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Procedures for calculation of the albedo with OLI-Landsat 8 images: Application to the Brazilian semi-arid

机译:OLI-Landsat 8影像反照率的计算程序:在巴西半干旱地区的应用

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The surface albedo plays an important role in the exchanges of energy and mass in the planetary boundary layer. Therefore, changes in albedo affect the balance of radiation and energy at the surface, which can be detected with its monitoring. Albedo determination has been performed through various sensors, but there is not yet any publication dealing with albedo calculation procedures using OLI (Operational Land Imager) - Landsat 8 images. The objective of the study is to present the procedures for computing the albedo with OLI images and map it in irrigated areas of the S?£o Gon?§alo Irrigated District, PB, Brazil. Images of the year 2013, path 215 and row 65, were selected. The data necessary for calculating the albedo were extracted from each image metadata: additive and multiplicative terms of radiance and reflectance, and sun elevation angle. There were large differences between the albedo values a€?a€?of irrigated plots, water bodies and native vegetation. The albedo obtained with OLI images provides a higher degree of differentiation of the various types of land use, due to the substantial increase in the radiometric resolution of this new sensor.
机译:表面反照率在行星边界层的能量和质量交换中起着重要作用。因此,反照率的变化会影响表面辐射和能量的平衡,这可以通过对其进行监测来检测。已经通过各种传感器执行了反照率确定,但是还没有任何出版物涉及使用OLI(Operational Land Imager)-Landsat 8图像的反照率计算程序。本研究的目的是介绍使用OLI图像计算反照率的程序,并将其映射到巴西PB S?o Gon?§alo灌溉区的灌溉区域。选择了2013年的图像(路径215和第65行)。从每个图像元数据中提取了计算反照率所需的数据:辐射率和反射率的加法和乘法项以及太阳仰角。灌溉地块,水体和原生植被的反照率值之间存在很大差异。由于这种新型传感器的辐射分辨率大大提高,因此使用OLI图像获得的反照率提供了各种土地利用类型的更高区分度。

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