Remote Sensing Essay 1

Introduce digital quantized value radiance values, an apparent reflectance, surface reflectance and atmospheric correction of the radiometric calibration and knowledge.

Digital quantized value DN: i.e., radiation received at the satellite to a quantized value, meaning there is no specific units.

Radiance Radiance: known emissivity, per unit area, radiant flux per unit wavelength, unit solid angle, can be converted by standard radiation into radiation of a given DN.

The apparent reflectance Reflectance: satellite reflectance, surface reflectance atmosphere, the atmosphere is not corrected, the received satellite reflectance.

Surface reflectance: Feature real reflectance, the reflectance of the apparent reflectance obtained by subtracting the atmospheric effects. Correction can be obtained from the atmosphere, the obtained value as flaash / 10000 to give the surface reflectance.

 

Moreover, the apparent reflectance spectra radiance is calculated by radiance, atmospheric correction is not performed. Formula = Pi * L * [rho] D * D / (ESUN * cos [theta])
  [rho] is the apparent reflectance or reflectance planets, L is the radiance value, d is the distance day, ESUN atmosphere average of the incident solar radiation, θ is solar zenith angle.

Additional information:

1.flaash atmospheric correction inputs must be obtained radiometric calibration radiance

2.quac atmospheric correction input may be raw DN \ reflectance \ radiance ...

3.6s atmospheric correction models subsequent supplements.

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Origin www.cnblogs.com/ljwgis/p/12057747.html