20 citations as recorded by crossref.

1. Refining the Laurentide Ice Sheet at Marine Isotope Stage 3: A data-based approach combining glacial isostatic simulations with a dynamic ice model T. Pico et al. https://doi.org/10.1016/j.quascirev.2018.07.023
2. What drives LGM precipitation over the western Mediterranean? A study focused on the Iberian Peninsula and northern Morocco P. Beghin et al. https://doi.org/10.1007/s00382-015-2720-0
3. The North American Cordillera—An Impediment to Growing the Continent-Wide Laurentide Ice Sheet M. Löfverström et al. https://doi.org/10.1175/JCLI-D-15-0044.1
4. Inverting Glacial Isostatic Adjustment signal using Bayesian framework and two linearly relaxing rheologies L. Caron et al. https://doi.org/10.1093/gji/ggx083
5. The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle J. Liakka et al. https://doi.org/10.5194/cp-12-1225-2016
6. The role of regional feedbacks in glacial inception on Baffin Island: the interaction of ice flow and meteorology L. Birch et al. https://doi.org/10.5194/cp-14-1441-2018
7. The impact of glacier retreat from the Ross Sea on local climate: Characterization of mineral dust in the Taylor Dome ice core, East Antarctica S. Aarons et al. https://doi.org/10.1016/j.epsl.2016.03.035
8. Orbital control of western North America atmospheric circulation and climate over two glacial cycles M. Lachniet et al. https://doi.org/10.1038/ncomms4805
9. Adding a dynamical cryosphere to iLOVECLIM (version 1.0): coupling with the GRISLI ice-sheet model D. Roche et al. https://doi.org/10.5194/gmd-7-1377-2014
10. The California Current System as a transmitter of millennial scale climate change on the northeastern Pacific margin from 10 to 50 ka M. Taylor et al. https://doi.org/10.1002/2014PA002738
11. Contrasting the Penultimate Glacial Maximum and the Last Glacial Maximum (140 and 21 ka) using coupled climate–ice sheet modelling V. Patterson et al. https://doi.org/10.5194/cp-20-2191-2024
12. Evolution of the large-scale atmospheric circulation in response to changing ice sheets over the last glacial cycle M. Löfverström et al. https://doi.org/10.5194/cp-10-1453-2014
13. Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach E. Bauer & A. Ganopolski https://doi.org/10.5194/cp-13-819-2017
14. Hypersensitivity of glacial summer temperatures in Siberia P. Bakker et al. https://doi.org/10.5194/cp-16-371-2020
15. The influence of atmospheric grid resolution in a climate model-forced ice sheet simulation M. Lofverstrom & J. Liakka https://doi.org/10.5194/tc-12-1499-2018
16. Constraint on the penultimate glacial maximum Northern Hemisphere ice topography (≈140 kyrs BP) F. Colleoni et al. https://doi.org/10.1016/j.quascirev.2016.01.024
17. Modelling Greenland ice sheet inception and sustainability during the Late Pliocene C. Contoux et al. https://doi.org/10.1016/j.epsl.2015.05.018
18. How might the North American ice sheet influence the northwestern Eurasian climate? P. Beghin et al. https://doi.org/10.5194/cp-11-1467-2015
19. Last glacial inception trajectories for the Northern Hemisphere from coupled ice and climate modelling T. Bahadory et al. https://doi.org/10.5194/cp-17-397-2021
20. Relative importance of the mechanisms triggering the Eurasian ice sheet deglaciation in the GRISLI2.0 ice sheet model V. van Aalderen et al. https://doi.org/10.5194/cp-20-187-2024