首页> 外文期刊>Arabian journal of geosciences >Assessment of spatial relationship between land surface temperature and landuse/cover retrieval from multi-temporal remote sensing data in South Karkheh Sub-basin, Iran
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Assessment of spatial relationship between land surface temperature and landuse/cover retrieval from multi-temporal remote sensing data in South Karkheh Sub-basin, Iran

机译:评估伊朗南卡尔凯次流域多时相遥感数据中地表温度与土地利用/覆盖物恢复之间的空间关系

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摘要

Land surface temperature (LST) is a required input data for modeling in climatological, hydrological, apicultural, and change detection studies. In the current study, remotely sensed thermal infrared data were applied to assess LST in south Karkheh sub-basin, Iran. This research deals with the extraction of LST and land surface emissivity (LSE) and the relationship between vegetation abundance using Landsat 5 TM and Landsat 7 ETM+ for October 1998 and 2002 over the studied area. The landuse/land cover (LULC) map was derived by using maximum likelihood classifier. The variety of LSE was investigated and extracted on the basis of NDVI threshold method, as well as the Plank equation was used to derive LST over the study region. The relationship between LST and different LULC is determined by zonal GIS and regression analysis. The results illustrate that the emissivity lies in the range of 0.860-0.992 and 0.855-0.992 in 1998 and 2002, respectively. The maximum value of LSE equal to similar to 0.99 was observed over the dense vegetation, while the minimum LSE value equal to similar to 0.880 was found over the sand dune. LST and NDVI analysis exhibits a strong inverse correlation except over water bodies. The strongest coefficient correlation was found over wetland (-0.76 and R-2=0.78).
机译:地表温度(LST)是在气候,水文,养蜂和变化检测研究中建模所需的输入数据。在当前的研究中,遥感热红外数据被用于评估伊朗南部卡尔凯次流域的LST。这项研究的目的是研究区域内1998年10月和2002年10月使用Landsat 5 TM和Landsat 7 ETM +提取LST和地表发射率(LSE)以及植被丰度之间的关系。土地利用/土地覆盖(LULC)图是通过使用最大似然分类器得出的。在NDVI阈值方法的基础上,研究并提取了LSE的多样性,并使用Plank方程推导了研究区域的LST。 LST和不同LULC之间的关系通过区域GIS和回归分析确定。结果表明,在1998年和2002年发射率分别在0.860-0.992和0.855-0.992范围内。在茂密的植被上观察到LSE的最大值等于0.99,而在沙丘上发现的LSE的最小值等于0.880。 LST和NDVI分析显示出很强的反相关性,除了在水体上。在湿地上发现最强的系数相关性(-0.76和R-2 = 0.78)。

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