Parallel and normal currents had different responses to different topography types. Results showed remarkable agreement between 3- D current analysis and surface velocity analysis. In this research, we analyzed the distribution characteristics of current velocity and velocity gradient in different cases using a 3- dimensional (3- D) hydrodynamic model to discuss the current–topography interaction part of the remote sensing imaging mechanism, especially the modulation by current parallel or normal to the underwater topography, both positive and negative. Current velocity is highly correlated with bathymetry, and velocity gradient is used as an indicator of sea surface roughness. In addition, few studies focused on different topography patterns. However, current–topography interaction constitutes the weakest link in the remote sensing imaging mechanism of underwater topography. Numerous studies have been conducted to understand the imaging mechanism of shallow water topography. Underwater topography can be imaged using remote sensing methods. Analysis of current–topography interaction in remote sensing imaging procedures for shallow water topography.
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