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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◆ update_flux_through_top_surface()
Computes the heat flux from the bedrock thermal layer upward into the ice/bedrock interface: \[G_0 = -k_b \frac{\partial T_b}{\partial z}\big|_{z=0}.\] Uses the second-order finite difference expression \[\frac{\partial T_b}{\partial z}\big|_{z=0} \approx \frac{3 T_b(0) - 4 T_b(-\Delta z) + T_b(-2\Delta z)}{2 \Delta z}\] where \(\Delta z\) is the equal spacing in the bedrock. The above expression only makes sense when Definition at line 210 of file BTU_Full.cc. References pism::array::Array2D< T >::copy_from(), m_bootstrapping_needed, pism::energy::BedThermalUnit::m_bottom_surface_flux, pism::Component::m_grid, m_k, m_Mbz, m_temp, pism::energy::BedThermalUnit::m_top_surface_flux, and pism::energy::BedThermalUnit::vertical_spacing(). Referenced by init_impl(), and update_impl(). |