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    High-frequency seafloor acoustic backscatter from coastal marine habitats of Australia.

    191023_73001_parnum_high_frequency_seafloor_acoustic_2012.pdf (790.3Kb)
    Access Status
    Open access
    Authors
    Parnum, Iain
    Gavrilov, Alexander
    Date
    2012
    Type
    Conference Paper
    
    Metadata
    Show full item record
    Citation
    Parnum, Iain and Gavrilov, Alexander. 2012. High-frequency seafloor acoustic backscatter from coastal marine habitats of Australia, in McMinn, Terrance (ed), Acoustics 2012 Fremantle: Acoustics, Development and the Environment, The 2012 Conference of the Australian Acoustical Society, Nov 21-23 2012. Fremantle, Western Australia: Australian Acoustical Society
    Source Title
    Proceedings fo the Australian Society of Australia
    Source Conference
    Acoustics 2012 Fremantle: Acoustics, Development and the Environment, the 2012 Conference of the Australian Acoustical Society
    Additional URLs
    http://www.acoustics.asn.au/conference_proceedings/AAS2012/papers/p93.pdf
    ISBN
    9780646590394
    URI
    http://hdl.handle.net/20.500.11937/45546
    Collection
    • Curtin Research Publications
    Abstract

    Backscatter strength versus incidence angle has been measured from a variety of seafloor types from Australian coastal waters using a Reson Seabat 8125 multibeam echo-sounder (MBES) operating at 455 kHz. MBES surveys were carried out at six sites around Australia (between 2004 and 2006). Seafloor habitats surveyed in this study included: seagrass meadows, rhodolith beds, coral reef, rock, gravel, sand, muddy sand, and mixtures of those habitats. The highest backscatter strength was observed not only for the hard and rough substrate, but also for marine flora, such as rhodolith and seagrass. The main difference in acoustic backscatter from the different habitats was the mean level, or angle-average backscatter strength. However, additional information was also obtained from the rate of change (or slope) of backscatter strength with incidence angle. Overall, analysis of MBES backscatter data found at least six different seafloor habitats could be identified, in descending order of their average backscatter strength: 1) Rhodolith, 2) Coral, 3) Rock, 4) Seagrass, 5) sand-dominated bare (i.e. no epibenthic cover) sediment, 6) mud-dominated bare (i.e. no epibenthic cover) sediment.

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