Abstract

The growing interest in monitoring the marine environment has strongly encouraged governmental agencies and research institutes to undertake seabed mapping programs and stimulated scientific interest in innovative mapping methods and tools. In this study, object-based image analysis was used to map a very shallow tidal inlet, characterized by high sediment variability and intense morphodynamic processes. The aim was to test the feasibility of reproducible mapping approaches within extended mapping programs of complex coastal areas. The study is based on full-coverage, high-resolution bathymetry and reflectivity, calibrated by means of sediment samples. Seafloor segmentation and classification were based on a cluster analysis performed on reflectivity, slope, and ruggedness. Statistics of clusters were extracted and analysed to identify the optimal number of clusters and evaluate the suitability of the clustering process to differentiate different seabed types. Clusters and samples data were joined to create a training and validation dataset for characterizing the seabed and carrying out an accuracy assessment. Misclassifications were explored and referred to three main reasons: (i) The not-perfect correspondence between sediment boundaries of classification systems and boundaries derived from the clustering process; (ii) the geomorphological features of the seabed; and (iii) the position accuracy of samples. The study contributes to testing of the feasibility of objective methods and highlights the importance of joining acoustic, lithological, and geomorphological analysis. It highlights issues and the need to critically analyse the mapping results and improve the accuracy of collected data.

Highlights

  • Seafloor mapping is the subject of several worldwide research programs dealing with the growing awareness that changes of the marine environmental conditions have to be accurately monitored

  • The analysis of variance performed on the segmented raster shows that the Within-Clusters Sum of Squares (WCSS)/Between-Clusters Sum of Squares (BCSS) ratio quickly decreases as the number of clusters increases from 2 to 5, and becomes approximately constant for more than six clusters

  • Slope and ruggedness substantially contribute to clear characterization of Cluster 5, since a mean value of 15.3◦ and a Terrain Ruggedness Index (TRI) of 0.61 highlight a steeper and more complex morphology compared to other clusters

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Summary

Introduction

Seafloor mapping is the subject of several worldwide research programs dealing with the growing awareness that changes of the marine environmental conditions have to be accurately monitored. The monitoring requirements strongly stimulate the scientific interest in innovative mapping methods and tools, which should be exploitable within the extensive mapping programs carried out by governmental agencies and institutes [1,2,3,4]. Modern hydro-acoustic technologies, supported by samples, provide a robust approach to the seabed investigation. Swath bathymetrical systems record stable and accurate measurements. They simultaneously collect full-coverage bathymetry and backscatter intensities, which strongly enlarges the range of applicable interpretation approaches. Results are artefact-reduced acoustic images, mainly depending on the seabed nature, and suitable for automatic mapping methods

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