Features of the atmospheric boundary layer block for three versions of the WAM wind wave model

The estimated characteristics of the atmospheric boundary layer, obtained by the simulation of wind wave fields using three versions of the WAM numerical model are compared with the well-known empirical dependences of drag coefficient C (d) on wind speed U (10) and wave age A, as well as with the dependence of dimensionless roughness height z (n) on inverse wave age u*/N NEuro. Calculations carried out for several years in the areas of the Pacific and Indian oceans, based on the ERA-interim and CFSR wind reanalyses have shown good agreement between the model and empirical dependences C (d) (U (10)) and C (d) (A). The range of estimated variability for z (n) (u*/N (NEuro) ) has been found to be significantly less than empirical. It has been also found that estimated values of wind speed U (10W) (t) are overestimated from 5 to 10% in all versions of WAM models compared with the input wind reanalysis U (10R) (t) at the moments of appearance maximum values of wind U (10R) (t). The reasons for the established features of the WAM model and their dependence on the model version are discussed.