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Sediment Mobility due to currents and waves in the Torres Strait - Gulf of Papua region

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Created 13/01/2025

Updated 13/01/2025

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The MECO hydrodynamic model was adapted for the Torres Strait - Gulf of Papua region at 0.051 resolution. Validation of the hydrodynamic model was carried out against observed current meter data and calculated tidal sea levels. Dispersal pathways of sediments derived from the Fly River, and from a resuspension event along the northern Great Barrier Reef were investigated using an Eulerian approach. Sediment input into Torres Strait is found to be greater during the Trade season by approximately 10%. Wave data were also obtained, and together with hydrodynamic model output, sediment mobility due to currents, waves and wave-current interactions was considered for both the Trade and Monsoon seasons. Sediment mobility in the Gulf of Papua is dominated by wave motion, whereas Torres Strait is a mixed environment of waves and tidal currents.

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Title Sediment Mobility due to currents and waves in the Torres Strait - Gulf of Papua region
Language eng
Licence Not Specified
Landing Page https://devweb.dga.links.com.au/data/dataset/bbadac4e-0f67-45c5-8a50-3b323ce581d7
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
Data Portal Data.gov.au