indonesian Upper Water (IUW) in the Indian Ocean has been examined during 2004–2020 based on the Argo product. Monthly salinity fields reveal a contrast of IUW salinity changes between two time periods (2004–2013 and 2014–2020 ...
Mochamad Riza Iskandar, Toshio Suga
doaj +2 more sources
The intrinsic 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
Ryo Furue +2 more
doaj +2 more sources
Impact of the Indonesian Throughflow on Agulhas leakage [PDF]
Using ocean models of different complexity we show that opening the Indonesian Passage between the Pacific and the Indian oceans increases the input of Indian Ocean water into the South Atlantic via the Agulhas leakage. In a strongly eddying global ocean
D. Le Bars +2 more
doaj +6 more sources
The Indonesian Throughflow and its Impact on Biogeochemistry in the Indonesian Seas
It has been widely known that the Indonesian Throughflow (ITF) is an important inter-ocean connection with unique and complex oceanographic and geographic conditions, as well as a strong relation to both regional and global ocean currents and climate ...
Edwards Taufiqurrahman +2 more
doaj +3 more sources
South China Sea throughflow impact on the Indonesian throughflow [PDF]
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
Arnold L Gordon +2 more
exaly +2 more sources
Pacific‐to‐Indian Ocean connectivity: Tasman leakage, Indonesian Throughflow, and the role of ENSO [PDF]
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.
Erik van Sebille +2 more
exaly +3 more sources
Opposite Variability of Indonesian Throughflow and South China Sea Throughflow in the Sulawesi Sea [PDF]
Based on a high-resolution (0.1° × 0.1°) regional ocean model covering the entire northern Pacific, this study investigated the seasonal and interannual variability of the Indonesian Throughflow (ITF) and the South China Sea Throughflow (SCSTF) as well ...
Gordon, A. L. +4 more
core +3 more sources
Detecting Change in the Indonesian Seas [PDF]
The Indonesian seas play a fundamental role in the coupled ocean and climate system with the Indonesian Throughflow (ITF) providing the only tropical pathway connecting the global oceans.
Janet Sprintall +35 more
doaj +4 more sources
Freshwater Contributions to Decadal Variability of the Indonesian Throughflow
The Makassar Strait, the main passageway of the Indonesian Throughflow (ITF), is an important component of Indo‐Pacific climate through its inter‐basin redistribution of heat and freshwater.
Shouyi Wang +6 more
doaj +2 more sources

