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Generalized Split-Window Algorithm for Estimate of Land Surface Temperature from Chinese Geostationary FengYun Meteorological Satellite (FY-2C) Data

机译:利用中国对地静止风云气象卫星(FY-2C)数据估算地表温度的广义分裂窗算法

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摘要

On the basis of the radiative transfer theory, this paper addressed the estimate of Land Surface Temperature (LST) from the Chinese first operational geostationary meteorological satellite-FengYun-2C (FY-2C) data in two thermal infrared channels (IR1, 10.3-11.3 μm and IR2, 11.5-12.5 μm), using the Generalized Split-Window (GSW) algorithm proposed by Wan and Dozier (1996). The coefficients in the GSW algorithm corresponding to a series of overlapping ranging of the mean emissivity, the atmospheric Water Vapor Content (WVC), and the LST were derived using a statistical regression method from the numerical values simulated with an accurate atmospheric radiative transfer model MODTRAN 4 over a wide range of atmospheric and surface conditions. The simulation analysis showed that the LST could be estimated by the GSW algorithm with the Root Mean Square Error (RMSE) less than 1 K for the sub-ranges with the Viewing Zenith Angle (VZA) less than 30° or for the sub-rangs with VZA less than 60° and the atmospheric WVC less than 3.5 g/cm2 provided that the Land Surface Emissivities (LSEs) are known. In order to determine the range for the optimum coefficients of the GSW algorithm, the LSEs could be derived from the data in MODIS channels 31 and 32 provided by MODIS/Terra LST product MOD11B1, or be estimated either according to the land surface classification or using the method proposed by Jiang et al. (2006); and the WVC could be obtained from MODIS total precipitable water product MOD05, or be retrieved using Li et al.' method (2003). The sensitivity and error analyses in term of the uncertainty of the LSE and WVC as well as the instrumental noise were performed. In addition, in order to compare the different formulations of the split-window algorithms, several recently proposed split-window algorithms were used to estimate the LST with the same simulated FY-2C data. The result of the intercomparsion showed that most of the algorithms give comparable results.
机译:基于辐射转移理论,本文从中国第一颗对地静止气象卫星风云2C(FY-2C)数据在两个红外热通道(IR1,10.3-11.3)中提出了对地表温度(LST)的估计。 μm和IR2,11.5-12.5μm),使用Wan和Dozier(1996)提出的广义分裂窗(GSW)算法。使用统计回归方法从准确的大气辐射传输模型MODTRAN所模拟的数值中,使用统计回归方法,得出GSW算法中与平均发射率,大气水汽含量(WVC)和LST的一系列重叠范围相对应的系数4在大范围的大气和地面条件下。仿真分析表明,对于视天顶角(VZA)小于30°的子范围或子范围,可以通过GSW算法估计LST,且均方根误差(RMSE)小于1 K如果已知陆地表面发射率(LSE),则VZA小于60°,大气WVC小于3.5 g / cm 2 。为了确定GSW算法最佳系数的范围,可以从MODIS / Terra LST产品MOD11B1提供的MODIS通道31和32中的数据得出LSE,或者根据地面分类或使用Jiang等人提出的方法。 (2006); WVC可以从MODIS的总可沉淀水产品MOD05中获得,也可以使用Li等进行检索。方法(2003)。对LSE和WVC的不确定性以及仪器噪声进行了灵敏度和误差分析。此外,为了比较拆分窗口算法的不同公式,使用了几种最近提出的拆分窗口算法来估计具有相同模拟FY-2C数据的LST。相互比较的结果表明,大多数算法给出了可比的结果。

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