Articles | Volume 91
https://doi.org/10.5194/polf-91-105-2023
https://doi.org/10.5194/polf-91-105-2023
Polar Fox
 | 
22 Dec 2023
Polar Fox |  | 22 Dec 2023

Polarfuchs (Kolumne): Die Antarktis im Computer – wie funktionieren Computermodelle?

Lena Nicola

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Cited articles

Albrecht, T., Winkelmann, R., and Levermann, A.: Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 2: Parameter ensemble analysis, The Cryosphere, 14, 633–656, https://doi.org/10.5194/tc-14-633-2020, 2020. a
Benn, D. and Evans, D. J.: Glaciers and glaciation, Routledge, 2nd Edn., ISBN 978-0-340-90579-1, 2013. a
Bueler, E. and Brown, J.: Shallow shelf approximation as a “sliding law” in a thermomechanically coupled ice sheet model, J. Geophys. Res.-Earth, 114, F03008, https://doi.org/10.1029/2008JF001179, 2009. a
Hutter, K.: The Application of the Shallow-Ice Approximation, Theoretical Glaciology: Material Science of Ice and the Mechanics of Glaciers and Ice Sheets, 256–332, https://doi.org/10.1007/978-94-015-1167-4_5, 1983. a
Reese, R., Garbe, J., Hill, E. A., Urruty, B., Naughten, K. A., Gagliardini, O., Durand, G., Gillet-Chaulet, F., Gudmundsson, G. H., Chandler, D., Langebroek, P. M., and Winkelmann, R.: The stability of present-day Antarctic grounding lines – Part 2: Onset of irreversible retreat of Amundsen Sea glaciers under current climate on centennial timescales cannot be excluded, The Cryosphere, 17, 3761–3783, https://doi.org/10.5194/tc-17-3761-2023, 2023. a
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Short summary
There are different ways to study the icy continent of Antarctica. One way to understand various processes in Antarctica or to investigate the future of the ice sheet under climate change, is to build a computer model. Several steps are needed to represent how ice flows inside a model. These include for example the derivation of the physical equations, the construction of a coordinate system and the choice of boundary conditions.
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