长沙都市圈不透水面覆盖时空格局分析

Wu Meng-Fan, Yang Bo, Huo Fei-fei, Liao Liu-Wen
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引用次数: 0

摘要

基于线性光谱混合模型(LSMM)、地带性统计、样带分析和城市土地覆被转换分析,提取了2005年、2009年和2013年长沙都市区不透水面覆盖度(ISC),分析了2005-2013年长沙都市区不透水面覆盖度的时空格局。结果表明:(1)增加和提高暗植被比例可以减少低反照率和阴影的误分类。(2)长沙都市圈ISC增长主要发生在2005 - 2009年。不透水表面由中心向四周扩展。2009-2013年,城市绿地建设受到高度重视。(3)不透水地表与植被的转化主要出现在市区和县域。土壤向不透水面的转变主要发生在2005 - 2009年。(4)长沙都市圈不透水面覆盖度(ISC)与地表温度(LST)呈线性关系。城市地表温度上升的主要原因是不透水地表密度高,而不是低密度和分散的不透水地表。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analyses on spatiotemporal patterns of impervious surface coverage in Changsha metropolitan area
Based on Linear Spectral Mixture Model (LSMM), Zonal Statistic, Transect analyses, and Transformation analyses of urban land cover, we extracted out the Impervious Surface Coverage (ISC) of Changsha metropolitan area in 2005, 2009, and 2013, and analyzed its spatiotemporal patterns in 2005-2013. The results were: (1) we reported that increasing and improving proportion of dark vegetation can reduce the misclassification of low albedo and shadow. (2) The main increase of ISC in Changsha metropolitan area was in 20052009. Impervious surface expanded from the center to all around. The construction of urban greenspace was paid closely attention in 2009-2013. (3) The transformation between impervious surface and vegetation appeared mainly in downtown and counties. The transform from soil to impervious surface mainly arose in 20052009. (4) The Impervious Surface Coverage (ISC) and Land Surface Temperature (LST) had linear relationship in Changsha Metropolitan Area. The primary reason for the rising of urban land surface temperature (LST) was high density of impervious surface, not low density and scattered ones.
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