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Jeffrey D. Massey, W. James Steenburgh, Jason C. Knievel, and William Y. Y. Cheng

) reduced the early morning warm bias in WRF simulations of three fall days over northern Utah through the use of an alternate soil thermal conductivity parameterization combined with soil moisture analyses based on in situ observations. The afternoon cold bias, however, was only partially reduced in Massey et al. (2014) and remains associated with a myriad of plausible, yet untested, error sources including 1) differences between model and observation site elevations ( Liu et al. 2008b

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