Data

Rapid erosion of sand dunes in response to seasonal changes in hydrodynamics - A potential hazard for seagrass communities in the Torres Strait 2006

Australian Ocean Data Network
CSIRO O&A Data Centre (QLD), (Point of contact) CSIRO O&A, Information & Data Centre (Point of contact) CSIRO Oceans & Atmosphere - Dutton Park (Associated with) CSIRO Oceans & Atmosphere - Hobart (Associated with)
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=https://marlin.csiro.au/geonetwork/srv/eng/catalog.search#/metadata/e07ce4ab-be5f-7434-e043-08114f8cb1b9&rft.title=Rapid erosion of sand dunes in response to seasonal changes in hydrodynamics - A potential hazard for seagrass communities in the Torres Strait 2006&rft.identifier=Anzlic Identifier: ANZCW0306014244&rft.publisher=Australian Ocean Data Network&rft.description=Presentation Abstract: Submerged sand banks in the northwest of Torres Strait typically have smaller dunes superimposed upon them. Survey work undertaken as part of the Torres Strait CRC measured the rates of sand dune migration on these banks in an effort to gauge their potential impact on local seagrass communities. Marine surveys at the end of the monsoon and trade wind seasons measured very similar hydrodynamic conditions but substantially different patterns of dune migration. At the end of the monsoon season migration rates of up to 17 meters were measured over a 14 day period, at the end of the trade wind season migration rates of up to 4 meters were measured over a similar time period. Wind data acquired for the two weeks before and during the monsoon season survey indicated the onset of the trade wind season during this time. As a result, the elevated levels of dune migration observed at the end monsoon season are probably the result of wind driven-currents, changing from predominantly eastwards during the monsoon season to predominantly westwards with the onset of the trade wind season. Dunes that were influenced by wind-driven currents during the monsoon season were east facing at the start of the trade wind season but these dunes then became hydrodynamically unstable under the influence of the westward-directed wind-driven currents and experienced accelerated levels of migration to the west. By comparison, the lower rates of sand dune migration observed during the trade wind season survey are considered to be representative of dunes that are hydrodynamically stable. The main conclusions from this research are that the dunes in the study area have been observed to move rapidly in response to seasonal changes in hydrodynamics however the typical rates of dune migration suggest that only seagrass communities in close proximity to the sandbanks are likely to be threatened by dune migration.Progress Code: completedMaintenance and Update Frequency: notPlannedStatement: Metadata collated for the Torres Strait Inventory 2013 Project.&rft.creator=Anonymous&rft.date=2013&rft.coverage=westlimit=142; southlimit=-11; eastlimit=143; northlimit=-9&rft.coverage=westlimit=142; southlimit=-11; eastlimit=143; northlimit=-9&rft_rights=Release with the permission of the custodian&rft_subject=geoscientificInformation&rft_subject=Earth Science | Oceans | Coastal Processes | Sediment Transport&rft_subject=Earth Science | Oceans | Marine Sediments | Sediment Transport&rft_subject=Earth Science | Oceans | Ocean Acoustics | Acoustic Reflectivity&rft_subject=Earth Science | Oceans | Tides | Tidal Currents&rft_subject=Underwater Surveys (acquisition and/or analysis)&rft_subject=Marine Features (Australia) | Torres Strait, QLD&rft_subject=Torres Strait Research Repository 2013&rft_subject=Ship: James Kirby (RV)&rft.type=dataset&rft.language=English Access the data

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Presentation Abstract: Submerged sand banks in the northwest of Torres Strait typically have smaller dunes superimposed upon them. Survey work undertaken as part of the Torres Strait CRC measured the rates of sand dune migration on these banks in an effort to gauge their potential impact on local seagrass communities. Marine surveys at the end of the monsoon and trade wind seasons measured very similar hydrodynamic conditions but substantially different patterns of dune migration. At the end of the monsoon season migration rates of up to 17 meters were measured over a 14 day period, at the end of the trade wind season migration rates of up to 4 meters were measured over a similar time period. Wind data acquired for the two weeks before and during the monsoon season survey indicated the onset of the trade wind season during this time. As a result, the elevated levels of dune migration observed at the end monsoon season are probably the result of wind driven-currents, changing from predominantly eastwards during the monsoon season to predominantly westwards with the onset of the trade wind season. Dunes that were influenced by wind-driven currents during the monsoon season were east facing at the start of the trade wind season but these dunes then became hydrodynamically unstable under the influence of the westward-directed wind-driven currents and experienced accelerated levels of migration to the west. By comparison, the lower rates of sand dune migration observed during the trade wind season survey are considered to be representative of dunes that are hydrodynamically stable. The main conclusions from this research are that the dunes in the study area have been observed to move rapidly in response to seasonal changes in hydrodynamics however the typical rates of dune migration suggest that only seagrass communities in close proximity to the sandbanks are likely to be threatened by dune migration.

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Progress Code: completed
Maintenance and Update Frequency: notPlanned
Statement: Metadata collated for the Torres Strait Inventory 2013 Project.

Notes

Credit
James Daniell

Data time period: 2006 to 2006

This dataset is part of a larger collection

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143,-9 143,-11 142,-11 142,-9 143,-9

142.5,-10

text: westlimit=142; southlimit=-11; eastlimit=143; northlimit=-9

Other Information
Daniell (2006) - AMSA2006 Oral Presentation Abstract (Data Link)

url : https://www.marine.csiro.au/data/trawler/download.cfm?file_id=2962

Identifiers
  • Local : Anzlic Identifier: ANZCW0306014244
  • Local : Marlin Record Number: 14244
  • global : e07ce4ab-be5f-7434-e043-08114f8cb1b9