Abstract

Airborne LiDAR bathymetry (ALB) is efficient and cost effective in obtaining shallow water topography, but often produces a low-accuracy sounding solution due to the effects of ALB measurements and ocean hydrological parameters. In bathymetry estimates, peak shifting of the green bottom return caused by pulse stretching induces depth bias, which is the largest error source in ALB depth measurements. The traditional depth bias model is often applied to reduce the depth bias, but it is insufficient when used with various ALB system parameters and ocean environments. Therefore, an accurate model that considers all of the influencing factors must be established. In this study, an improved depth bias model is developed through stepwise regression in consideration of the water depth, laser beam scanning angle, sensor height, and suspended sediment concentration. The proposed improved model and a traditional one are used in an experiment. The results show that the systematic deviation of depth bias corrected by the traditional and improved models is reduced significantly. Standard deviations of 0.086 and 0.055 m are obtained with the traditional and improved models, respectively. The accuracy of the ALB-derived depth corrected by the improved model is better than that corrected by the traditional model.

Highlights

  • Airborne LiDAR bathymetry (ALB) is an accurate, cost-effective, and rapid technique for shallow water measurements [1,2,3,4,5,6]

  • The height models of green ALB systems proposed by Jianhu Zhao et al [38] that consider near water surface penetration (NWSP) of the green laser should be used to correct the green water surface and water bottom heights

  • The t-test of the model coefficient showed that all of the parameters in the improved model are significant and should be included, which indicates that the proposed improved model is reasonable

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Summary

Introduction

Airborne LiDAR bathymetry (ALB) is an accurate, cost-effective, and rapid technique for shallow water measurements [1,2,3,4,5,6]. IR laser is used to detect the water surface accurately, depth bias is mainly induced by pulse stretching of the green bottom return [2,13,14]. 2 2ofof1616 temporal stretching of the received green bottom return, and this phenomenon is known as the pulse stretching effect [1,2,3,13,14,15,16]. Peak shifting induces is bias in bathymetry estimates that based onstretching a peak detection effect [1,2,3,13,14,15,16]. Small waves develop [17].isAs gainssurface energy, waves surface waves alsocapillary affect depth bias. Actual received green bottom return distorted by the pulse stretching effect, and round-trip time of the ideal green bottom return, respectively

A Monte simulation is used depth biases with the impulse response
Influencing Factors and Depth Bias Model
Development of the Depth Bias Model
Variable Selection for the Depth Bias Model
Data Acquisition
Model Construction
Influence Analysis
Accuracy Analysis
Discussion
With the the sounding result the residual residualdepth depth biases in
Conclusions and Suggestions
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