ANALYSIS OF TEMPERATURE REGIME OF LAND SURFACE FOR BYSTRYTSIA RIVER BASIN AND THE INFLUENCE OF TERRAIN ATTRIBUTES USING LANDSAT 8 DATA

A. Mkrtchian, I. Kovalchuk
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Abstract

Terrain morphology is a powerful factor influencing climate characteristics, which manifests itself at various scale levels. At the detailed scale, this effect is mainly due to the redistribution of solar radiation on surfaces and slopes of different slope and aspect, which causes their unequal heating, and local redistribution of air masses. Spatial distribution of land surface temperatures can be effectively studied using remote sensing data in far-infrared range, which can be recalculated into temperature values. The values of the land surface temperature in the Bystrytsia river basin were calculated with far-infrared channels of Landsat spatial images for three time slices: October 5, 2013, February 13, 2015, August 10, 2016. The statistical analysis has been carried out on the impact of terrain morphometric parameters and land surface type and characteristics on its temperature. To determine the relative influence of each specific factor, the method of hierarchical partitioning has been implemented with the hier.part package of R software environment. Significant seasonal differentiation of the influence of individual factors on temperature was revealed. During all the seasons of the year, absolute height appeared as the most significant factor among those analyzed. The influence of absolute height on temperature distribution was the strongest in autumn, somewhat weaker in winter and the weakest in summer. Artificial surfaces, dry grass and soil were heated more strongly despite their lower albedo due to smaller heat consumption by evaporation, whereas vegetation surface and wet soils were less heated. On the other hand, the influence of relative surface insolation, being differentiated by terrain elements appeared to be relatively weaker, which can be explained by the calculation method used (insolation has been calculated for the moment the images were taken, whereas surface heating takes some time). The influence of the level of surface moisture also appeared to be significant. Key words: land surface temperature, Landsat, Bystrytsia, morphometric parameters, hierarchical partitioning.
基于landsat 8数据的柏斯特河流域地表温度变化及地形属性影响分析
地形形态是影响气候特征的重要因素,在不同尺度上均有体现。在细部尺度上,这种影响主要是由于太阳辐射在不同坡度和坡向的地表和斜坡上的再分布,导致其受热不均,以及气团的局部再分布。利用远红外遥感数据可以有效地研究地表温度的空间分布,并将其重新计算为温度值。利用2013年10月5日、2015年2月13日、2016年8月10日三个时间片的Landsat空间影像远红外通道,计算了Bystrytsia河流域的地表温度。统计分析了地形形态参数和地表类型特征对其温度的影响。为了确定各个具体因素的相对影响,采用层次划分的方法,采用分层划分的方法。部分包的R软件环境。各因子对气温的影响具有明显的季节差异。在所有季节中,绝对高度都是最显著的影响因素。绝对高度对气温分布的影响在秋季最强,冬季稍弱,夏季最弱。人工地表、干草和土壤的反照率较低,但由于蒸发热量消耗较小,因此受热更强,而植被表面和湿土壤受热较少。另一方面,相对地表日晒的影响,由于地形要素的差异,似乎相对较弱,这可以解释为所使用的计算方法(日晒是在拍摄图像时计算的,而地表加热需要一段时间)。地表湿度水平的影响似乎也很显著。关键词:地表温度;Landsat; Bystrytsia;
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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