density_bcs
Module
Quick access
- Routines:
bc_ism_dens(),bc_lnrho_cfb_r_iso(),bc_lnrho_hds_z_iso_dens(),bc_lnrho_hdss_z_iso(),initialize_density_bcs()
Needed modules
Variables
- densitybcs/reference_state (*,*) [real,private/pointer]
- densitybcs/xbot [integer,private/parameter/optional/default=1]
- densitybcs/xtop [integer,private/parameter/optional/default=nx]
Subroutines and functions
- subroutine densitybcs/initialize_density_bcs()
- Use :
- Call to:
- subroutine densitybcs/bc_lnrho_cfb_r_iso(f, topbot)
Boundary condition for radial centrifugal balance
- This sets
partial_{r} lnrho
- such that
(partial_{r} p)/rho = cs^2 partial_{r} lnrho} = uphi**2/rad - partial_{r} Phi
where Phi is the gravitational potential
i.e. it enforces centrifugal balance at the boundary.
As it is, works only for isobaric, isothermal and cylindrical coordinates
21-aug-2006/wlad: coded
- Parameters:
f (,,*,*) [real,inout]
topbot [integer,in]
- Use :
densitymethods(getrho()),gravity(potential()),sub(div())- Call to:
- subroutine densitybcs/bc_lnrho_hdss_z_iso(f, topbot)
Smooth out density perturbations with respect to hydrostatic stratification in Fourier space.
Note: Since boundconds_x and boundconds_y are called first, this doesn’t set the corners properly. However, this is not a problem since cross derivatives of density are never needed.
05-jul-07/tobi: Adapted from bc_aa_pot3
- Parameters:
f (,,*,*) [real,inout]
topbot [integer,in]
- Use :
fourier(fourier_transform_xy_xy(),fourier_transform_other(),kx_fft(),ky_fft()),gravity(potential())- Call to:
- subroutine densitybcs/bc_lnrho_hds_z_iso_dens(f, topbot)
Boundary condition for density and entropy.
- This sets
partial_{z} lnrho
- such that
partial_{z} p = rho g_{z},
i.e. it enforces hydrostatic equlibrium at the boundary.
- Currently this is only correct if
partial_{z} lnT = 0
at the boundary.
12-Juil-2006/dintrans: coded
- subroutine densitybcs/bc_ism_dens(f, topbot, j)
30-nov-15/fred: Replaced bc_ctz and bc_cdz. Apply observed scale height locally from Reynolds 1991, Manchester & Taylor 1981 for warm ionized gas - dominant scale height above 500 parsecs. Apply constant local temperature across boundary for entropy. Motivation to prevent numerical spikes in shock fronts, which cannot be absorbed in only three ghost cells, but boundary thermodynamics still responsive to interior dynamics.
- Parameters:
f (,,*,*) [real]
topbot [integer,in]
j [integer]
- Call to: