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Received Mar 9, 2017; Revised Jun 7, 2017; Accepted Jun 21, 2017
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1. Introduction
Land Surface Temperature and Emissivity (LST and LSE) are two key parameters in quantitative remote sensing and have been widely used in many fields such as meteorological and climate models, lithological mapping, and resources exploration [1, 2].
Over recent decades, great effort has been made to retrieve the LST and LSEs from multispectral thermal infrared (TIR) data, and some typical algorithms have been successfully used to determine the LST and LSEs from space measurements [3]. For example, the Split Window algorithm and Day/Night algorithm are used for the Moderate Resolution Imaging Spectroradiometer (MODIS), and the Temperature and Emissivity Separation (TES) algorithm is used for the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) [4–7]. According to the current multispectral land products, the general accuracy of the LST can be approximately 1 K [7–10]. However, in most algorithms, some empirical constraints on LSE are also needed to determine the LST, such as prior knowledge of the LSE in the Split Window (SW) algorithm and the assumption of a constant LSE during night and day in the Day/Night (D/N) algorithm [4, 5]. Unlike the LST product, the current LSE products are usually determined according to a classification map, which makes the accuracy of the LSE product highly dependent on prior knowledge [8, 10]....