2015
DOI: 10.1016/j.jher.2014.10.005
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Analyzing the physics of non-tidal barotropic sea level anomaly events using multi-scale numerical modelling in Singapore regional waters

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Cited by 13 publications
(9 citation statements)
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“…Notwithstanding its maritime history, Malacca Strait is also an area with rich resources including productive coastal ecosystems, mangrove forests, coral reefs, seagrass beds, and fisheries (Thia-Eng et al 2000). Located between the Andaman Sea and the South China Sea, Malacca Strait is hydrodynamically complex due to the confluence of tides from these two large water bodies with seasonal monsoons that have effect on the net flow transport through the strait (Rizal et al 2010;Van Maren and Gerritsen 2012;Kurniawan et al 2014Kurniawan et al , 2015Tay et al 2016). In this paper, the flow condition is defined by a combination of tidal and non-tidal.…”
Section: Introductionmentioning
confidence: 99%
“…Notwithstanding its maritime history, Malacca Strait is also an area with rich resources including productive coastal ecosystems, mangrove forests, coral reefs, seagrass beds, and fisheries (Thia-Eng et al 2000). Located between the Andaman Sea and the South China Sea, Malacca Strait is hydrodynamically complex due to the confluence of tides from these two large water bodies with seasonal monsoons that have effect on the net flow transport through the strait (Rizal et al 2010;Van Maren and Gerritsen 2012;Kurniawan et al 2014Kurniawan et al , 2015Tay et al 2016). In this paper, the flow condition is defined by a combination of tidal and non-tidal.…”
Section: Introductionmentioning
confidence: 99%
“…This is because the hydrodynamics in southern Malacca Strait is highly complex. (Kurniawan et al, 2011, 2015, Tay et al, 2016 have pointed out that this area is a major tidal mixing zone between Indian Ocean and South China Sea. (Tay et al, 2016) have also shown that the local non-tidal hydrodynamics are heavily influenced by both Indian Ocean and South China Sea and their degree of influence is seasonally varying.…”
Section: Resultsmentioning
confidence: 99%
“…Details of tidal calibration and representation of model is described by (Tay et al, 2013). 6-hourly 0.75 degree horizontal resolution surface wind and pressure fields obtained from ECMWF ERA-Interim database (www.ecmwf.int) are applied to the model to generate non-tidal barotropic flow in the model domain (Kurniawan et al, 2015;Tay et al, 2016).…”
Section: Physics-based Numerical Modelmentioning
confidence: 99%
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