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不断演变的城市发展对城市内部表面热环境的影响:来自 323 个中国城市的证据。

Impacts of the evolving urban development on intra-urban surface thermal environment: Evidence from 323 Chinese cities.

机构信息

Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, NT, China.

Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, NT, China; Department of Geography and Resource Management, The Chinese University of Hong Kong, Shatin, NT, China.

出版信息

Sci Total Environ. 2021 Jun 1;771:144810. doi: 10.1016/j.scitotenv.2020.144810. Epub 2021 Jan 26.

Abstract

Urban development has significantly modified the surface thermal environment in urban areas. This study provides the first attempt to characterize the urban development imprint on surface thermal environment for 323 cities across the entire country of China, using an intra-urban perspective. Specifically, it investigates the variation of surface thermal environment in terms of land surface temperature (LST) difference triggered by significant urban evolution of intra-urban division containing two primary classes: old urban areas developed by 1992 and new ones expanded in the 1992-2015 period. Under this "old-new" dichotomy, the relationship between urban development and the LST difference is explored through Multi-scale Geographically Weighted Regression (MGWR). Results reveal that urban development is closely related to the difference in LST between old and new urban areas in 2015, which varies from -2.66 °C to 2.46 °C, up to -6.27 °C in western China. 264 cities manifest relatively "cooler" urban environments in the generally larger-sized new urban areas. The seven selected urban development indicators can explain 75% of the variance in the LST difference through MGWR. Among them, the old-new elevation difference, the normalized difference vegetation index (NDVI) difference, and Gini coefficient are found to influence the LST difference in various spatially varying manners. The elevation difference, a generally underestimated nature-driven indicator, is found dominant in explaining the LST difference for 252 cities, among which 216 cities demonstrate higher LSTs in the urban areas with lower elevations. Overall, this study provides valuable information of human-environment interaction across many cities in a generalized way, which complements similar studies at local level, and helps to depict a complete picture of environmental impacts of urban development. The integrated workflow can also be promoted to other periods or other countries to examine the corresponding urbanization imprint on intra-urban surface warming.

摘要

城市发展显著改变了城市地区的地表热力环境。本研究首次尝试从城市内部视角出发,以全国 323 个城市为研究对象,刻画城市发展对地表热力环境的影响。具体而言,研究考察了由于城市内部划分的显著演变而引起的地表热力环境变化,包含两个主要类别:1992 年前发展的老城区和 1992-2015 年扩展的新城区。在这种“新老”二分法下,通过多尺度地理加权回归(MGWR)探讨了城市发展与 2015 年老新城区之间的 LST 差异的关系。结果表明,城市发展与老新城区之间的 LST 差异密切相关,其差异范围在-2.66°C 到 2.46°C 之间,在中国西部可达-6.27°C。264 个城市在一般较大的新城区中表现出相对“凉爽”的城市环境。通过 MGWR,七个选定的城市发展指标可以解释 LST 差异的 75%。其中,新老城区之间的海拔差异、归一化植被指数(NDVI)差异和基尼系数被发现以不同的空间变化方式影响 LST 差异。海拔差异是一个普遍被低估的自然驱动指标,被发现对 252 个城市的 LST 差异具有主导作用,其中 216 个城市的城区海拔较低,其 LST 较高。总体而言,本研究以一种广义的方式为许多城市之间的人-环境相互作用提供了有价值的信息,补充了局部层面的类似研究,并有助于描绘城市发展对环境影响的全貌。该综合工作流程还可以推广到其他时期或其他国家,以研究相应的城市化对城市内部地表变暖的影响。

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