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Relationships of LST to NDBI and NDVI in Wuhan City based on Landsat ETM+ image

机译:基于Landsat ETM +图像的武汉市LST与NDBI和NDVI的关系

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Based on four Landsat ETM+ images covering Wuhan City, Normalized Difference Vegetation Index (NDVI) and Normalized Difference Built-up Index (NDBI) in spring, summer, autumn and winter were calculated. The land surface temperature (LST) of the city in four seasons was estimated using the radiative transfer model. The spatial and temporal pattern and characteristics of NDVI, NDBI and LST and their relationship were analyzed in detail. Results show that the regions with higher NDBI and LST values were mainly in the municipal district of Wuhan City, including Hankou and Wuchang. The maximum NDBI of the district in four seasons was 0.669, 0.685, 0.659 and 0.703 respectively, while the maximum LST was 43.529°C, 59.849°C, 47.143°C and 23.875°C. Higher NDVI values were mainly distributed in the regions such as along the Han River, the lake beach and the wetlands area in the southwest and central hilly areas, and the maximum NDVI in different seasons was 0.432, 0.564, 0.442 and 0.158 respectively. There existed a strong positive correlation between NDBI and LST in all seasons. The Pearson's correlation coefficient in four seasons was 0.639, 0.717, 0.807 and 0.762 respectively. In autumn, NDBI and LST were most significantly correlated. The relationship between NDVI and LST changed with season, but without obvious regularity. The correlation between NDVI and LST was weaker in four seasons than that between NDBI and LST, with the Pearson coefficients of −0.515, −0.577, −0.246 and −0.038 respectively. NDVI values had negatively linkage with NDBI. The Pearson's correlation coefficients in four seasons was −0.568, −0.582, −0.536 and −0.242, which indicated that NDVI could be used to characterize the evolution of urban construction land. The throughout study suggests that NDBI not only can be used as an important indicator to analyze LST and urban heat island effects, but also will- provide a reliable basis for urban construction and planning.
机译:根据覆盖武汉市的四幅Landsat ETM +图像,计算了春季,夏季,秋季和冬季的归一化植被指数(NDVI)和归一化植被指数(NDBI)。使用辐射传输模型估算了该城市四个季节的地表温度(LST)。详细分析了NDVI,NDBI和LST的时空格局,特征及其相互关系。结果表明,NDBI和LST值较高的地区主要集中在武汉市辖区,包括汉口和武昌。该地区四个季节的最大NDBI分别为0.669、0.685、0.659和0.703,而最大LST则为43.529°C,59.849°C,47.143°C和23.875°C。 NDVI值较高的地区主要分布在汉江,湖滩和西南部和中部丘陵区的湿地地区,不同季节的NDVI最大值分别为0.432、0.564、0.442和0.158。在所有季节,NDBI和LST之间都存在很强的正相关。四个季节的皮尔逊相关系数分别为0.639、0.717、0.807和0.762。秋季,NDBI和LST的相关性最高。 NDVI和LST之间的关系随季节而变化,但没有明显的规律性。在四个季节中,NDVI和LST之间的相关性比NDBI和LST之间的相关性弱,皮尔逊系数分别为-0.515,-0.577,-0.246和-0.038。 NDVI值与NDBI负相关。四个季节的皮尔逊相关系数为-0.568,-0.582,-0.536和-0.242,这表明NDVI可用于表征城市建设用地的演变。整个研究表明,NDBI不仅可以用作分析LST和城市热岛效应的重要指标,而且还将为城市建设和规划提供可靠的基础。

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