Modeling urban canopy air temperature at city-block scale based on urban 3D morphology parameters- A study in Tianjin, North China

被引:10
|
作者
Li, Xiaorui [1 ,2 ]
Yang, Bisheng [1 ,2 ]
Liang, Fuxun [1 ,2 ]
Zhang, Hongsheng [3 ]
Xu, Yong [4 ]
Dong, Zhen [1 ,5 ]
机构
[1] Wuhan Univ, State Key Lab Informat Engn Surveying Mapping & Re, Wuhan, Peoples R China
[2] Wuhan Univ, Engn Res Ctr Spatio temporal Data Smart Acquisit &, Minist Educ China, Wuhan, Peoples R China
[3] Univ Hong Kong, Dept Geog, Hong Kong, Peoples R China
[4] Guangzhou Univ, Sch Geog Sci, Dept Geog Informat Sci, Guangzhou, Peoples R China
[5] Wuhan Univ, Hubei Luojia Lab, Wuhan, Peoples R China
关键词
Urban heat island; Canopy air temperature; Local climate zone; ENVI-met; Urban 3D morphology; Random forest regression; LOCAL CLIMATE ZONES; HEAT-ISLAND; MICROCLIMATE MODEL; SURFACE;
D O I
10.1016/j.buildenv.2023.110000
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Urban 3D morphology significantly influences the outdoor thermal environment. Understanding the influence of urban expansion in both horizontal and vertical landscapes helps the canopy urban heat island (CUHI) effect mitigation. However, the microscale numerical CUHI models are difficult to be applied for large-area CUHI effect studies. On the other hand, the mesoscale CUHI models make a wider study area workable but lost some of the model accuracies. To perform a large-area study on the CUHI effect with relatively light computing costs and fine accuracy, this paper builds a canopy air temperature predicting model at city-block scale with urban 3D morphology parameters including building coverage ratio (BCR), grass coverage ratio (GCR) and the mean value of building height (BH) to obtain the citywide block-mean 2-m temperature (T2M). The model accuracy was validated through RMSEs and comparison with the mereological station data. The proposed model shows an RMSE of 0.286 straight degrees C and an R-square of 0.83. Using the validated model, Tianjin with an area of 647 km 2 was performed to investigate the effects of vertical landscape on the canopy air temperature under different scenarios between 2010 and 2016, including the changes in landcover and building heights. It finds that a 40% increase in BCR may lead to the highest canopy air temperature, and the increase of BH may lead to an increase in the canopy air temperature in low-rise and high-rise building areas, but there is an opposite trend in multi-story and mid-rise building areas.
引用
收藏
页数:11
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