Please use this identifier to cite or link to this item: https://doi.org/10.1016/j.jher.2014.10.005
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dc.titleAnalyzing the physics of non-tidal barotropic sea level anomaly events using multi-scale numerical modelling in Singapore regional waters
dc.contributor.authorKurniawan, Alamsyah
dc.contributor.authorTay, Serene Hui Xin
dc.contributor.authorOoi, Seng Keat
dc.contributor.authorBabovic, Vladan
dc.contributor.authorGerritsen, Herman
dc.date.accessioned2020-04-08T04:15:48Z
dc.date.available2020-04-08T04:15:48Z
dc.date.issued2015-09-01
dc.identifier.citationKurniawan, Alamsyah, Tay, Serene Hui Xin, Ooi, Seng Keat, Babovic, Vladan, Gerritsen, Herman (2015-09-01). Analyzing the physics of non-tidal barotropic sea level anomaly events using multi-scale numerical modelling in Singapore regional waters 9 (3) : 404-419. ScholarBank@NUS Repository. https://doi.org/10.1016/j.jher.2014.10.005
dc.identifier.issn1570-6443
dc.identifier.issn1876-4444
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/166569
dc.description.abstract© 2015 International Association for Hydro-environment Engineering and Research, Asia Pacific Division. The hydrodynamic flows in the Singapore regional waters (SRW) are the result of a complex mix of tide, seasonal and meteorological effects. The study of non-tidal effects or sea level anomalies (SLA) in this region has shown that it is possible to model some of these anomalies. The present study addresses the non-tidal barotropic water levels and currents in the Singapore region in detail. This analysis includes a multi-scale approach, and addresses amongst others hydrodynamic model grid resolution and the importance of resolving non-linear tide-surge interaction. The results show that the water level and current anomalies phenomena in a complex region like SRW can be effectively modelled using an approach combining non-tidal barotropic and multi-scale numerical modelling. A detailed investigation of the levels of non-linear tide-surge interaction is carried out by simulating SLA events in the Singapore regional waters during North-East (positive SLA) and South-West (negative SLA) monsoons based on ECMWF numerical weather forcing conditions. The results of combining both approaches suggest that the finer grid resolution improves the accuracy of water level and current anomalies simulations. Furthermore, the results also indicate that for the simulations of non-tidal barotropic flows in this area, non-linear tide-surge interaction is important and should be taken into account. Finally, the behaviour of the non-tidal barotropic flow in the region and its changes with tidal variation in the shallow region of the Singapore Strait is now much better understood. Therefore, for reliable operational forecast of sea level, the inclusion of non-linear tide-surge interaction should be required in numerical models to reproduce both tides and surges with improved accuracy in this region.
dc.publisherELSEVIER
dc.sourceElements
dc.subjectScience & Technology
dc.subjectTechnology
dc.subjectLife Sciences & Biomedicine
dc.subjectPhysical Sciences
dc.subjectEngineering, Civil
dc.subjectEnvironmental Sciences
dc.subjectWater Resources
dc.subjectEngineering
dc.subjectEnvironmental Sciences & Ecology
dc.subjectSea level anomalies
dc.subjectSingapore regional waters
dc.subjectNon-tidal barotropic modelling
dc.subjectMulti-scale approach
dc.subjectTide surge interaction
dc.subjectSURGE
dc.subjectCIRCULATION
dc.typeConference Paper
dc.date.updated2020-04-08T03:43:02Z
dc.contributor.departmentCIVIL AND ENVIRONMENTAL ENGINEERING
dc.contributor.departmentTROPICAL MARINE SCIENCE INSTITUTE
dc.description.doi10.1016/j.jher.2014.10.005
dc.description.volume9
dc.description.issue3
dc.description.page404-419
dc.published.statePublished
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