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大气订正
相关语句
  atmospheric correction
    ATMOSPHERIC CORRECTION FOR AMTIS SINGLE-CHANNEL MULTI-ANGULAR THERMAL-INFRARED IMAGERY
    AMTIS单通道多角度热红外图像的大气订正
短句来源
    The atmospheric correction result is validated by using synchronous experiment data,and the precision of brightness temperature is less than 1.2 K,which is acceptable when the atmosphere profiles is not available.
    通过将大气订正后的亮度温度与地面实测点亮度温度比较,两者相差约1.2K,这对于无大气廓线情况下单通道热红外图像的大气订正来说,结果是可以接受的.
短句来源
  atmospheric correction
    ATMOSPHERIC CORRECTION FOR AMTIS SINGLE-CHANNEL MULTI-ANGULAR THERMAL-INFRARED IMAGERY
    AMTIS单通道多角度热红外图像的大气订正
短句来源
    The atmospheric correction result is validated by using synchronous experiment data,and the precision of brightness temperature is less than 1.2 K,which is acceptable when the atmosphere profiles is not available.
    通过将大气订正后的亮度温度与地面实测点亮度温度比较,两者相差约1.2K,这对于无大气廓线情况下单通道热红外图像的大气订正来说,结果是可以接受的.
短句来源
  atmospheric correction
    ATMOSPHERIC CORRECTION FOR AMTIS SINGLE-CHANNEL MULTI-ANGULAR THERMAL-INFRARED IMAGERY
    AMTIS单通道多角度热红外图像的大气订正
短句来源
    The atmospheric correction result is validated by using synchronous experiment data,and the precision of brightness temperature is less than 1.2 K,which is acceptable when the atmosphere profiles is not available.
    通过将大气订正后的亮度温度与地面实测点亮度温度比较,两者相差约1.2K,这对于无大气廓线情况下单通道热红外图像的大气订正来说,结果是可以接受的.
短句来源
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  atmospheric correction
An efficient approach to the atmospheric correction of satellite information is developed.
      
Substantial interannual variability in the errors of the standard atmospheric correction algorithm resulting in an underestimation of the shortwave radiances were revealed.
      
For the turbid atmosphere with strong-ly absorbing aerosol, the Homogeneous Model and the Two-layer Model are not suitable for atmospheric correction application.
      
Atmospheric effect makes NDVI smaller, and atmospheric correction has the tendency of increasing NDVI values.
      
Finally, a simplified model function of the atmospheric contribution is derived, as a first step to develop an atmospheric correction method for passive polarimetry of the wind over sea.
      
更多          
  atmospheric correction
An efficient approach to the atmospheric correction of satellite information is developed.
      
Substantial interannual variability in the errors of the standard atmospheric correction algorithm resulting in an underestimation of the shortwave radiances were revealed.
      
For the turbid atmosphere with strong-ly absorbing aerosol, the Homogeneous Model and the Two-layer Model are not suitable for atmospheric correction application.
      
Atmospheric effect makes NDVI smaller, and atmospheric correction has the tendency of increasing NDVI values.
      
Finally, a simplified model function of the atmospheric contribution is derived, as a first step to develop an atmospheric correction method for passive polarimetry of the wind over sea.
      
更多          
  atmospheric correction
An efficient approach to the atmospheric correction of satellite information is developed.
      
Substantial interannual variability in the errors of the standard atmospheric correction algorithm resulting in an underestimation of the shortwave radiances were revealed.
      
For the turbid atmosphere with strong-ly absorbing aerosol, the Homogeneous Model and the Two-layer Model are not suitable for atmospheric correction application.
      
Atmospheric effect makes NDVI smaller, and atmospheric correction has the tendency of increasing NDVI values.
      
Finally, a simplified model function of the atmospheric contribution is derived, as a first step to develop an atmospheric correction method for passive polarimetry of the wind over sea.
      
更多          


The atmospheric correction algorithm for the TIR band of AMTIS(airborne multi-angle TIR/VNIR imaging System)was presented.This algorithm is suitable for the case in which no atmospheric profile is available.Three parameters are considered in this algorithm: the atmospheric equivalent temperature is determined from the image itself by using a "minimal standard deviation" method or the local air temperature near the surface;the transmittance is calculated from the water vapor content of the column,which can be...

The atmospheric correction algorithm for the TIR band of AMTIS(airborne multi-angle TIR/VNIR imaging System)was presented.This algorithm is suitable for the case in which no atmospheric profile is available.Three parameters are considered in this algorithm: the atmospheric equivalent temperature is determined from the image itself by using a "minimal standard deviation" method or the local air temperature near the surface;the transmittance is calculated from the water vapor content of the column,which can be determined from the surface absolute humidity or from sunphotometer;the emissivity of the pixel is determined from NDVI.The atmospheric correction result is validated by using synchronous experiment data,and the precision of brightness temperature is less than 1.2 K,which is acceptable when the atmosphere profiles is not available.

给出了在假定无大气廓线情况下,AMTIS单通道多角度热红外图像的大气订正算法.算法需要三个参数:其中大气等效温度,用“最小标准差法”从图像自身来估算;大气透过率通过地表的绝对湿度或者太阳辐射计得到的大气水汽含量参数来估算;像元的辐射率比由AMTIS得到的NDVI计算.通过将大气订正后的亮度温度与地面实测点亮度温度比较,两者相差约1.2K,这对于无大气廓线情况下单通道热红外图像的大气订正来说,结果是可以接受的.

 
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