2015
DOI: 10.1007/s00704-015-1655-z
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A prediction model for wind speed ratios at pedestrian level with simplified urban canopies

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Cited by 34 publications
(7 citation statements)
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“…When the height of each building in the typical block was increased, the breeze zone on the leeward side of the buildings in the upwind area increased. This is consistent with the research findings of Ikegaya et al [43] , that is, regarding the correlation coefficient between the wind speeds averaged over the entire region, the values in the front or side region were greater than 0.9, while in the area behind a building, the wind speeds were weakly correlated. The proportion of the calm wind in the typical block increased, and the proportion of the light air significantly decreased.…”
Section: Impact Of Building Height Changes On Wind Environmentsupporting
confidence: 93%
“…When the height of each building in the typical block was increased, the breeze zone on the leeward side of the buildings in the upwind area increased. This is consistent with the research findings of Ikegaya et al [43] , that is, regarding the correlation coefficient between the wind speeds averaged over the entire region, the values in the front or side region were greater than 0.9, while in the area behind a building, the wind speeds were weakly correlated. The proportion of the calm wind in the typical block increased, and the proportion of the light air significantly decreased.…”
Section: Impact Of Building Height Changes On Wind Environmentsupporting
confidence: 93%
“…Frontal area index (FAI) has been adopted in urban thermal [26] [27] and wind environment studies [28] [29]. The FAI is an indicator describing the blocking effect of buildings on wind [30], and it describes an averaged status of urban forms at the entire urban canopy level [31] [32].…”
Section: Introductionmentioning
confidence: 99%
“…The heat island intensity was categorized into seven levels [12]: a strong cold island (SCI), sub-strong cold island (SSCI), weak cold island (WCI), no heat island (NHI), weak heat island (WHI), sub-strong heat island (SSHI), and strong heat island (SHI) (Table 1). Studies have shown that in summer, urban surface temperatures follow the following pattern: bodies of water < forests < crops < lawns < bare lands < buildings [13]. Due to the temperature difference between the built-up area and water bodies or forest land, the flow of cold fresh air can be generated even under weak background wind conditions, which can effectively alleviate the urban heat island effect [14].…”
Section: Assessment Of Thermal Environmentmentioning
confidence: 99%