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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◆ CHSystem()
Model of the energy content in the cryo-hydrologic system. This model can be used to include the influence of cryo-hydrologic warming on the internal energy of the ice. This model is based on @article{PhillipsRajaramSteffan2010, author = {Phillips, T. and Rajaram, H. and Steffen, K.}, doi = {10.1029/2010GL044397}, journal = {Geophy. Res. Lett.}, number = {20}, pages = {1–5}, title = {{Cryo-hydrologic warming: A potential mechanism for rapid thermal response of ice sheets}}, volume = {37}, year = {2010} } We assume that during the melt season the enthalpy in the cryo-hydrologic system is equal to the enthalpy of the ice with a fixed water fraction corresponding to the amount of water remaining in the system once all of the moving water drains out (0.5% by default). During the winter the CH system is allowed to cool. Definition at line 57 of file CHSystem.cc. References pism::energy::EnergyModel::m_ice_enthalpy, pism::array::Array::metadata(), pism::array::Array::set_name(), and pism::VariableMetadata::set_name(). |