“…By assuming that the water body being studied is a homogeneous and incompressible fluid, a hydrostatic pressure distribution can be assumed in the vertical direction, and dynamic changes in temperature and salinity are not considered. The three‐dimensional shallow water wave equations are the continuity equation, the momentum equation, and the free surface equation (Chen et al, 2006; Zhang, Huang, Guo, Song, & Hu, 2019):where , and are the east, north and vertical axes in the Cartesian coordinate system, respectively; , and are the velocity components in the , and directions, respectively; is temperature; is salinity; is density; …”