Results 61 to 70 of about 389,376 (197)
ENSO and IOD influence on Indonesian Throughflow variability in the Makassar Strait and Banda Sea [PDF]
BIO Web of ConferencesThe Indonesian Throughflow (ITF) is a critical component of global ocean circulation, yet its response to simultaneous climate phenomena remains complex.
Srioktoviana Siti Khadijah +6 more
doaj +1 more source
Interplay between the Indonesian Throughflow and the Luzon Strait Throughflow [PDF]
, 2006 Author Posting. © Science in China Press and Springer, 2006. This is the author's version of the work. It is posted here by permission of Science in China Press and Springer for personal use, not for redistribution. The definitive version was published
Huang, Qizhou +4 more
core
Tracing the Abyssal Water Pathways in the Indian Ocean
Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.Abstract Antarctic‐origin abyssal waters occupy a significant fraction of the global ocean volume and play a key role in deep circulation and ventilation, yet their volume is declining rapidly in a warming climate. Although the Indian Ocean (IO) contains a substantial fraction of these waters, abyssal pathways and upwelling in the basin remain poorly ...
Kaushik Mishra +4 more
wiley +1 more source
Statistical Inversion of Sea Surface Temperature to Predict Submesoscale Near‐Surface Ocean Currents
Journal of Advances in Modeling Earth Systems, Volume 18, Issue 7, July 2026.Abstract Direct in situ measurements of sea surface currents (SSC) at submesoscales (1–100 km) are challenging. For this reason, inversion techniques have been utilized to infer SSC from satellite sea surface temperature (SST) data, which are straightforward to obtain. However, existing inversion methods often do not adequately account for uncertainty.
Rick de Kreij +4 more
wiley +1 more source
Indonesian throughflow in a coupled general circulation model [PDF]
Journal of Geophysical Research: Oceans, 1997 The Indonesian throughflow is analyzed in an extended simulation with a coupled ocean‐atmosphere model. The model, developed by the Max‐Planck‐Institut für Meteorologie, Hamburg, Germany, combines an atmospheric general circulation model at T42 resolution (2.8° latitude by 2.8° longitude) and a primitive equation ocean model with zonal resolution of 2 ...
Niklas Schneider, Tim P. Barnett
openaire +1 more source
, 2020 s of the 29th Annual Scientific Meeting of the Indonesian Heart Association (ASMIHA) 1st ASMIHA Digital Conference, 23-25 October ...
Indonesian Heart Association, ASMIHA
core +1 more source
Neogene Stable Carbon Isotopic Evolution of the Atmosphere and Low‐Latitude Surface Ocean
Paleoceanography and Paleoclimatology, Volume 41, Issue 7, July 2026.Abstract We reconstruct the stable carbon isotopic composition of Neogene surface ocean dissolved inorganic carbon (δ13CDIC) and atmospheric CO2 (δ13CATM) to serve as input for carbon cycle modeling and proxy‐related studies. The largely observation‐based δ13CDIC reconstructions are inferred from Neogene planktic foraminifer carbonate δ13C records with
J. A. van Dam +2 more
wiley +1 more source
, 2020 s of the 29th Annual Scientific Meeting of the Indonesian Heart Association (ASMIHA) 1st ASMIHA Digital Conference, 23-25 October ...
Indonesian Heart Association, ASMIHA
core +1 more source
Mesoscale and Submesoscale Variability in the Indian Ocean
Reviews of Geophysics, Volume 64, Issue 2, June 2026.Abstract Material transport and air‐sea coupling dynamics associated with monsoon‐related mesoscale and submesoscale processes in the Indian Ocean significantly modulate biogeochemical cycles, the large‐scale energy balance, and both regional and global climate change.
Lei Zhou +19 more
wiley +1 more source
Indonesian Throughflow in an eddy-resolving ocean model [PDF]
Chinese Science Bulletin, 2013 The performance of the eddy-resolving LICOM2.0 in simulating the Indonesian Throughflow has been evaluated against the INSTANT data in the present study. The mean vertical structures of the along strait velocities are simulated well in LICOM2.0, but the large velocities at the bottom of the Lifamatola Passage and the Timor Passage cannot be reproduced ...
Feng, Xue +4 more
openaire +1 more source