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\begin{document}

\title{Determining Optimal Resolution for Urban Terrain Inputs to Microclimate
Modeling}



\author[1]{Melissa R. Allen-Dumas}%
\author[1]{Levi Thomas Sweet}%
\author[1]{Christa Brelsford}%
\affil[1]{Oak Ridge National Laboratory}%


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  \date{June 12, 2024}


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\textbackslash{}sout

As the numerical weather prediction community seeks deeper understanding
of multi-scale interactions among the atmosphere, human systems and the
overall earth system, more explicit representation of surface terrain in
these models has become necessary. While a great body of work has
examined the differences in error and uncertainty of simulations at
various horizontal grid resolution, no studies have been performed that
compare the results of running the models at the same horizontal grid
resolution but with different resolutions of surface terrain. We examine
the differences in meteorological output from the Weather Research and
Forecasting (WRF) model run at 270m horizontal resolution using 10m
resolution urban terrain (morphology) inputs and 100m resolution inputs.
We find that differences in urban terrain resolution may amplify or
dampen the representation of shortwave absorption by low albedo concrete
and asphalt and the re-radiation of this energy as heat to the
neighborhood.%
\end{abstract}%



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