Abstract
Cities are growing higher and denser, and understanding and constructing the compact city form is of great importance to optimize sustainable urbanization. The two-dimensional (2D) urban compact form has been widely studied by previous researchers, while the driving mechanism of three-dimensional (3D) compact morphology, which reflects the reality of the urban environment has seldom been developed. In this study, land surface temperature (LST) was retrieved by using the mono-window algorithm method based on Landsat 8 images of Xiamen in South China, which were acquired respectively on 14 April, 15 August, 2 October, and 21 December in 2017, and 11 March in 2018. We then aimed to explore the driving mechanism of the 3D compact form on the urban heat environment (UHE) based on our developed 3D Compactness Index (VCI) and remote sensing, as well as Geo-Detector techniques. The results show that the 3D compact form can positively effect UHE better than individual urban form construction elements, as can the combination of the 2D compact form with building height. Individually, building density had a greater effect on UHE than that of building height. At the same time, an integration of building density and height showed an enhanced inter-effect on UHE. Moreover, we explore the temporal and spatial UHE heterogeneity with regards to 3D compact form across different seasons. We also investigate the UHE impacts discrepancy caused by different 3D compactness categories. This shows that increasing the 3D compactness of an urban community from 0.016 to 0.323 would increase the heat accumulation, which was, in terms of satellite derived LST, by 1.35 °C, suggesting that higher compact forms strengthen UHE. This study highlights the challenge of the urban 3D compact form in respect of its UHE impact. The related evaluation in this study would help shed light on urban form optimization.
Highlights
Building height of the selected communities ranged from 1 floor to 38 floors, with an average of 9 floors, while the building density had an average of 35.781%, as compared to the highest value of 85.257% and the lowest of 10.198%
The results showed that NVCI had varying impacts on heat accumulation exhibited levels from 3 (31.84%, 8 floors) to 2 (41.44%, 8 floors), and level 1
land surface temperature (LST) that was derived from Landsat 8 imagery
Summary
The urban form plays an important role in the accommodation of human urban activities and has changed greatly during a period of rapid urbanization. One obvious change is the expansion of urban land to support rapidly growing urban populations. The urban population accounted for 55% of the world’s population in 2018 and is expected to grow to 68% in 2050 according to the 2018 revision of World Urbanization Prospects [1]. Unlimited land expansion is not possible owing to limited land resources. Urbanization is accelerating and the living standards of people are improving, while the current
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