B. Finite difference equations of the model   d. Radiation up previous next
B.d.i. Infrared radiation of atmospheric CO2

In the radiateve transfer equation of CO2 described in section A.d.i, the infrared radiative flux (A.23), (A.24), and the Plank function (A.26) are discretized as follows.

 
    (B.44)
(B.45)
(B.46)
(B.47)

The averaged transmission function, the equivalent width, and the effective path length are discretized as follows.





A numerical simulation of thermal convection in the Martian lower atmosphere.
Odaka, Nakajima, Ishiwatari, Hayashi,   Nagare Multimedia 2001
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