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Validation of automated supervised segmentation of multibeam backscatter data from the Chatham Rise,New Zealand
Authors:Jess I T Hillman  Geoffroy Lamarche  Arne Pallentin  Ingo A Pecher  Andrew R Gorman  Jens Schneider von Deimling
Institution:1.Department of Geology,University of Otago,Dunedin,New Zealand;2.National Institute of Water and Atmospheric Research,Wellington,New Zealand;3.GNS Science,Lower Hutt,New Zealand;4.School of Environment,University of Auckland,Auckland,New Zealand;5.Christian-Albrechts-University of Kiel,Kiel,Germany
Abstract:Using automated supervised segmentation of multibeam backscatter data to delineate seafloor substrates is a relatively novel technique. Low-frequency multibeam echosounders (MBES), such as the 12-kHz EM120, present particular difficulties since the signal can penetrate several metres into the seafloor, depending on substrate type. We present a case study illustrating how a non-targeted dataset may be used to derive information from multibeam backscatter data regarding distribution of substrate types. The results allow us to assess limitations associated with low frequency MBES where sub-bottom layering is present, and test the accuracy of automated supervised segmentation performed using SonarScope® software. This is done through comparison of predicted and observed substrate from backscatter facies-derived classes and substrate data, reinforced using quantitative statistical analysis based on a confusion matrix. We use sediment samples, video transects and sub-bottom profiles acquired on the Chatham Rise, east of New Zealand. Inferences on the substrate types are made using the Generic Seafloor Acoustic Backscatter (GSAB) model, and the extents of the backscatter classes are delineated by automated supervised segmentation. Correlating substrate data to backscatter classes revealed that backscatter amplitude may correspond to lithologies up to 4 m below the seafloor. Our results emphasise several issues related to substrate characterisation using backscatter classification, primarily because the GSAB model does not only relate to grain size and roughness properties of substrate, but also accounts for other parameters that influence backscatter. Better understanding these limitations allows us to derive first-order interpretations of sediment properties from automated supervised segmentation.
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