17 citations as recorded by crossref.

1. Impact of Dust on Climate and AMOC During the Last Glacial Maximum Simulated by CESM1.2 M. Zhang et al. 10.1029/2021GL096672
2. Small Impact of Stratospheric Dynamics and Chemistry on the Surface Temperature of the Last Glacial Maximum in CESM2(WACCM6ma) J. Zhu et al. 10.1029/2022GL099875
3. Large-ensemble simulations of the North American and Greenland ice sheets at the Last Glacial Maximum with a coupled atmospheric general circulation–ice sheet model S. Sherriff-Tadano et al. 10.5194/cp-20-1489-2024
4. Impact-induced initiation of Snowball Earth: A model study M. Fu et al. 10.1126/sciadv.adk5489
5. The Glacier‐Climate Interaction Over the Tibetan Plateau and Its Surroundings During the Last Glacial Maximum Q. Wei et al. 10.1029/2023GL103538
6. Last Glacial Maximum pattern effects reduce climate sensitivity estimates V. Cooper et al. 10.1126/sciadv.adk9461
7. Sea ice feedbacks cause more greenhouse cooling than greenhouse warming at high northern latitudes on multi-century timescales J. Kay et al. 10.1088/2752-5295/ad8026
8. LGM Paleoclimate Constraints Inform Cloud Parameterizations and Equilibrium Climate Sensitivity in CESM2 J. Zhu et al. 10.1029/2021MS002776
9. Does Disabling Cloud Radiative Feedbacks Change Spatial Patterns of Surface Greenhouse Warming and Cooling? J. Chalmers et al. 10.1175/JCLI-D-21-0391.1
10. Asymmetric Warming/Cooling Response to CO2 Increase/Decrease Mainly Due To Non‐Logarithmic Forcing, Not Feedbacks I. Mitevski et al. 10.1029/2021GL097133
11. Objectively combining climate sensitivity evidence N. Lewis 10.1007/s00382-022-06468-x
12. Global and Regional Climate Feedbacks in Response to Uniform Warming and Cooling M. Ringer et al. 10.1029/2023JD038861
13. Northern Hemisphere vegetation change drives a Holocene thermal maximum A. Thompson et al. 10.1126/sciadv.abj6535
14. Simulating surface warming in Earth's three polar regions during the Middle Miocene Climatic Optimum using isotopic and non-isotopic versions of the Community Earth System Model Y. Sun et al. 10.1016/j.palaeo.2024.112156
15. Causes of the weak emergent constraint on climate sensitivity at the Last Glacial Maximum M. Renoult et al. 10.5194/cp-19-323-2023
16. network-based constraint to evaluate climate sensitivity L. Ricard et al. 10.1038/s41467-024-50813-z
17. Assessment of Equilibrium Climate Sensitivity of the Community Earth System Model Version 2 Through Simulation of the Last Glacial Maximum J. Zhu et al. 10.1029/2020GL091220