Xiao Rong-bo, Ouyang Zhi-yun, Zheng Hua, Li Wei-feng, Schienke Erich W, Wang Xiao-ke
State Key Lab of Urban and Regional Ecology Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
J Environ Sci (China). 2007;19(2):250-6. doi: 10.1016/s1001-0742(07)60041-2.
Land surface temperature (LST), which is heavily influenced by urban surface structures, is a significant parameter in urban environmental analysis. This study examined the effect impervious surfaces (IS) spatial patterns have on LST in Beijing, China. A classification and regression tree model (CART) was adopted to estimate IS as a continuous variable using Landsat images from two seasons combined with QuickBird. LST was retrieved from the Landsat Thematic Mapper (TM) image to examine the relationships between IS and LST. The results revealed that CART was capable of consistently predicting LST with acceptable accuracy (correlation coefficient of 0.94 and the average error of 8.59%). Spatial patterns of IS exhibited changing gradients across the various urban-rural transects, with LST values showing a concentric shape that increased as you moved from the outskirts towards the downtown areas. Transect analysis also indicated that the changes in both IS and LST patterns were similar at various resolution levels, which suggests a distinct linear relationship between them. Results of correlation analysis further showed that IS tended to be positively correlated with LST, and that the correlation coefficients increased from 0.807 to 0.925 with increases in IS pixel size. The findings identified in this study provide a theoretical basis for improving urban planning efforts to lessen urban temperatures and thus dampen urban heat island effects.
地表温度(LST)受城市地表结构的影响很大,是城市环境分析中的一个重要参数。本研究考察了中国北京不透水表面(IS)的空间格局对地表温度的影响。采用分类回归树模型(CART),结合两个季节的Landsat影像和QuickBird影像,将不透水表面作为连续变量进行估算。从Landsat专题制图仪(TM)影像中反演地表温度,以研究不透水表面与地表温度之间的关系。结果表明,分类回归树模型能够以可接受的精度持续预测地表温度(相关系数为0.94,平均误差为8.59%)。不透水表面的空间格局在不同的城乡样带上呈现出变化的梯度,地表温度值呈同心圆状,从郊区向市中心逐渐升高。样带分析还表明,在不同分辨率水平下,不透水表面和地表温度格局的变化相似,这表明两者之间存在明显的线性关系。相关分析结果进一步表明,不透水表面与地表温度呈正相关,且随着不透水表面像素大小的增加,相关系数从0.807增加到0.925。本研究的结果为改进城市规划以降低城市温度、减轻城市热岛效应提供了理论依据。