PISM, A Parallel Ice Sheet Model
stable v2.1.1 committed by Constantine Khrulev on 2024-12-04 13:36:58 -0900
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◆ assemble_R()
Assemble the R array. The R value switches at the CTS. In a simple abstract diffusion \[ \frac{\partial u}{\partial t} = D \frac{\partial^2 u}{\partial z^2}, \] with time steps \(\Delta t\) and spatial steps \(\Delta z\) we define \[ R = \frac{D \Delta t}{\Delta z^2}. \] This is used in an implicit method to write each line in the linear system, for example [MortonMayers]: \[ -R U_{j-1}^{n+1} + (1+2R) U_j^{n+1} - R U_{j+1}^{n+1} = U_j^n. \] In the case of conservation of energy [AschwandenBuelerKhroulevBlatter], \[ u=E \qquad \text{ and } \qquad D = \frac{K}{\rho} \qquad \text{ and } \qquad K = \frac{k}{c}. \] Thus \[ R = \frac{k \Delta t}{\rho c \Delta z^2}. \] Definition at line 393 of file enthSystem.cc. References pism::k, k_from_T(), pism::columnSystemCtx::m_dz, m_EC, m_Enth, m_Enth_s, m_ice_k, m_ice_thickness, m_k_depends_on_T, pism::columnSystemCtx::m_ks, m_R, m_R_cold, m_R_factor, and m_R_temp. Referenced by init(). |