Marine ice-sheet dynamics. Part 1. The case of rapid sliding

By Christian Schoof. Journal of Fluid Mechanics, 2007

256 citations recorded by the source corpus.

Subfields: Atmospheric Science, Pulmonary and Respiratory Medicine

View Paper: https://www.semanticscholar.org/paper/a2d87acedd3f15e96ebe75eb72cb918bbd5b740a

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Citations in the corpus

Thin-Film Flows with Wall Slip: An Asymptotic Analysis of Higher Order Glacier Flow Models (2010, methodology): “Free boundary methods have been suggested as an approach to tracking regions of slow and fast sliding within an ice sheet, so that the relevant thin film model can be applied in each region (15, 16, 17).”
Deglaciation of the Eurasian ice sheet complex (2017, methodology): “The model is applied to a 10 km finite-difference mesh with the inclusion of grounding-line dynamics based on the analytical boundary-treatment of Schoof (2007) and adapted in 2D by Pollard and DeConto (2007), which defines the ice flux at the grounding line as a function of ice thickness linearly…”
Continental scale, high order, high spatial resolution, ice sheet modeling using the Ice Sheet System Model (ISSM) (2012, background): “[28] Grounding line migration is a key control on ice flow dynamics [Schoof, 2007a, 2007b; Nowicki, 2007; Durand et al., 2009b, 2009a], which is important to capture in order for transient ice flow models to be realistic.”
Grounding line movement and ice shelf buttressing in marine ice sheets (2009, methodology): “Depending on various factors, this zone can have a length scale ranging from onetomany icethicknesses [Chugunov andWilchinsky, 1996; Pattyn et al., 2006; Schoof, 2007a; Nowicki and Wingham, 2007] and its importance to the large-scale system dynamics of marine ice sheets has been debated.”
The Potsdam Parallel Ice Sheet Model (PISM-PIK) – Part 1: Model description (2010, methodology): “The results of these simulations allow a comparison with the semi-analytical solution by Schoof(2007a), and give insight into the quality of the numerical treatment of grounding line motion.”
Marine ice-sheet profiles and stability under Coulomb basal conditions (2015, methodology): “(5b) ensures continuity with the stresses in the ice shelf (Schoof, 2007b).”
The stability of grounding lines on retrograde slopes (2012, methodology): “These models produced in turn steady-state solutions that were in a close agreement with a semi-analytical solution (Schoof, 2007a) of this problem.”
Marine ice sheet dynamics: Hysteresis and neutral equilibrium (2009, methodology): “[47] In agreement with the BL theory results [Schoof, 2007a], a marine ice sheet is unstable on an upsloping bed, confirming once again the marine ice sheet instability hypothesis proposed by Weertman [1974].”
Antarctic sub-shelf melt rates via PICO (2017, background): “The ice grounded below sea level in its marine basins is susceptible to ocean forcing and might respond nonlinearly to changes in ocean boundary conditions (Mercer, 1978; Schoof, 2007).”
Ice sheet grounding line dynamics: Steady states, stability, and hysteresis (2007, methodology): “In our paper, the size of the transition zone is determined by the model parameters C and � and the geometry of the ice sheet bed, see Schoof [2007] and equation (A9) in Appendix A below.”