Structural Uncertainty in the Sensitivity of Urban Temperatures to Anthropogenic Heat Flux

Dan LiTing SunJiachuan YangNing ZhangPouya VahmaniAndrew Jones

Acknowledgment of support from the U.S. Department of Energy, Office of Science, MultiSector Dynamics, Earth and Environmental System Modeling (MSD) program area

DOI:https://doi.org/10.1029/2024MS004431

Abstract

One key source of uncertainty for weather and climate models is structural uncertainty arising from the fact that these models must simplify or approximate complex physical, chemical, and biological processes that occur in the real world. However, structural uncertainty is rarely examined in the context of simulated effects of anthropogenic heat flux in cities. Using the Weather Research and Forecasting (WRF) model coupled with a single-layer urban canopy model, it is found that the sensitivity of urban canopy air temperature to anthropogenic heat flux can differ by an order of magnitude depending on how anthropogenic heat flux is released to the urban environment. Moreover, varying model structures through changing the treatment of roof-air interaction and the parameterization of convective heat transfer between the canopy air and the atmosphere can affect the sensitivity of urban canopy air temperature by a factor of 4. Urban surface temperature and 2-m air temperature are less sensitive to the methods of anthropogenic heat flux release and the examined model structural variants than urban canopy air temperature, but their sensitivities to anthropogenic heat flux can still vary by as much as a factor of 4 for surface temperature and 2 for 2-m air temperature. Our study recommends using temperature sensitivity instead of temperature response to understand how various physical processes (and their representations in numerical models) modulate the simulated effects of anthropogenic heat flux.

Caption: A schematic of four structural variants (SV) of single-layer urban canopy model (SLUCM) (panels a–d) and three Qah release methods (indicated by 1–3 on each panel). (a) SV 1: the default WRF-SLUCM structure; (b) SV 2: a CLMU (Community Land Model—Urban)-like structure where the roof interacts with the canopy air instead of with the atmosphere directly; (c) SV 3: the default SLUCM structure but rc is computed with the momentum roughness length (denoted as r’c); (d) SV 4: a CLMU-like structure and rc is computed with the momentum roughness length (denoted as r’c). In this figure, T is temperature and r is the resistance for heat transfer, and subscripts ARWCG represent atmosphere, roof, wall, canopy air, and canyon ground, respectively. HRG represent the building height, the roof width, and the canyon width, respectively. Qah is a prescribed input that supposedly represents the total anthropogenic heat flux from all sources.

Leave a Reply