Visibility in Bad Weather from a Single Image Robby T. Tan Imperial College London CVPR. 2008
Outline Introduce Model Algorithm Result Future work and conclusion
x is the 2D spatial location. L∞ is the atmospheric light. ρ is the reflectance of an object in the image. β is the atmospheric attenuation coefficient. d is the distance between an object in the image and the observer.
Define image chromaticity Assume distant (d = ∞) , since e^-βd = 0 , light chromaticity Assume no effect of scattering particles e^-βd = 1 , object chromaticity
By utilizing the light chromaticity (α) we can transform the color of the atmospheric light of the input image into white color Color vectors:
Maximizing contrast
Airlight Smoothness Constraint Data term Smooth term
Algorithm
Future work and conclusion 失真情形