“…They are often used to describe geophysical flows (such as rivers, lakes, coastal areas, etc. ), rainfall runoff, tsunami propagation, or even atmospheric flows, given the appropriate initial conditions and source terms (Backhaus, 1983;Cea & Bladé, 2015;Rahman & Mandokhail, 2018;Galewsky, Scott & Polvani, 2004;Fu et al, 2017;Liu et al, 2008Liu et al, , 1995. SWE are derived from the Navier-Stokes equations, with the main assumption that the horizontal length scale is much greater than the vertical length scale.…”