"Relationship Between Land Surface Temperature and Imperviousness Density in The Urban Area of Iasi. "

Claudiu Crețu, Pavel Ichim, L. Sfîcă, I. Breabăn
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引用次数: 1

Abstract

This study aims to quantify the relationship between Land Surface Temperature (LST) and Imperviousness Density (IMD) in Iași. This was done through linear regression analysis which involves quantifying the relationship between one independent variable (explanatory, predictor) and one dependent variable (response). Thus, in our study, the dependent variable is represented by the LST product obtained through MODIS sensors in the period 2014-2018, while the independent variable is represented by IMD. The coefficient of determination (R2) obtained, higher than 0.5 for most of the year, indicates a statistically significant relationship between LST and IMD. The highest values of R2 are identified during the day spring and summer seasons. Thus, 70% and respectively 80% of the spatial variation of LST is explained by the distribution of IMD during these two seasons and the regression coefficients indicate, on the one hand, that the relationship between the two variables is a direct one (LST values increase at the same time with IMD values), and on the other hand, that the increase of LST corresponds to a gradient between 0.3-0.6 oC per 10% IMD. During the day, the lowest values of R2 appear in autumn and winter seasons, as a result of the local topography that facilitates the frequency of thermal inversions in this period of the year. On the other hand, during the night, R2 has values between 0.40 and 0.60, with the lowest values in the autumn season and the highest in the spring season, respectively.
“雅西市区地表温度与不透水密度的关系”
本研究旨在量化Iași中地表温度(LST)与不透水密度(IMD)之间的关系。这是通过线性回归分析完成的,其中包括量化一个自变量(解释,预测)和一个因变量(反应)之间的关系。因此,在我们的研究中,因变量以2014-2018年MODIS传感器获得的LST产品表示,自变量以IMD表示。得到的决定系数(R2)在大部分年份都大于0.5,表明LST与IMD之间的关系具有统计学意义。R2的最大值出现在春季和夏季。因此,这两个季节的地表温度的空间变化分别有70%和80%是由IMD的分布来解释的,回归系数表明,两者之间的关系是直接的(地表温度与IMD同时增加),另一方面,地表温度的增加对应于0.3-0.6 oC / 10% IMD之间的梯度。在白天,R2的最低值出现在秋季和冬季,这是由于当地地形有利于一年中这个时期的逆温频率。夜间R2值在0.40 ~ 0.60之间,秋季最小,春季最大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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