文章摘要
陈梦迪1,2 ,张友水1,2*.福州城市扩张对地表温度影响及其空间分异分析[J].海南师范大学学报自科版,2023,36(3):301-311
福州城市扩张对地表温度影响及其空间分异分析
Influence of Urban Expansion on Land Surface Temperature and Spatial Differentiation Analysis in Fuzhou, China
  
DOI:10.12051/j.issn.1674-4942.2023.03.008
中文关键词: 城市热环境  不透水面覆盖度  地理探测器  热效应贡献  混合像元分解  空间分异
英文关键词: urban thermal environment  Impervious Surface Percentage  geodetector  thermal effect contribution  mixed pixel decomposition  spatial heterogeneity
基金项目:国家自然科学基金项目(42271380);福建省自然科学基金项目(2021J01144)
作者单位
陈梦迪1,2 ,张友水1,2* 1. 福建师范大学 地理科学学院/碳中和未来技术学院福建 福州 350117 2. 福建师范大学 地理研究所福建 福州 350117 
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中文摘要:
      基于福州城区两时相 Landsat 影像,根据城市发展程度差异将研究区划分为 Zone 1、 Zone 2、Zone 3三个环形区域,在反演地表温度和获取不透水面覆盖度信息的基础上,计算各区域 各级不透水面覆盖度的热分布指数和热效应贡献度指数,分析2004—2021年福州市不同发展程度 区不透水面覆盖度与地表温度之间的定量关系,并运用地理探测器分析植被覆盖度、不透水面覆 盖度和海拔高度对地表温度(Land Surface Temperature,LST)空间异质性的影响。结果表明:2004— 2021年,Zone 1不透水面扩张较少,Zone 2和Zone 3不透水面扩张明显,增加最明显的为Zone 3内 不透水面覆盖度大于60%的区域;不透水面覆盖度大于60%的区域对城市高温面积贡献最大,不 透水面覆盖度为80% ~ 100%时热效应贡献度最大;2004年影响地表温度的主导因子为植被覆盖 度,2021年Zone 1中不透水面覆盖度为影响地表温度的主导因子,其余区域中海拔高度为影响地 表温度的主导因子;福州市地表温度空间分异受多因子共同影响且两因子交互q值均高于单因子q 值。研究结果可为城市规划和缓解城市热岛效应提供参考。
英文摘要:
      Based on the two-phase Landsat images of Fuzhou urban area, the study area was divided into three ring re⁃ gions (Zone 1, Zone 2, Zone 3) according to the different development degrees of the cities. On the basis of Land Surface Temperature (LST) inversion and the obtained Impervious Surface Percentage (ISP) of the study area, the thermal distribu⁃ tion index and thermal effect contribution index of ISPs in different zones were calculated, and the quantitative relationship between ISP and LST in different development levels of Fuzhou from 2004 to 2021 was analyzed, and the influence of Frac⁃ tional Vegetation Coverage (FVC), ISP and EL on spatial heterogeneity of LST was further analyzed by using geographic probe. The results show that: (1) From 2004 to 2021, the penetration of impervious water surface in Zone 1 is relatively low, while the penetration of impervious water surface in Zone 2 and Zone 3 is obvious. The most obvious increase is in Zone 3 with ISP greater than 60%. (2) The area with ISP greater than 60% contributes the most to the urban high temperature area,and the area with ISP of 80%~100% contributes the most to the thermal effect. The contribution degree of thermal effect in the study area is related to the ISP area at all levels in three regions with different development degrees. (3) From the per⁃ spective of single factor, the dominant factor affecting LST is FVC in 2004, ISP in Zone 1 in 2021, and EL in other ring zones. From the perspective of the interaction of two factors, the spatial differentiation of thermal environment in Fuzhou is the result of multiple factors, and the q value of the interaction of two factors is higher than that of the single factor. The re⁃ sults can provide reference for urban planning and ecological environment construction.
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