Please use this identifier to cite or link to this item: https://doi.org/10.1088/1755-1315/55/1/012012
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dc.titleUnderstanding coastal processes to assist with coastal erosion management in Darwin Harbour, Northern Territory, Australia
dc.contributor.authorTonyes, S.G
dc.contributor.authorWasson, R.J
dc.contributor.authorMunksgaard, N.C
dc.contributor.authorEvans, K.G
dc.contributor.authorBrinkman, R
dc.contributor.authorWilliams, D.K
dc.date.accessioned2020-10-23T04:51:12Z
dc.date.available2020-10-23T04:51:12Z
dc.date.issued2017
dc.identifier.citationTonyes, S.G, Wasson, R.J, Munksgaard, N.C, Evans, K.G, Brinkman, R, Williams, D.K (2017). Understanding coastal processes to assist with coastal erosion management in Darwin Harbour, Northern Territory, Australia. IOP Conference Series: Earth and Environmental Science 55 (1) : 12012. ScholarBank@NUS Repository. https://doi.org/10.1088/1755-1315/55/1/012012
dc.identifier.issn17551307
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/179521
dc.description.abstractSand transport pathways in Darwin Harbour, Northern Territory, Australia, are being investigated to assist with coastal management. Coastal erosion, which threatens public and private infrastructure, is one of the major problems along the harbour beaches. A study of sediment transport is essential to identify the challenges encountered by the stakeholders in coastal management. Darwin Harbour, located in the tropical, cyclone prone area of Australia, was, until recently, considered a near pristine estuary. A semi-diurnal macro-tidal embayment, the tidal variation in the harbour reaches up to 8 m with a mean tidal range of 3.7 m. The beach morphology consists of sandy pocket beaches between coastal cliffs, sandbars, rocky shore platforms, tidal flats and mangrove fringes. A two-dimensional depth averaged finite-element hydrodynamic model (RMA-2), coupled with a sediment transport model (RMA-11) from Resource Modelling Associates, has been used to infer the sources and the depositional areas of sand in the harbour. Grain size distributions and geochemical analysis are also used to characterize the sand and its source(s). Initial results show that the beach sand is mostly of offshore origin with small sand input from the rivers. Potential supplementary sand sources are the eroded materials from the shore platforms and the rocky cliffs. Due to the rapid development in Darwin Harbour, this study is fundamental in understanding coastal processes to support decision making in coastal management, particularly in a macro-tidal, tropical estuary. @ Published under licence by IOP Publishing Ltd.
dc.rightsAttribution 4.0 International
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.sourceUnpaywall 20201031
dc.subjectAnalytical geochemistry
dc.subjectBeaches
dc.subjectCoastal engineering
dc.subjectCoastal zones
dc.subjectErosion
dc.subjectFinite element method
dc.subjectGrain size and shape
dc.subjectSand
dc.subjectSediment transport
dc.subjectSedimentation
dc.subjectStorms
dc.subjectTides
dc.subjectTropics
dc.subjectCoastal erosion
dc.subjectDarwin Harbour
dc.subjectGeochemical analysis
dc.subjectGrain size distribution
dc.subjectHydrodynamic model
dc.subjectNorthern territories
dc.subjectSand transport
dc.subjectSediment transport model
dc.subjectDecision making
dc.typeConference Paper
dc.contributor.departmentLEE KUAN YEW SCHOOL OF PUBLIC POLICY
dc.description.doi10.1088/1755-1315/55/1/012012
dc.description.sourcetitleIOP Conference Series: Earth and Environmental Science
dc.description.volume55
dc.description.issue1
dc.description.page12012
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