“…In view of the three-dimensional flow, the RANS equations are solved with a vegetation drag term in the momentum equations and the corresponding vegetation-induced turbulence production terms in the turbulence closure equation (standard k-ε turbulence model, GLS model, and LES method, and other methods) (Jin et al, 2007;Chi-wai and Afis, 2019); this methodology has been verified by a large number of flume data with varying vegetation submergence ratios, densities, and velocities areas (Kombiadou et al, 2014). Scholars have used the numerical simulation method to simulate the influence of vegetation on the wind-induced current in the shallow lakes, but these studies are based on the two-dimensional hydrodynamic model (Xu et al, 2018) and use the method of increasing local Manning coefficient to simulate the vegetation resistance (Li et al, 2020), so it is unable to describe the submerged vegetation effect and the three-dimensional characteristics of shallow lake flow field. In recent years, several open-source three-dimensional models which allow custom editing to study the complex interactions between vegetation and water flow have been developed, such as FVCOM (Morales-Marín et al, 2017), SCHISM (Zhang et al, 2019b), and ROMS (Beudin et al, 2017).…”