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Land surface temperature retrieval from LANDSAT TM 5

机译:从LANDSAT TM 5检索地表温度

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The land surface temperature (LST) from thermal infrared data supplied by band 6 of the Thematic Mapper (TM) sensor onboard the Landsat 5 satellite are compared. The first of them lies on the estimation of the land surface temperature from the radiative transfer equation using in situ radiosounding data. The others two are the mono-window algorithm developed by Qin et al. [International Journal of Remote Sensing 22 (2001) 3719] and the single-channel algorithm developed by Jimenez-Munoz and Sobrino [Journal of Geophysical Research 108 (200.3)]. The land surface emissivity (LSE) values needed in order to apply these methods have been estimated from a methodology that uses the visible and near infrared bands. Finally, we present a comparison between the LST measured in situ and the retrieved by the algorithms over an agricultural region of Spain (La Plana de Requena-Utiel). The results show a root mean square deviation (rmsd) of 0.009 for emissivity and lower than 1 K for land surface temperature when the Jimenez-Munoz algorithm is used.
机译:比较了由Landsat 5卫星上的Thematic Mapper(TM)传感器的波段6提供的红外热数据得出的地面温度(LST)。首先是利用原位无线电探测数据根据辐射传递方程估算陆地表面温度。另外两个是Qin等人开发的单窗口算法。 [国际遥感杂志22(2001)3719]和Jimenez-Munoz和Sobrino开发的单通道算法[地球物理研究杂志108(200.3)]。应用这些方法所需的地表发射率(LSE)值已通过使用可见光和近红外波段的方法进行了估算。最后,我们提出了在西班牙农业地区(La Plana de Requena-Utiel)现场测量的LST与通过算法检索的LST之间的比较。结果表明,使用Jimenez-Munoz算法时,发射率的均方根偏差(rmsd)为0.009,而地表温度的均方根偏差小于1K。

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