AI Article Synopsis

  • The study investigates the cooling effects of vertical greenery systems (VGSs) in street canyons with different aspect ratios (H/W = 1 and 2) in Guangzhou, focusing on their impact on urban wind and temperature.
  • On a hot day, VGSs reduced wind speed substantially (38.0% for H/W = 1 and 21.0% for H/W = 2) and significantly decreased temperatures across various surfaces and air.
  • The VGS with H/W = 2 showed greater temperature reductions, especially at upper levels in the canyons, highlighting the importance of design and placement for maximizing cooling effects in urban environments.

Article Abstract

Many studies have focused mainly on the thermal and energy performance of VGSs on a building scale; however, little is known about the cooling effect of VGSs in street canyons and its response to different aspect ratios (building height/street width, H/W). Therefore, a scaled outdoor experiment was conducted to investigate the spatiotemporal variation of the urban wind and thermal environment caused by west-facing vertical greenery systems (VGSs) in street canyons with H/W = 1 and 2 in the subtropical city of Guangzhou, China. On a typical hot day (26th Oct. 2021), VGSs reduced wind speed by 38.0 % and 21.0 % in street canyons with H/W = 1 and 2, respectively. Compared with the reference cases, the temperature regimes of VGS cases (H/W = 1 and 2), including west-facing wall temperature (T), east-facing wall temperature (T), ground temperature (T), and air temperature (T), were all significantly decreased. Because of the cooling effect of VGSs, the maximum reduction of T in the upper level of street canyons with H/W = 1 and 2 was 20.3 and 16.8 °C, respectively. The maximum reduction of T in the center of the VGS case with H/W = 2 was 4.6 °C, which was more pronounced than in the VGS case with H/W = 1 (1.8 °C). The maximum reduction of T at the pedestrian level along the central axis of street canyons with H/W = 1 and 2 was 0.8 and 1.6 °C, respectively, which was more pronounced than at the upper level. The reduction of T in the upper level and of T and T in the VGS case with H/W = 2 was greater than that in the VGS case with H/W = 1 due to lower wind speed and albedo.

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Source
http://dx.doi.org/10.1016/j.scitotenv.2022.160408DOI Listing

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