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Driving forces of UHI changes in China's major cities from the perspective of land surface energy balance.
Hou, Haoran; Su, Hongbo; Liu, Kai; Li, Xueke; Chen, Shaohui; Wang, Weimin; Lin, Jinhuang.
Afiliación
  • Hou H; Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
  • Su H; Department of Civil, Environmental and Geomatics Engineering, Florida Atlantic University, Boca Raton, FL 33431, USA. Electronic address: suh@fau.edu.
  • Liu K; Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources, Chinese Academy of Sciences, Beijing 100101, China.
  • Li X; Institute at Brown for Environment and Society, Brown University, Providence, RI 02912, USA.
  • Chen S; Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources, Chinese Academy of Sciences, Beijing 100101, China.
  • Wang W; Shenzhen Environmental Monitoring Center, Shenzhen 518049, China.
  • Lin J; School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China.
Sci Total Environ ; 829: 154710, 2022 Jul 10.
Article en En | MEDLINE | ID: mdl-35331766
As remarkable human-induced temperature anomalies on the land surface, variations of urban heat island (UHI) and its driving factors have been investigated in numerous studies. However, few studies discussed the spatiotemporal heterogeneity of the driving forces exerted by land surface energy fluxes, i.e., net radiation, sensible heat, latent heat and heat storage, on UHI behaviors at large scale and long term. In this study, a comprehensive application of multisource datasets and statistical methods have been implemented based on land surface energy balance theory, the spatiotemporal variations of surface UHI intensity (urban-rural temperature difference) and changes of their driving forces have been quantified. The results demonstrate the dynamics of UHI intensity in 32 major cities of China from 2003 to 2017 are generally coherent with the common perception, the overall surface UHI intensity is 4.57 K higher in summer than in winter. The spatial variations of the fluxes that alter UHI intensity can be largely attributed to the varied energy interactions between vegetated/paved surface and atmosphere and the differences of background temperature and precipitation, the contribution of latent heat to UHI changes declines nearly 40% from semiarid/arid climate at the north to subtropical humid climate at the south, while the contributions of other fluxes are stable. The temporal changes of the effect of these fluxes, however, imply more complex mechanisms. The contributions of sensible heat and latent heat to UHI intensity variations are three times and eight times larger in the warm season than in the cold season respectively, indicating the influence of seasonality of background temperature, precipitation and vegetation. The low contributions of these fluxes in the cold season also suggest the significant effect of other driving forces such as anthropogenic heat, especially in semiarid/semihumid climate zones. This study highlights the temporal shifts of major driving forces of UHI intensity, the mitigation tactics for UHI in different cities and seasons should be customized for better validity.
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Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Monitoreo del Ambiente / Calor Límite: Humans Idioma: En Revista: Sci Total Environ Año: 2022 Tipo del documento: Article País de afiliación: China

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Monitoreo del Ambiente / Calor Límite: Humans Idioma: En Revista: Sci Total Environ Año: 2022 Tipo del documento: Article País de afiliación: China