Results 11 to 20 of about 389,376 (197)

Freshwater Contributions to Decadal Variability of the Indonesian Throughflow

open access: yesGeophysical Research Letters, 2023
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   +3 more sources

The Indonesian Throughflow circulation under solar geoengineering [PDF]

open access: yesEarth System Dynamics, 2023
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

The intrinsic variability of the Indonesian Throughflow

open access: yesFrontiers in Marine Science, 2023
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

Change in Salinity of Indonesian Upper Water in the Southeastern Indian Ocean during Argo Period [PDF]

open access: yesHeliyon, 2022
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

Impact of the Indonesian Throughflow on Agulhas leakage [PDF]

open access: yesOcean Science, 2013
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

open access: yesASEAN Journal on Science and Technology for Development, 2020
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]

open access: yesGeophysical 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
exaly   +2 more sources

Interplay between the Indonesian Throughflow and the South China Sea Throughflow

open access: yesChinese Science Bulletin, 2006
Analysis both based on the wind stress and ocean assimilation dataset shows that the interannual variability of the Indonesian Throughflow and the South China Sea (Luzon Strait) Throughflow is out of phase. Wind anomaly forcing in the equatorial Pacific plays an important role in setting up this phase relation.
Qinyan Liu   +4 more
openaire   +2 more sources

The Indonesian throughflow, its variability and centennial change [PDF]

open access: yesGeoscience Letters, 2018
The Indonesian Throughflow (ITF) is an important component of the upper cell of the global overturning circulation that provides a low-latitude pathway for warm, fresh waters from the Pacific to enter the Indian Ocean.
Ming Feng   +3 more
doaj   +2 more sources

Post‐Hiatus Enhancement of ENSO Forecast Skill via Salinity‐Mediated Indo‐Pacific Inter‐Basin Coupling

open access: yesGeophysical Research Letters
The El Niño–Southern Oscillation (ENSO) predictability has notably declined since the 1998–2013 global warming hiatus, challenging conventional sea surface temperature (SST)‐based forecast models.
Jing Wang   +3 more
doaj   +2 more sources

Home - About - Disclaimer - Privacy