Dynamics of the Makassar Strait

Clicks: 17
ID: 308060
2001
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Abstract
Data collected as part of the Arlindo Project (“ Arlindo” is an acronym for Arus Lintas Indonesia, meaning “ throughe ow” in Bahasa Indonesia) from October 1996 to March 1998 are analyzed to study the characteristics of the e ow through the Makassar Strait. Analysis of inverted echo sounders (IES) and bottom pressure data (PIES) combined with TOPEX/POSEIDON satellite-derived sea height anomaly suggest that a minimum of three-layer approximation is necessary to explain the dynamics of the e ow in the Makassar Strait. The simple two-layer model used in several studies of the throughe ow is rejected based on total incompatibility with the data sets. A three-layer model with signie cant contributions by the middle layer provides a consistent interpretation of PIES and satellite data. Results are interpreted in the framework of the large-scale circulation.
Reference Key
openalex_W1988507115 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors M. Waworuntu, Silvia L. Garzoli, Donald B. Olson
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Journal journal of marine research
Year 2001
DOI
10.1357/002224001762882673
URL
https://doi.org/10.1357/002224001762882673
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