 
 
 
 
 
   
 : 2 Atmospheric model
 : Two dimensional anelastic model
 : 目次
The outline of finite difference method adapted for this model
   is as follows.
- Space differencing
- 
    The finite difference form of governing equations of the model are
       considered on the Lorenz type staggered grid. 
    The space differencing is evaluated by the forth order centered
       scheme for scalar advection terms and the continuity equation,
       and the second order centered scheme for others.
    The numerical diffusion is introduced to the equation of motion,
       turbulent kinetic energy equation, and advection diffusion
       equation of dust so that the 2-grid noise associated with
       central finite differencing can be suppressed.  
    The numerical diffusion in equation of motion is proportional to
       the squared wind shear and that in turbulent kinetic energy
       equation, and advection diffusion equation of dust is
       proportional to the third power of Laplace operator.
The vertical integral in calculating CO infrared radiative flux is evaluated by the trapezoidal rule. infrared radiative flux is evaluated by the trapezoidal rule.
 
 
- Time differencing
- 
    The time integration is performed by the leap-frog scheme for
        advection and buoyancy terms and the forward scheme for
        turbulent diffusion and forcing terms. 
    The forward scheme is also adapted once per 20 steps for
        advection and buoyancy terms to stabilized numerical solution.
    The radiative flux associated with dust is given by iteration
        method of the matrix equation, where the number of iteration
        is 4.  
    The time integration of 1D thermal conduction equation of grand
        surface is performed by the Crank-Nicolson scheme.
 
In the following sections, the subscripts  show horizontal and vertical grid point, and the superscripts
   show horizontal and vertical grid point, and the superscripts 
    show time step. 
The number of vertical grid level is
 show time step. 
The number of vertical grid level is  .
The scalar and basic state variables are evaluated on the grid point
   and the other variables are evaluated on the half grid point.
.
The scalar and basic state variables are evaluated on the grid point
   and the other variables are evaluated on the half grid point.
 and
 and  are the
   horizontal and vertical grid intervals, and
 are the
   horizontal and vertical grid intervals, and  is
   the time interval.
 is
   the time interval.
 
 
 
 
 
   
 : 2 Atmospheric model
 : Two dimensional anelastic model
 : 目次
Odaka Masatsugu
平成19年4月26日