Abstract

Coastal landscapes are one of the most changeable areas of the earth’s surface. Given this spatial complexity and temporal variability, the construction of reference maps useful for geo-engineering is a challenge. In order to improve the performance of geomorphic models, reliable multiscale and multi-temporal base maps and Digital Elevation Models (DEM) are needed. The work presented in this paper addresses this issue using an inter-geo-disciplinary approach to optimize the processing of multisource and multi-temporal data and DEMs by using field surveys, conceptual model, and analytical computation on a test area. The data acquired with two surveying techniques were analyzed and compared: Aerial Laser Scanning (ALS) and photogrammetry from stereo pairs of High-Resolution Satellite Images (HRSI). To assess the reliability of the DEMs produced from point clouds, the residuals between the point cloud and the interpolated filtered surface were identified and analyzed statistically. In addition to the contour maps, some feature maps such as slope, planar, and profile curvature maps were produced and analyzed. The frequency distribution of the slope and curvature values were compared with the diffusion, advection, and stream power model, revealing a good agreement with the past and present geomorphic processes acting on the different parts of the study area. Moreover, the integrated geomatics–geomorphic analysis of the outliers’ map showed a good correspondence (more than 75%) between the identified outliers and some specific geomorphological features, such as micro-landforms, which are significant for erosive and gravity-driven mechanisms. The different distribution of the above singularities by different data sources allowed us to attribute their spatial model to the temporal variation of the topography and, consequently, to the geomorphic changes, rather than to the different accuracy. For monitoring purposes and risk mitigation activities, the methodology adopted seems to meet the requirements to make a digital mapping of the coast analyzed, characterized by a rapid evolution of the surface, and can be extended to other stretches of coast with similar characteristics.

Highlights

  • Studies aimed at analyzing the evolution of the high and rocky coasts are less numerous than those dedicated to the low and sandy coasts because of their greater economic interest

  • Tests showed that parameter b had a greater impact than parameter a; as parameter b increased and all other parameters were equal, the output surface was smoother and a much greater number of points was removed as was the natural roughness of the ground

  • With regard to the shift value g, our tests have shown that the resulting surface is not very dependent on its value but its combination with the parameter w is significant

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Summary

Introduction

Studies aimed at analyzing the evolution of the high and rocky coasts are less numerous than those dedicated to the low and sandy coasts because of their greater economic interest. Many rocky coastal areas of the Mediterranean coast have been affected by frequent and very intense geomorphological events These include the phenomenon of erosion, which is increasing due to climate changes. Italian rocky coasts such as those of the Abruzzo region, the phenomenon is producing a significant increase in danger and risk for settlements, infrastructure, and residential and tourist buildings [2]. This high level of risk was related both to anthropogenic factors (cut-slopes and deforestation) on the upslope and to an accelerated upslope cliff retreat due to the sea-level rise, increased winter rainfall, and more intense storm activity [3]

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