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The study of turbulent boundary layer flow holds significant importance in urban climate research, particularly concerning numerical simulation studies where it serves as a crucial inflow boundary condition. However, understanding the turbulent boundary layer's influence on flow and heat features within canyon and canopy flow remains incomplete. To address this knowledge gap, our current work employs simultaneous Particle Image Velocimetry and Laser-Induced Fluorescence (PIV-LIF) measurements within a large closed-circuit water tunnel. Through this approach, we obtain valuable flow information under various flow and thermal conditions, allowing us to explore the impacts of three distinct turbulent boundary layer flows. The three chosen turbulent boundary layer flows display distinct influences on flow characteristics and heat removal capacity. The ventilation rate exhibits a maximum difference of 80% among the tested boundary layer flows. Additionally, the most significant variation in heat removal capacity is approximately 45%. Moreover, the different turbulence inlet profiles result in diverse fluctuating features at the canyon opening, while the deeper region of the canyon remains less affected.

Urban areas are known for their complex atmospheric environments, with the building morphology having a significant impact on local climate patterns, air quality, and overall urban microclimate. Understanding the heat transport and fluid flow in complex urban environments is crucial for improving urban climate resilience, which remains an open frontier in the field of urban studies. To gain a more profound insight into the physical processes occurring in urban areas, particularly within street canyons, we conducted an experimental investigation in a large-scale water tunnel. This study involved the simultaneous examination of heat and flow fields, carried out at high spatial and temporal resolutions, utilizing Laser-induced Fluorescence (LIF) for heat analysis and Particle Image Velocimetry (PIV) for flow analysis. Our results of heat and flow in different street canyons indicate that the flow is significantly influenced by a combination of factors, including canyon configuration, the presence of buoyant force, and the magnitude of the approaching flow. The ventilation rate and heat flux from the street canyon, which are key factors shaping the urban microclimate, are found dominated significantly by the street canyon morphology. For instance, changing the aspect ratio of a street canyon results in a significant change of air ventilation rate, ranging from as low as 0.02 to as high as 1.5 under the same flow conditions. Additionally, canyons with high air ventilation rates exhibit significant heat flux removal at the canyon roof level, which is accurately described by the local Richardson number.