The DOI matches its Crossref record.
Variation of Indonesian throughflow and the El Niño‐Southern Oscillation
Abstract
The expendable bathythermograph (XBT) line Fremantle‐Sunda Strait transects the eastern Indian Ocean between northwestern Australia and Java. It was established in 1983 with low‐density sampling and upgraded to a frequently repeated line (>18 times per year) in 1987 to monitor currents. The observations during 1983 to 1994 are described and related to the field of wind stress. Variation of thermal structure shows a rich mixture of annual, semiannual, and interannual timescales. Empirical orthogonal function (EOF) analysis of anomalies of sea surface temperature (SST), dynamic height, and depth of the 20°C isotherm D20 identifies two distinctive signals. The El Niño ‐ Southern Oscillation (ENSO) signal (EOF 1) appears throughout the region and is strongest off the coast of Australia. A modulation of the annual signal (EOF 2) appears off the coast of Java. EOF 2 has a shorter timescale than the ENSO signal, and its temporal coefficients are correlated to zonal winds over the equatorial Indian Ocean. For both EOFs, anomalously low SST and dynamic height occur at the same time as anomalously shallow D20 and vice versa for opposite anomalies. The XBT data are used with a climatological temperature‐salinity relationship to calculate net, relative (0/400 dbar) geostrophic transports T through the section. For long timescales, T is representative of Indonesian throughflow. The variations associated with ENSO show a maximum during the La Niña of 1988–1989 and minima during the El Niños of 1986–1987 and 1991–1994. The peak‐to‐trough amplitude of the ENSO signal is 5 Sv. The ENSO signal in throughflow is discussed in terms of earlier studies. For the shorter timescales, T is representative of currents from the Indian Ocean flowing in and out of the region between northwestern Australia and Indonesia, changing the volume of upper layer water stored there. Associated with EOF 2, a sharp peak in westward transport developed during May to October 1994.
Overview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cited by
A dipole mode in the tropical Indian Ocean
Saji, N. H., Goswami, B. N., Vinayachandran, P. N., & Yamagata, T. (1999) · Nature · doi:10.1038/43854 · Cited by 5,510
The monsoon circulation of the Indian Ocean
Schott, F. A., & McCreary, J. P. (2001) · Progress in Oceanography · doi:10.1016/s0079-6611(01)00083-0 · Cited by 1,798
Masumoto, Y. (2004) · Institutional Repositories DataBase (IRDB) · doi:10.32131/jes.1.35 · Cited by 527
A CGCM Study on the Interaction between IOD and ENSO
Behera, S. K., Luo, J. J., Masson, S., Rao, S. A., Sakuma, H., & Yamagata, T. (2006) · Journal of Climate · doi:10.1175/jcli3797.1 · Cited by 391
A Look at the Relationship between the ENSO and the Indian Ocean Dipole.
ASHOK, K., GUAN, Z., & YAMAGATA, T. (2003) · Journal of the Meteorological Society of Japan. Ser. II · doi:10.2151/jmsj.81.41 · Cited by 316
Metadata
- Authors
- Meyers, G.
- Venue
- Journal of Geophysical Research: Oceans
- Publisher
- American Geophysical Union (AGU)
- Published
- 1996-05-15
- Volume
- 101
- Issue
- C5
- Pages
- 12255-12263
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W2022330015
- Cited by
- 484
- References
- 0
- FWCI
- 10.52
- Type
- journal article
- Language
- en
- Open access
- closed
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: Variation of Indonesian throughflow and the El Niño‐Southern Oscillation. https://app.cochat.ai/papers/10.1029/95jc03729
- The paper
- Meyers, G. (1996). Variation of Indonesian throughflow and the El Niño‐Southern Oscillation. Journal of Geophysical Research: Oceans. https://doi.org/10.1029/95jc03729
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.