Articles | Volume 13, issue 2
https://doi.org/10.5194/gmd-13-521-2020
https://doi.org/10.5194/gmd-13-521-2020
Development and technical paper
 | 
11 Feb 2020
Development and technical paper |  | 11 Feb 2020

Implementation of a roughness sublayer parameterization in the Weather Research and Forecasting model (WRF version 3.7.1) and its evaluation for regional climate simulations

Junhong Lee, Jinkyu Hong, Yign Noh, and Pedro A. Jiménez

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Cited articles

Arnqvist, J. and Bergström, H.: Flux-profile relation with roughness sublayer correction, Q. J. Roy. Meteorol. Soc., 141, 1191–1197, 2015. 
Basu, S. and Lacser, A.: A Cautionary Note on the Use of Monin–Obukhov Similarity Theory in Very High-Resolution Large-Eddy Simulations, Bound.-Lay. Meteorol., 163, 351–355, 2017. 
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Brunet, Y. and Irvine, M. R.: The control of coherent eddies in vegetation canopies: streamwise structure spacing, canopy shear scale and atmospheric stability, Bound.-Lay. Meteorol., 94, 139–163, 2000. 
Carlson, T. N. and Boland, F. E.: Analysis of urban-rural canopy using a surface heat flux/temperature model, Bound.-Lay. Meteorol., 17, 998–1013, 1978. 
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Short summary
As the computing power increases, the grid size of atmospheric models moves toward the gray zone of turbulence (the scales on the order of the energy-containing range). Nevertheless, the roughness sublayer, which is a compartment of the inertial sublayer, has not been considered in high-resolution mesoscale models. This study coupled a roughness sublayer parameterization into the Weather Research and Forecasting model and evaluated its performance to simulate climate near the Earth's surface.