“…As such, glaciology synthesizes elements from a multitude of scientific disciplines including continuum mechanics, fluid mechanics, hydraulics, chemistry, and meteorology. Bueler et al (2005) introduce analytical solutions for the SIA PDE, a commonly used model for the dynamics of glaciers (Fowler and Larson, 1978;Hutter, 1982;Flowers et al, 2005;Cuffey and Paterson, 2010;van der Veen, 2013;Brinkerhoff et al, 2016;Guan et al, 2016;Gopalan et al, 2018). Based on the principle of conservation of mass, the SIA dictates that glacier flow is in the direction of the (negative) gradient of the glacier surface and is due to gravity and basal sliding (also referred to as friction or drag if in the direction of the positive gradient).…”