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Preface The expedition ARK XIX/3 with the German icebreaking RV ...

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Hydrosweep DS2 is installed onboard <strong>RV</strong> Polarstern. It operates at a frequency of<br />

15.5kHz. In addition to depth measurements, echo amplitudes are recorded by <strong>the</strong><br />

system. <strong>The</strong> amplitudes can be converted into multibeam sidescan and angular<br />

backscatter data. <strong>The</strong> main application of sidescan is to detect small scale features which<br />

cannot clearly be recognised in <strong>the</strong> bathymetry (e.g. shallow channels or iceberg plough<br />

marks). In contrast, angular backscatter shows <strong>the</strong> same resolution as <strong>the</strong> depth<br />

measurements but supplies additional information about physical properties of <strong>the</strong><br />

seafloor (surface- and volume roughness) (Fig. A4.2.2-1).<br />

Fig. A4.2-1: Angular backscatter curve for a) rough and b) smooth seafloor.<br />

<strong>The</strong>refore, <strong>the</strong> backscatter strength and its dependence on <strong>the</strong> incidence angle of <strong>the</strong><br />

acoustic pulse onto <strong>the</strong> seafloor is considered. Using a terrain model and taking into<br />

account <strong>the</strong> effect of <strong>the</strong> water column as well as internal signal processing of <strong>the</strong><br />

multibeam, <strong>the</strong> recorded amplitude values are transformed into angular backscatter<br />

strength. Maps showing <strong>the</strong> spatial extension of <strong>the</strong> backscatter data are used as a basis<br />

to segment <strong>the</strong> seafloor into regions of different backscatter characteristics. <strong>The</strong><br />

segments are based on different echo levels and changing slope of <strong>the</strong> angular<br />

backscatter fall (dB per degree incidence angle). <strong>The</strong> combination of <strong>the</strong>se maps <strong>with</strong><br />

surface samples helps to determine different sediment properties in <strong>the</strong> segments and <strong>the</strong><br />

spatial validity of surface samples can be extended from <strong>the</strong> sampling spot to <strong>the</strong><br />

segmented areas. <strong>The</strong>reafter, <strong>the</strong> sediment data can serve as input for seafloor<br />

classification.<br />

<strong>The</strong> aim of this study is to investigate <strong>the</strong> link between seafloor properties and angular<br />

backscatter in order to use Hydrosweep bathymetric measurements for remote sensing of<br />

<strong>the</strong> seafloor. Sparsely distributed seafloor samples and related seafloor properties will be<br />

utilised to enhance interpretation of <strong>the</strong> entire area where backscatter data is available.<br />

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