B. Finite difference equations of the model a. Atmospheric model
B.a.iv. Basic state equations
The basic state pressure () and density ()
are calculated by the hydrostatic equation (A.6) and the equation of state
(A.7) given the basic state
temperature
(B.30)
(B.31)
are calculated by using as
follows.
(B.32)
(B.33)
A numerical simulation of thermal convection in the Martian lower
atmosphere.
Odaka, Nakajima, Ishiwatari, Hayashi,
Nagare Multimedia 2001