A full Stokes subgrid model for simulation of grounding line migration in ice sheets using Elmer/ICE(v8.3)

Gong Cheng, Per Lötstedt, L. von Sydow
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Abstract

Abstract. The full Stokes equations are solved by a finite element method for simulation of large ice sheets and glaciers. The simulation is particularly sensitive to the discretization of the grounding line which separates the ice resting on the bedrock and the ice floating on water and is moving in time. The boundary conditions at the ice base are enforced by Nitsche's method and a subgrid treatment of the elements in the discretization close to the grounding line. Simulations with the method in two dimensions for an advancing and a retreating grounding line illustrate the performance of the method. It is implemented in the two dimensional version of the open source code Elmer/ICE.
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使用Elmer/ ice (v8.3)模拟冰盖接地线迁移的全Stokes子网格模型
摘要用有限元法求解了大冰原和冰川的全Stokes方程。模拟对基岩上的冰与水面上随时间移动的冰之间的接地线的离散化特别敏感。冰基的边界条件由Nitsche方法和靠近接地线的离散化单元的子网格处理来实现。用该方法对前进接地线和后退接地线进行了二维仿真,验证了该方法的有效性。它是在开源代码Elmer/ICE的二维版本中实现的。
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