quantity used in atmospheric physics and physical oceanography : for a monochromatic component of wavelength λ of the radiation of a collimated beam propagating along the given length from the point x1 to the point x2 on its path through a homogeneous or non-homogeneous diffusing medium, the spectral optical thickness δ(λ) of the medium between x1 and x2 is defined by the formula
where μ(x,λ) is the spectral linear attenuation coefficient at the location of dx
unit : 1
NOTE 1 – The spectral radiant flux Φe, λ (x1, λ) of the beam at the point x1 is reduced to the value of Φe, λ (x2, λ) at the point x2 according to the formula
so that
NOTE 2 – For a homogeneous non-diffusing layer, δ(λ) is the Napierian spectral internal transmittance density.
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