Grounding-line migration in plan-view marine ice-sheet models: results of the ice2sea MISMIP3d intercomparison

• Published in: Journal of Glaciology
• Main Authors: Pattyn, Frank, Perichon, Laura, Durand, Gael, Favier, Lionel, Gagliardini, Olivier, Hindmarsh, Richard C. A., Zwinger, Thomas, Albrecht, Torsten, Cornford, Stephen, Docquier, David, Furst, Johannes J., Goldberg, Daniel, Gudmundsson, G. Hilmar, Humbert, Angelika, Huetten, Moritz, Huybrechts, Philippe, Jouvet, Guillaume, Kleiner, Thomas, Larour, Eric, Martin, Daniel, Morlighem, Mathieu, Payne, Anthony J., Pollard, David, Rueckamp, Martin, Rybak, Oleg, Seroussi, Helene, Thoma, Malte, Wilkens, Nina
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2013
• Subjects: HIGHER-ORDER; PART 1; FLOW; DYNAMICS; SHELF; SENSITIVITY; ANTARCTICA; STABILITY; Antarc*; Antarctica; Ice Sheet; Journal of Glaciology
• Online Access: https://hdl.handle.net/1983/cff21583-d719-4a0c-86e0-e709dcaa0106; https://research-information.bris.ac.uk/en/publications/cff21583-d719-4a0c-86e0-e709dcaa0106; https://doi.org/10.3189/2013JoG12J129

Predictions of marine ice-sheet behaviour require models able to simulate grounding-line migration. We present results of an intercomparison experiment for plan-view marine ice-sheet models. Verification is effected by comparison with approximate analytical solutions for flux across the grounding line using simplified geometrical configurations (no lateral variations, no buttressing effects from lateral drag). Perturbation experiments specifying spatial variation in basal sliding parameters permitted the evolution of curved grounding lines, generating buttressing effects. The experiments showed regions of compression and extensional flow across the grounding line, thereby invalidating the boundary layer theory. Steady-state grounding-line positions were found to be dependent on the level of physical model approximation. Resolving grounding lines requires inclusion of membrane stresses, a sufficiently small grid size (