上海市热环境与生态环境空间格局

Cui Lin-li, Zhou Hongmei, Yang Yinming, Shi Jun, T. Jianguo
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摘要

在过去的三十年里,上海经历了快速的城市化。随着城市的快速发展和扩张,城市下垫面物理特征(如土地覆盖类型、地表反照率等)和性质正在发生重大变化,对气候和生态环境产生重大影响。以Landsat TM遥感影像为基础,结合遥感(RS)和地理信息系统(GIS)空间分析技术,分析了地表温度(LST)、土地利用类型、植被覆盖度、地表反照率以及地表温度与植被关系的空间格局。结果表明,上海城区和近郊的地表温度均高于近郊。城市以居住用地为主,远郊以耕地为主。从市区到远郊,植被覆盖度和地表反照率逐渐增加。市区、近郊和远郊的平均植被覆盖度分别为0.01、0.078和0.126,平均地表反照率分别为0.067、0.083和0.189。上海市地表温度的分布与土地利用类型有较好的对应关系,住区和建筑物的地表温度较高。地表温度与植被覆盖度和归一化植被指数(NDVI)均呈负相关,在城市地区,低植被覆盖度是地表温度升高的重要因素。城市反照率的变化对地表温度的演变有显著影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial pattern of thermal and ecological environment in Shanghai
Shanghai has experienced rapid urbanization over the past three decades. With the rapid development and expansion of city, the physical characteristics (such as land cover types, surface albedo and so on) and property of the urban underlying surface are undergoing substantially changes, which significantly impact the climate and ecological environment. Based on the Landsat TM remote sensing imagery, with the remote sensing (RS) and geographic information system (GIS) spatial analysis techniques, spatial pattern of land surface temperature (LST), land use type, vegetation coverage, surface albedo and the relationship between LST and vegetation was analyzed in this study. The results indicate that LST in urban and suburban areas is higher than that in exurban areas of Shanghai. The dominant land use type in urban areas is residential land, but in exurban areas, farmland is the main land use type. From urban to exurban areas, the vegetation coverage and surface albedo increase gradually. In urban, suburban and exurban areas, the mean vegetation coverage is 0.01, 0.078 and 0.126 respectively, and the mean surface albedo is 0.067, 0.083 and 0.189 respectively. The distribution of LST is well corresponding with the land use types in Shanghai, with residential areas and buildings have higher LST. LST possesses a negative correlation with the vegetation coverage and normalized difference vegetation index (NDVI) for all land cover types, and in the urban areas, the low vegetation coverage is the important contributor of the higher LST. The change in urban albedo has significant impact on the evolution of LST.
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