Abstract

This paper describes a new methodology to map intertidal sediment using a commercially available unmanned aerial system (UAS). A fixed-wing UAS was flown with both thermal and multispectral cameras over three study sites comprising of sandy and muddy areas. Thermal signatures of sediment type were not observable in the recorded data and therefore only the multispectral results were used in the sediment classification. The multispectral camera consisted of a Red–Green–Blue (RGB) camera and four multispectral sensors covering the green, red, red edge and near-infrared bands. Statistically significant correlations (>99%) were noted between the multispectral reflectance and both moisture content and median grain size. The best correlation against median grain size was found with the near-infrared band. Three classification methodologies were tested to split the intertidal area into sand and mud: k-means clustering, artificial neural networks, and the random forest approach. Classification methodologies were tested with nine input subsets of the available data channels, including transforming the RGB colorspace to the Hue–Saturation–Value (HSV) colorspace. The classification approach that gave the best performance, based on the j-index, was when an artificial neural network was utilized with near-infrared reflectance and HSV color as input data. Classification performance ranged from good to excellent, with values of Youden’s j-index ranging from 0.6 to 0.97 depending on flight date and site.

Highlights

  • A key aspect of both coastal research and environmental impact assessment for coastal development is the mapping of intertidal sediment type

  • This paper describes the use of a commercially available unmanned aerial system (UAS) to conduct such mapping

  • An analysis of 10 years of weather data from a station at Mumbles close to the Neath Estuary site showed that conditions were only suitable for flying 40% of the time. This contribution explores the use of UASs to map intertidal sediment type

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Summary

Introduction

A key aspect of both coastal research and environmental impact assessment for coastal development is the mapping of intertidal sediment type. The focus of this work is on sands and muds. A key motivation for the work was the potential development of a tidal energy lagoon industry where altered intertidal coverage of sand and mud is perceived to be the primary environmental impact by both regulators and developers [1]. Gravels and cobbles are less important in this context: such sediment classes make up a much lower percentage of the intertidal in the areas of interest so are not considered a key receptor compared to sands and muds, which provide important benthic habitats. The contrast between cobbles and sand is greater and they are considered less difficult to identify in remotely sensed data; the authors have previously demonstrated such distinction using terrestrial laser scanners [2]

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