“…In still scarce studies where flood routing is analyzed with the use of vegetationroughness models, some researchers tend to consider plant properties to be model parameters that should be calibrated, i.e., identified with respect to observations. So, treating them similarly to Manning coefficients, which are usually obtained by the model calibration, where their values are adjusted, ensures an agreement between computed and observed, e.g., water levels, stream velocities, or flow rates -by solving the inverse problem (e.g., Khatibi et al, 1997;Marcinkowski et al, 2018Marcinkowski et al, , 2019Yu et al, 2019). The example is given by Dalledonne et al (2019), who identified vegetation parameters describing, e.g., stem diameters, their heights, drag coefficients, and a leaf area index in the two-dimensional flow model.…”