Abstract

Active remote sensing technology represented by multi-beam and lidar provides an important approach for the effective acquisition of underwater coral reef geomorphological information. A spatially continuous surface model of coral reef geomorphology reconstructed from active remote sensing datasets can provide important geomorphological parameters for the research of coral reef geomorphological and ecological changes. However, the surface modeling methods commonly used in previous studies, such as ordinary kriging (OK) and natural neighborhood (NN), often represent a “smoothing effect”, which causes the strong spatial variability of coral reefs to be imprecisely reflected by the reconstructed surfaces, thus affecting the accurate calculation of subsequent geomorphological parameters. In this study, a spatial variability modified OK (OK-SVM) method is proposed to reduce the impact of the “smoothing effect” on the high-precision reconstruction of the complex geomorphology of coral reefs. The OK-SVM adopts a collaborative strategy of global parameter transformation, local residual correction, and extremum correction to modify the spatial variability of the reconstructed model, while maintaining high local accuracy. The experimental results show that the OK-SVM has strong robustness to spatial variability modification. This method was applied to the geomorphological reconstruction of the northern area of a coral atoll in the Nansha Islands, South China Sea, and the performance was compared with that of OK and NN. The results show that OK-SVM has higher numerical accuracy and attribute accuracy in detailed morphological fidelity, and is more adaptable in the geomorphological reconstruction of coral reefs with strong spatial variability. This method is relatively reliable for achieving high-precision reconstruction of complex geomorphology of coral reefs from active remote sensing datasets, and has potential to be extended to other geomorphological reconstruction applications.

Highlights

  • Global environmental changes have posed a strong threat to coral reef ecosystems, with increasing coral reef bleaching and death [1,2,3,4,5,6,7]

  • Since there is no dedicated satellite for coral reef monitoring, most of the data used in passive remote sensing are mainly the optical images of airborne aerial platforms or land satellite platforms [17], and they are susceptible to the influence of the atmosphere and the water column [18]

  • Active remote sensing datasets of multi-beam and lidar are independent of solar radiation sources, which can make up for the limitations imposed by water transparency on passive remote sensing, and has been applied to the survey and evaluation of coral reef geomorphology [19,20,21,22]

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Summary

Introduction

Global environmental changes have posed a strong threat to coral reef ecosystems, with increasing coral reef bleaching and death [1,2,3,4,5,6,7]. 2022, 14, 253 and exploration of coral reef geomorphology and continuously obtain information on coral reef geomorphology and its changes to provide data and a decision-making basis for coral reef research, development, utilization, and protection. Remote sensing technology is regarded as the most promising way to carry out largescale coral reef geomorphology survey and exploration [12,13,14,15,16], mainly including passive remote sensing and active remote sensing. Since there is no dedicated satellite for coral reef monitoring, most of the data used in passive remote sensing are mainly the optical images of airborne aerial platforms or land satellite platforms [17], and they are susceptible to the influence of the atmosphere and the water column [18]. For coral reef geomorphology with strong spatial variability, a high-precision, spatially continuous geomorphological surface is the key to accurately obtain geomorphological parameters

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