利用Landsat数据估算地表温度:以印度阿格拉市为例

Kamal S. Bisht
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引用次数: 3

摘要

地表温度(LST)是气候变化研究、城市环境研究、热平衡研究、水文和农业过程研究、城市土地利用和土地覆盖研究以及气候模式用户输入的重要指标。陆地卫星数据被用于环境研究、沼气池和资源管理等许多应用。陆地表面温度是在ArcGIS的帮助下通过Landsat 8和5卫星图像估算的。采用归一化植被指数(NDVI)阈值法估算地表发射率(LSE);NDVI在其公式中是通过近红外(NIR)和红色光谱波段来计算的。Ndvi = (nir-red)/(nir-red)。热红外波段是本研究区域LSE的来源。本研究的目的是计算印度阿格拉市的地表温度和NDVI,为了完成这项任务,使用了ArcGIS光栅计算器。NDVI、LSE和LST的实证确定值具有适当的准确性,有助于实现本研究的目的。最后推导出印度阿格拉市不同土地利用方式和土地覆盖面积的温度变化。关键词:ArcGIS, Landsat卫星图像,地表发射率,地表温度,归一化植被指数,栅格计算器,Landsat 8
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of Land Surface Temperature using Landsat Data: a Case Study of Agra City, India
Land surface temperature (LST) is an important indicator for the study of climate change, urban environment, heat balance studies, hydrological and agricultural process, and urban land use and land cover as well as user input for climate models. Landsat data is utilized for the number of applications such as environment study, digester and resource management. Land surface temperate is estimated by the help of ArcGIS through Landsat 8 and 5 satellites images. The normalized difference vegetation index (NDVI) thresholds method was used for land surface emissivity (LSE) estimation; NDVI is calculated by near infrared (NIR) and red spectral bands in its formula. NDVI = (NIR-RED)/(NIR-RED). The thermal infrared band is the source of LSE in this study area. The aim of this study is to calculate the LST and NDVI of Agra city, India, and to accomplish this task, ArcGIS Raster calculator is utilized. The empirical determine value of NDVI, LSE, and LST with appropriate accuracy help to achieve the aim of this study. In the last drive out the temperature variance in different land use and land cover area of Agra city, India. Keywords: ArcGIS, Landsat satellite images, land surface emissivity, land surface temperature, normalized difference vegetation index, raster calculator, Landsat 8
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