An updated parameterization of the unstable atmospheric surface layer in the Weather Research and Forecasting (WRF) modeling system

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Abstract

The accurate parameterization of atmospheric surface layer processes is crucial for weather forecasts using numerical weather prediction models. Here, an attempt has been made to improve the surface layer parameterization in the Weather Research and Forecasting model version 4.2.2 (WRFv4.2.2) by implementing similarity functions proposed by Kader and Yaglom (1990) to make it consistent in producing the transfer coefficient for momentum observed over the tropical region (Srivastava and Sharan, 2015). The surface layer module in WRFv4.2.2 is modified in such a way that it contains the commonly used similarity functions for momentum ('m) and heat ('h) under convective conditions instead of the existing single functional form. The updated module has various alternatives of 'm and 'h, which can be controlled by a flag introduced in the input file. The impacts of utilizing different functional forms have been evaluated using the bulk flux algorithm as well as real-case simulations with the WRFv4.2.2 model. The model-simulated variables have been evaluated with observational data from a flux tower at Ranchi (23.412 N, 85.440 E), India, and the ERA5-Land reanalysis dataset. The transfer coefficient for momentum simulated using the implemented scheme is found to agree well with its observed non-monotonic behavior in convective conditions (Srivastava and Sharan, 2021). The study suggests that the updated surface layer scheme performs well in simulating the surface transfer coefficients and could be potentially utilized for the parameterization of surface fluxes under convective conditions in the WRF model. Author(s) 2024..

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Namdev, P., Sharan, M., Srivastava, P., & Mishra, S. K. (2024). An updated parameterization of the unstable atmospheric surface layer in the Weather Research and Forecasting (WRF) modeling system. Geoscientific Model Development, 17(22), 8093–8114. https://doi.org/10.5194/gmd-17-8093-2024

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