List of publications using PISM

Photo: NRKbeta / Unsplash

The list below is generated by processing submitted.bib.


  1. M. Depolli, M. Žebre, U. Stepišnik, and G. Kosec. Simulation of a former ice field with PISM – Snežnik study case. EGUsphere, 2024:1–30, 2024. doi:10.5194/egusphere-2024-544.
  2. J. Feldmann, A. Levermann, and R. Winkelmann. Hysteresis of idealized, instability-prone outlet glaciers under variation of pinning-point buttressing. EGUsphere, 2024:1–23, 2024. doi:10.5194/egusphere-2024-457.
  3. Ward van Pelt and Thomas Frank. A new glacier thickness and bed map for Svalbard. EGUsphere, May 2024. doi:10.5194/egusphere-2024-1525.


  1. T. Albrecht, M. Bagge, and V. Klemann. Feedback mechanisms controlling Antarctic glacial cycle dynamics simulated with a coupled ice sheet–solid Earth model. EGUsphere, 2023:1–31, 2023. doi:10.5194/egusphere-2023-2990.
  2. David Chandler, Petra Langebroek, Ronja Reese, Torsten Albrecht, Julius Garbe, and Ricarda Winkelmann. Antarctic Ice Sheet tipping in the last 800 kyr warns of future ice loss. research square preprint, 2023. doi:10.21203/
  3. A. K. Klose, V. Coulon, F. Pattyn, and R. Winkelmann. The long-term sea-level commitment from Antarctica. The Cryosphere Discussions, 2023:1–37, 2023. URL:, doi:10.5194/tc-2023-156.
  4. Moritz Kreuzer, Torsten Albrecht, Lena Nicola, Ronja Reese, and Ricarda Winkelmann. Oceanic gateways in Antarctica – Impact of relative sea-level change on sub-shelf melt. EGUsphere, 2023:1–26, 2023. doi:10.5194/egusphere-2023-2737.
  5. L. Nicola, R. Reese, M. Kreuzer, T. Albrecht, and R. Winkelmann. Oceanic gateways to Antarctic grounding lines – Impact of critical access depths on sub-shelf melt. EGUsphere, 2023:1–30, 2023. doi:10.5194/egusphere-2023-2583.
  6. C. Wirths, J. Sutter, and T. Stocker. The influence of present-day regional surface mass balance uncertainties on the future evolution of the Antarctic Ice Sheet. EGUsphere, 2023:1–39, 2023. URL:, doi:10.5194/egusphere-2023-2233.


  1. C. Yue, L. S. Schmidt, L. Zhao, M. Wolovick, and J. C. Moore. Insensitivity of mass loss of Icelandic Vatnajökull ice cap to solar geoengineering. The Cryosphere Discussions, 2021:1–20, 2021. doi:10.5194/tc-2021-318.
  2. M. Zeitz, R. Winkelmann, and A. Levermann. Implications of flow law uncertainty for flow-driven ice-loss in greenland under idealized warming pathways. The Cryosphere Discussions, 2021. URL:


  1. P. Gierz, L. Ackermann, C. B. Rodehacke, U. Krebs-Kanzow, C. Stepanek, D. Barbi, and G. Lohmann. Simulating interactive ice sheets in the multi-resolution awi-esm 1.2: a case study using scope 1.0. Geoscientific Model Development Discussions, 2020:1–32, 2020. doi:10.5194/gmd-2020-159.
  2. Z. Zhang, Q. Yan, R. Zhang, F. Colleoni, G. Ramstein, G. Dai, M. Jakobsson, M. O’Regan, S. Liess, D.-D. Rousseau, N. Wu, E. J. Farmer, C. Contoux, C. Guo, N. Tan, and Z. Guo. Rapid waxing and waning of beringian ice sheet reconcile glacial climate records from around north pacific. Climate of the Past Discussions, 2020:1–25, 2020. doi:10.5194/cp-2020-38.


  1. A. Winter, T. Kleiner, D. Steinhage, T. Creyts, and O. Eisen. Deducing large-scale age distribution and paleoaccumulation rates from radiostratigraphy in east antarctica. 2018. URL:


  1. M. A. Martin, A. Levermann, and R. Winkelmann. Comparing ice discharge through west antarctic gateways: weddell vs. amundsen sea warming. The Cryosphere Discussions, 9(2):1705–1733, 2015. doi:10.5194/tcd-9-1705-2015.


  1. R. Winkelmann, A. Levermann, K. Frieler, and M. A. Martin. Uncertainty in future solid ice discharge from antarctica. The Cryosphere Discussions, 6(1):673–714, 2012. doi:10.5194/tcd-6-673-2012.


  1. Ed Bueler, Constantine Khroulev, Andy Aschwanden, Ian Joughin, and Ben E. Smith. Modeled and observed fast flow in the Greenland ice sheet. 2009. URL:

Latest news

MARUM Bremen: open postdoc in ice-sheet modeling

MARUM - Center for Marine Environmental Sciences at the University of Bremen is offering a position for one postdoctoral researcher in ice-sheet modeling, in the project “PalMod III-From the Last Interglacial to the Anthropocene”.

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