An attractive way to predict lightning flash rates in numerical models is to rely on correlations between the lightning flash rate and available model parameters. These correlations can then be used for other applications such as the parameterization to predict the production of nitrogen oxides from lightning. In this study the potential for some model parameters to be used as a proxy for the total lightning rate in cloud resolving model studies has been investigated using the Weather Research and Forecasting model (WRF) in two different storms: the 10 July 1996 STERAO-A severe storm that occurred in the U.S. High Plains and the 13 July 2005 airmass thunderstorm near Huntsville, AL.
It is shown that the WRF model reproduces the structure and morphology of the two storms. We test 5 storm parameters, precipitation ice mass, updraft volume, maximum updraft velocity, ice mass flux product, and ice water path, as proxies for lightning flash rate. Results show that the Price and Rind (1992) power law relation of maximum updraft velocity with flash rate has good correlations with flash rate, and ice mass flux product and precipitation ice mass can repeat the trend in flash rate but not the magnitude. The updraft volume and ice water path predict flash rate poorly.