In the next set of experiments, the land surface is then classified in to ten urban categories using the Local Climate Zones classification, along with the incorporation of an anthropogenic flux term.This classification improves upon the treatment of urban areas as mere impervious regions and provides a more realistic representation, by parameterizing the canopy scale dynamics on to the mesoscale. These parameters allow us to observe the cascading effect of thermal gradients and heat fluxes within the city, resulting in an improved representation of the convective activity.
The overall theme is to understand the impact of regional scale forcing in the context of larger scale forcings, towards intensifying an extreme heat wave scenario. Findings from this study will hopefully form a stepping stone towards more informed mitigative measures at a regional scale when subject to such extreme stressors.
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