Tuesday, 7 January 2025
The urban canopy layer (UCL) is characterized by a heterogeneous flow pattern that responds to complex urban geometries. The varying heights and layouts of buildings play a pivotal role in shaping this spatial variability, as they block, divert, and slow wind and determine the exchange of momentum and energy above the urban canopy. When representing these complex dynamics, however, research has conventionally relied on microscale simulations conducted over limited (often idealized) building arrays. Extending the findings to realistic urban neighbourhoods and urban parameterizations presents a clear limitation, as evidenced by discrepancies in multi-model comparisons with observational data in cities. The discrepancies are better amended by incorporating urban flux tower observation that reflects the most realistic flow pattern within UCL. However, the flux tower observation only covers a few cities under limited meteorological conditions, which is inadequate to cover heterogeneous urban flow patterns over global cities.
More extensive datasets of urban airflow are needed to cover a range of realistic urban neighbourhoods and provide a more holistic analysis of turbulent flow in different urban characteristics. Responding to this gap in the field, we developed a historically extensive Urban Turbulent Airflow using systematic Large Eddy Simulations (UrbanTALES) dataset over 600 urban layouts with both idealized and realistic configurations. Realistic urban neighbourhoods were obtained from major cities worldwide, incorporating variations in plan area densities [0.0625-0.64] and height distributions [4-70m]. Idealized urban arrays, on the other hand, include two commonly studied configurations (aligned and staggered arrays), featuring both uniform and variable height scenarios along with oblique wind directions.
UrbanTALES offers canopy-averaged data as well as 2D and 3D flow fields tailored for different applications in urban climate research. The dataset provides time-averaged wind flow properties, as well as second- and third-order flow moments that are critical for a) revisiting neighbourhood-scale urban canopy parameterizations in various models and b) informing in-canopy flow and turbulent analyses.
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