A Revised Scheme for the WRF Surface Layer Formulation

Author:

Jiménez Pedro A.1,Dudhia Jimy2,González-Rouco J. Fidel3,Navarro Jorge4,Montávez Juan P.5,García-Bustamante Elena6

Affiliation:

1. División de Energías Renovables, CIEMAT, Madrid, Spain, and Mesoscale and Microscale Meteorology Division, NCAR, Boulder, Colorado

2. Mesoscale and Microscale Meteorology Division, NCAR, Boulder, Colorado

3. Departamento de Astrofísica y Ciencias de la Atmósfera, Universidad Complutense de Madrid, Madrid, Spain

4. División de Energías Renovables, CIEMAT, Madrid, Spain

5. Departamento de Física, Universidad de Murcia, Murcia, Spain

6. Departamento de Astrofísica y Ciencias de la Atmósfera, Universidad Complutense de Madrid, and División de Energías Renovables, CIEMAT, Madrid, Spain

Abstract

AbstractThis study summarizes the revision performed on the surface layer formulation of the Weather Research and Forecasting (WRF) model. A first set of modifications are introduced to provide more suitable similarity functions to simulate the surface layer evolution under strong stable/unstable conditions. A second set of changes are incorporated to reduce or suppress the limits that are imposed on certain variables in order to avoid undesired effects (e.g., a lower limit in u*). The changes introduced lead to a more consistent surface layer formulation that covers the full range of atmospheric stabilities. The turbulent fluxes are more (less) efficient during the day (night) in the revised scheme and produce a sharper afternoon transition that shows the largest impacts in the planetary boundary layer meteorological variables. The most important impacts in the near-surface diagnostic variables are analyzed and compared with observations from a mesoscale network.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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