2021
DOI: 10.3390/fluids6070254
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Improvement of a Diagnostic Urban Wind Model for Flow Fields around a Single Rectangular Obstacle in Micrometeorology Simulation

Abstract: In general, computational fluid dynamics (CFD) models incur high computational costs when dealing with realistic and complicated flows. In contrast, the mass-consistent flow (MASCON) field model provides a three-dimensional flow field at reasonable computational cost. Unfortunately, some weaknesses in simulating the flow of the wake zone exist because the momentum equations are not considered in the MASCON field model. In the present study, a new set of improved algebraic models to provide initial flow fields … Show more

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Cited by 3 publications
(2 citation statements)
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References 18 publications
(58 reference statements)
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“…In the vicinity of a single building, the flow field (Figure 2) is characterized by distinct regions, including the upstream recirculation, rooftop recirculation zone, near-wake zone, and far-wake zone [36]. When multiple buildings encircle an individual structure, the flow fields intersect and interact, giving rise to intricate flow patterns both among the buildings and within the building array.…”
Section: Idealized Simulations Of Microscale Meteorological Processesmentioning
confidence: 99%
“…In the vicinity of a single building, the flow field (Figure 2) is characterized by distinct regions, including the upstream recirculation, rooftop recirculation zone, near-wake zone, and far-wake zone [36]. When multiple buildings encircle an individual structure, the flow fields intersect and interact, giving rise to intricate flow patterns both among the buildings and within the building array.…”
Section: Idealized Simulations Of Microscale Meteorological Processesmentioning
confidence: 99%
“…Replenishment of the ejected air takes place due to the surface layers, which are inhibited, can change direction, carry out a vortex movement and flow from the area of increased pressure to the under-pressure zone. On the windward side there is a stagnation zone (aerodynamic wake zone) [26]. The length of this zone is taken from the condition that the speed of the flow in it is at least 95% of the speed of the undisturbed flow at the same height from the surface of the earth.…”
Section: Theoretical Backgroundmentioning
confidence: 99%