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Donghai Zheng, Rogier van der Velde, Zhongbo Su, Martijn J. Booij, Arjen Y. Hoekstra, and Jun Wen

and z 0h to calculate u * , θ * , and H cal from Eqs. (2a) – (2e) , 4) use u * and θ * to calculate kB −1 from kB −1 = ln( z 0m / z 0h ) according to each of the four z 0h schemes, and 5) repeat steps 2–4 until the cost function is minimized. c. Noah LSM The Noah LSM is widely used and forms the land component of the regional and global weather forecasting models at the National Centers for Environmental Prediction (NCEP) and of the Weather Research and Forecasting model (WRF

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