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生态学杂志 ›› 2021, Vol. 40 ›› Issue (10): 3290-3303.doi: 10.13292/j.1000-4890.202110.032

• 研究报告 • 上一篇    下一篇

基于RS技术的皖北城市阜阳市主城区热环境效应分析

姚晓洁*,王霞,姚侠妹   

  1. (安徽建筑大学建筑与规划学院, 合肥 230022)
  • 出版日期:2021-10-10 发布日期:2022-04-01

Thermal environmental effect of the main urban area of Fuyang City in northern Anhui based on RS technology.

YAO Xiao-jie*, WANG Xia, YAO Xia-mei   

  1. (School of Architecture and Urban Planning, Anhui Jianzhu University, Hefei 230022, China).
  • Online:2021-10-10 Published:2022-04-01

摘要: 热岛效应是评估城市环境和气候质量的重要因素。本文基于RS技术,利用地表温度反演、下垫面参数提取、相关性分析等方法,采用2007年、2013年和2018年阜阳市主城区三幅遥感影像,分析各年度地表温度与热场等级的时空分异特征,并在此基础上探究城市热环境的演变趋势和地表温度与地表参数的相关性。结果表明:在各年度中,阜阳市主城区存在着明显的热岛效应,并且随时间呈现先分散后集中的趋势;在时间尺度上,2007—2013年相较于2013—2018年热场等级减弱和不变区域的比例呈现增长趋势,热场等级增强区域的比例呈现下降趋势;在空间上呈现由北至南逐渐增强的趋势;地表温度与归一化植被指数(Normalized Difference Vegetation Index,NDVI)、湿度指数(TC-Wetness,Wet)呈负相关,与归一化建筑指数(Normalized Difference Build up Index,NDBI)、裸土指数(bare soil index,BSI)呈正相关;不同下垫面指数对地表温度的贡献存在很大差异,其中Wet指数对温度降低的作用最强,Wet指数每增加0.1,温度分别降低5.383 ℃(2007年)、2.645 ℃(2013年)和3.289 ℃(2018年)。

关键词: RS, 热岛效应, 温度反演, 地表参数, 阜阳市主城区

Abstract: Heat island effect is an important factor for evaluating urban environment and climate quality. Based on RS technology, we used three remote sensing images of the main urban area of Fuyang City in 2007, 2013, and 2018 to analyze the spatiotemporal variations of land surface temperature and heat field grade using the methods of land surface temperature inversion, underlying surface parameter extraction, and correlation analysis. We further examined the evolution trend of urban thermal environment and the correlation between surface temperature and surface parameters. The results showed that there was an obvious heat island effect in the main urban area of Fuyang City, with the trend being first dispersed and then concentrated with time. Compared with the case during 2013-2018, the proportion of areas with reduced and unchanged thermal field grade increased in 2007-2013, while the proportion of areas with enhanced thermal field grade decreased. Spatially, heat island effect increased gradually from north to south. There was a negative relationship between land surface temperature and Normalized Difference Vegetation Index (NDVI) and TC-Wetness (Wet), but a positive relationship between land surface temperature and Normalized Difference Build-up Index (NDBI) and bare soil index (BSI). The contribution of different underlying surface indices to land surface temperature was different, with Wet index having the strongest effect on reducing temperature. Every 0.1 increase of Wet index would reduce temperature by 5.383 ℃ in 2007, 2.645 ℃ in 2013, and 3.289 ℃ in 2018, respectively.

Key words: RS, heat island effect, temperature inversion, land surface parameter, main urban area of Fuyang City.