摘要

Coastal areas are vulnerable to the impacts of tropical cyclones (TC), tsunamis and other water super-elevation events, but the frequency of these events is often poorly represented by conventional records. Coastal overwash deposits (including washover fans) can provide a longer-term archive of event frequency. Because of their low-gradient geomorphic form, washover fans require high accuracy (centimetre-resolution) topographic models to understand patterns of connectivity and dynamics that control archive formation. Using images collected by a remotely piloted aircraft system (RPAS, or drone') and Structure-from-Motion (SfM) photogrammetry techniques, we apply a novel point-cloud filtering technique based on KMeans classification of the R-G-B colour of each X-Y-Z point to remove vegetation and create a centimetre-resolution and accuracy bare-earth digital terrain model (DTM) of a washover fan in Exmouth Gulf (Western Australia). Using the RPAS-SfM orphophoto and DEM data, supported by ground-penetrating radar (GPR) and field stratigraphic analysis, we show how this approach can be applied to understand dynamics controlling low-gradient geomorphic landforms, using an example of a washover fan sedimentary archive in northwestern Australia created by extreme overwash events. Our approach reveals the likely role of backflooding and terrestrial runoff in creating backwater environment for sub-aqueous deposition and good sediment preservation and identifies key areas to target for detailed dating and stratigraphic analysis of a potentially decadal to sub-millennial resolution sediment archive of TC activity.

  • 出版日期2018-9-30