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作者

来源

OPEN HOUSE INTERNATIONAL,Vol.42,Issue3,P.108-111

语言

英文

关键字

Core Water Surface Ratio; Scale Sensitivity; Attenuation; Uhi Intensity; Remote Sensing

作者单位

[Xu, Jiangang] Nanjing Univ, Sch Architecture & Urban Planning, Nanjing, Jiangsu, Peoples R China. Nanjing Forestry Univ, Coll Landscape Architecture, Nanjing, Jiangsu, Peoples R China. Tianjin Univ, Sch Architecture, Tianjin, Peoples R China. Tianjin Planning Bur Tianjin, Tianjin, Peoples R China. Kyoto Univ, Grad Sch Global Environm Studies, Kyoto, Japan. Xu, JG (reprint author), Nanjing Univ, Sch Architecture & Urban Planning, Nanjing, Jiangsu, Peoples R China. E-Mail: xjg129@sina.com

摘要

Urban water bodies play an important role in reducing summertime urban heat island (UHI) effects. Previous studies focused mainly on the impact of water bodies of large areas, and there is no analysis of the efficacy and scale effect of how small and medium-sized water bodies reduce the UHI effects. Hence, these studies could not provide theoretical support for the scientific planning and design of urban water bodies. This study aims to confirm, within different scale ranges, the efficacy of a water body in reducing the summertime UHI effects. We propose a scale sensitivity method to investigate the temporal and spatial relationship between urban water bodies and UHI. Based on the scale theory and geostatistical analysis method in landscape ecology, this study used the platforms of 3S, MATLAB, and SPSS to analyze the distance-decay law of water bodies in reducing summertime UHI effects, as well as the scale response at different water surface ratios. The results show that the influence of water surfaces on UHIs gradually decreases with increasing distance, and the temperature rises by 0.78 degrees C for every 100 m away from the water body. During daytime, there is a scaled sensitivity of how much water surfaces reduce the summertime UHI effects. The most sensitive radius from the water was found at the core water surface ratio of 200 m. A reduction of UHI intensity by 2.3 degrees C was observed for every 10% increase of the average core water surface ratio. This study provides a theoretical reference to the control of heat islands for the planning and design of urban water bodies.