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Relationship Between Land Cover Ratio and Urban Heat Island from Remote Sensing and Automatic Weather Stations Data

机译:遥感与自动气象站数据的土地覆盖率与城市热岛的关系

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Urban heat island (UHI) effect has a close relation to land covers type. This paper investigates the relationship between land cover ratio and UHI in Guangzhou, south of China using remote sensing and automatic weather stations data. The temperature data were obtained by Automatic weather stations (AWS) of Guangzhou in October, 2004, at the same time with the CBERS remote sensing image acquired. Firstly, the hourly mean temperature was computed from hourly AWS data. Secondly, the CBERS remote sensing image was classified using support vector machine (SVM) and land covers classification were output. Thirdly, the classification result was overlapped with a round buffer with 1.5 KM radius centered on the AWS, and then the land cover ratio, Edge Density (ED) and Mean Fractal Dimension (MFRACT) of buffers were computed out. Finally, the correlation coefficient between hourly mean temperature and land cover ratio, ED and MFRACT was calculated. It concluded that UHI intensity was heavier during nighttime than daytime. Stations with higher vegetation ratio and higher ED had lower heat island effect. On the contrary, stations with higher impervious ratio and lower ED had more serious heat island effect. The positive-negative of correlation coefficient between hourly mean temperature and vegetation ratio during 11:00-17:00 h (local time) was opposite to that during other time. ED was negatively correlated with hourly mean temperature except during 11:00-17:00 h. On the contrary, MFRACT was positively correlated with hourly mean temperature. It implied that fragmentations of patches were favorable to UHI alleviation, and complexities of patch were unfavorable factors.
机译:城市热岛效应与土地覆盖类型密切相关。本文利用遥感和自动气象站数据,研究了华南地区广州市土地覆盖率与UHI之间的关系。温度数据是在2004年10月由广州自动气象站(AWS)获得的,同时获得了CBERS遥感图像。首先,根据每小时的AWS数据计算每小时的平均温度。其次,利用支持向量机(SVM)对CBERS遥感图像进行分类,并输出土地覆盖分类。第三,将分类结果与以AWS为中心,半径为1.5 KM的圆形缓冲区重叠,然后计算缓冲区的土地覆盖率,边缘密度(ED)和平均分形维数(MFRACT)。最后,计算了小时平均温度与土地覆盖率,ED和MFRACT之间的相关系数。结论是,夜间UHI强度比白天高。植被比例较高和ED较高的站的热岛效应较低。相反,具有较高的不透水率和较低的ED的站具有更严重的热岛效应。当地时间11:00-17:00 h,小时平均温度与植被比之间的相关系数为正,与其他时间相反。除11:00-17:00时外,ED与小时平均温度呈负相关。相反,MFRACT与小时平均温度呈正相关。暗示斑块的碎片化有利于UHI的缓解,斑块的复杂性是不利的因素。

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