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Explore the intricate details of radiance and visibility in the atmosphere, including the equilibrium radiance, path radiance, and contrast sensitivity. Learn how aerosol optical properties affect visibility metrics and illumination effects.
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Illumination Dependent Aerosol Optical Properties • Volume scattering function • Path function • Path radiance • Atmospheric modulation transfer function
Radiation Transfer Equation loss gain
Equilibrium Radiance When Nr has some special value, Nq, such that bextNq= , then dNq/dr = 0. Nq is independent of r and is commonly referred to as the equilibrium radiance.
Radiance Difference If Nq is constant, the previous equation can be integrated to yield where
Path Radiance Rearranging yields The second term is the path radiance (airlight), , which results from scattering processes throughout the sight path. The parameter is the sky radiance
Path Radiance Approximation If T is approximately zero, then Nq= =Ns (sky radiance) and:
Apparent and Inherent Contrast Define: Apparent Contrast: Inherent Contrast:
Estimating Extinction If background is sky, Ns: and, which yields
The Visual Range Concept The distance at which Cr approaches a threshold contrast of between -0.02 or -0.05 defines the visual range, Vr. If Co= 1 (black object) and -0.02 is taken to be a threshold contrast, then the previous equation becomes
Visibility Metrics • Apparent contrast: Cr = Coe-bextr • Visual Range: vr = 3.912/ bext • decView: dv = 10 ln(bext/.01)
Mt Trumbull -- 130km Mt Trumbull -- 130km