The Impact Of A Pressurized Regional Sea Or Global Ocean On Stresses On Enceladus: Numerical Models

Comsol Multiphysics models solving the stress field in Enceladus' ice shell when a regional sea of global ocean is pressurized. Model parameters are included as part of the file name according to the template EnceladusT<em>t</em>D<em>d</em><em>Label</em>.mph with <em>t</em> is the ice shell thickness <em>d</em> is the thickness of the south polar sea or indentation <em>Label </em>indicates model configuration <em>Fixed</em>: The base of the ice shell (outside the south polar sea) is in contact with the core with a no-slip boundary condition <em>Roller</em>: The base of the ice shell (outside the south polar sea) is in contact with the core with a free-slip boundary condition <em>Ocean</em>: The base of the ice shell is floating with a constant pressure condition; there is a single indentation at the South pole <em>North</em>: The base of the ice shell is floating with a constant pressure condition; there are indentations at both poles, with the north pole indentation having half the thickness of the South pole indentation There are two solved datasets in each model. The first uses a default value of the ocean angle (40°). The second results from a parameter sweep in which the sea angle varies systematically in increments of 2°.