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Atmospheric compensation for surface temperature and emissivity separation

机译:用于表面温度和发射率分离的大气补偿

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摘要

A new method for atmospheric compensation of longwave infrared (LWIR) hyerspectral images is presented. The technique exploits the large amount of data in hyperspectral images to btain the most information about atmospheric and surface parameters of interest. This is doen with Canonical Correlation Analysis (CCA) by casting the problem onto a multivariate framework. The procedure accounts for the joint effects of surface and atmospheric rediation, thus addressing the complex interaction between the Earth's surface properties, thermodynamic state, and the atmosphere. After atmospheric compensation, the calculated surface readiance is used to estimate temperature and emissivity. The technique was tested with radiative transfer model simulations and airborne multispectral data. Results obtained from MODTRAN simulations and the MODerate resolution Imaging Spectrometer (MODIS) and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) (MASTER) airborne sensor show that it is feasible to retrieve land surface temperature and emissivity with 1 deg K and 0.01 accuracies, respectively.
机译:提出了一种用于长波红外(LWIR)红外光谱图像大气补偿的新方法。该技术利用高光谱图像中的大量数据来获取有关感兴趣的大气和地面参数的最多信息。通过将问题投射到多变量框架上,可以通过规范相关分析(CCA)进行处理。该程序考虑到了表面和大气再氧化的共同作用,从而解决了地球表面特性,热力学状态和大气之间的复杂相互作用。大气补偿后,将使用计算出的表面准备度来估算温度和发射率。该技术已通过辐射传输模型模拟和机载多光谱数据进行了测试。从MODTRAN模拟,适度分辨率成像光谱仪(MODIS)和先进的星载热发射与反射辐射仪(ASTER)(MASTER)机载传感器获得的结果表明,以1度K和0.01精度检索地面温度和发射率是可行的,分别。

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