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Illumination Dependent Aerosol Optical Properties n Volume scattering function n Path function n Path radiance n Atmospheric modulation transfer function
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gainloss Radiation Transfer Equation
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When N r has some special value, N q, such that b ext N q =, then dN q /dr = 0. N q is independent of r and is commonly referred to as the equilibrium radiance. Equilibrium Radiance
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If N q is constant, the previous equation can be integrated to yield where Radiance Difference
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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
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If T is approximately zero, then N q = =N s (sky radiance) and: Path Radiance Approximation
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In general:
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.. Radiance Difference and Real World
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Apparent and Inherent Contrast Define: Apparent Contrast: Inherent Contrast:
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Radiance Difference Transmittance
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Contrast Transmittance
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If background is sky then: and
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If background is sky, N s : Estimating Extinction and, which yields
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The distance at which C r approaches a threshold contrast of between -0.02 or -0.05 defines the visual range, V r. If C o = 1 (black object) and -0.02 is taken to be a threshold contrast, then the previous equation becomes The Visual Range Concept
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Visibility Metrics n Apparent contrast: C r = C o e -b ext r n Visual Range: vr = 3.912/ b ext n decView: dv = 10 ln(b ext /.01)
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Contrast Sensitivity Surface (back)
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Contrast Sensitivity Surface (forward)
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Forward Scattering
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Back Scattering
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Optics of Visibility
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La Sals –Forward Scattering
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La Sals – Backward Scattering
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La Sals -- 30km
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Mt Trumbull -- 130km
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North Rim of Grand Canyon Through Smoke Plume
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Easterly View of Grand Canyon from Desert View Watch Tower
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Westerly View from Desert View Watch Tower
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Clouds Evaporate Leaving Sulfate Haze
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Clouds Evaporated Leaving Sulfate Haze
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Sulfate Haze Trapped Below Rim
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Next Day After Haze is Blown Out
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Path Radiance Absent Because of Clouds
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Nitrogen Dioxide Haze
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Nitrogen Dioxide Plume
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Illumination Effects
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