70 citations as recorded by crossref.

1. Empirical estimate of the signal content of Holocene temperature proxy records M. Reschke et al. 10.5194/cp-15-521-2019
2. Effects of CO2 and Ocean Mixing on Miocene and Pliocene Temperature Gradients G. Lohmann et al. 10.1029/2020PA003953
3. The Impact of Different Atmospheric CO2 Concentrations on Large Scale Miocene Temperature Signatures A. Hossain et al. 10.1029/2022PA004438
4. How changing the height of the Antarctic ice sheet affects global climate: a mid-Pliocene case study X. Huang et al. 10.5194/cp-19-731-2023
5. Flat meridional temperature gradient in the early Eocene in the subsurface rather than surface ocean S. Ho & T. Laepple 10.1038/ngeo2763
6. The initiation of Neoproterozoic "snowball" climates in CCSM3: the influence of paleocontinental configuration Y. Liu et al. 10.5194/cp-9-2555-2013
7. A suite of early Eocene (~ 55 Ma) climate model boundary conditions N. Herold et al. 10.5194/gmd-7-2077-2014
8. Transitivity of the climate–vegetation system in a warm climate U. Port & M. Claussen 10.5194/cp-11-1563-2015
9. Initiation of a Marinoan Snowball Earth in a state-of-the-art atmosphere-ocean general circulation model A. Voigt et al. 10.5194/cp-7-249-2011
10. Progress in Greenhouse Climate Modeling M. Huber 10.1017/S108933260000262X
11. The Paleocene‐Eocene Thermal Maximum: How much carbon is enough? K. Meissner et al. 10.1002/2014PA002650
12. Simulated climate variability in the region of Rapa Nui during the last millennium C. Junk & M. Claussen 10.5194/cp-7-579-2011
13. Evaluating the dominant components of warming in Pliocene climate simulations D. Hill et al. 10.5194/cp-10-79-2014
14. Simulation of the climate and ocean circulations in the Middle Miocene Climate Optimum by a coupled model FGOALS-g3 J. Wei et al. 10.1016/j.palaeo.2023.111509
15. Uncertainties in the modelled CO2 threshold for Antarctic glaciation E. Gasson et al. 10.5194/cp-10-451-2014
16. Modeling the Miocene Climatic Optimum. Part I: Land and Atmosphere* N. Herold et al. 10.1175/2011JCLI4035.1
17. Reconstructing early Eocene (∼55 Ma) paleogeographic boundary conditions for use in paleoclimate modelling Z. He et al. 10.1007/s11430-019-9366-2
18. On the climatic influence of CO2 forcing in the Pliocene L. Burton et al. 10.5194/cp-19-747-2023
19. Geobiological constraints on Earth system sensitivity to CO2 during the Cretaceous and Cenozoic D. ROYER et al. 10.1111/j.1472-4669.2012.00320.x
20. Strong effects of tropical ice-sheet coverage and thickness on the hard snowball Earth bifurcation point Y. Liu et al. 10.1007/s00382-016-3278-1
21. A model–data comparison for a multi-model ensemble of early Eocene atmosphere–ocean simulations: EoMIP D. Lunt et al. 10.5194/cp-8-1717-2012
22. Simulation of Arctic sea ice within the DeepMIP Eocene ensemble: Thresholds, seasonality and factors controlling sea ice development I. Niezgodzki et al. 10.1016/j.gloplacha.2022.103848
23. Sensitivity of Neoproterozoic snowball-Earth inceptions to continental configuration, orbital geometry, and volcanism J. Eberhard et al. 10.5194/cp-19-2203-2023
24. Sensitivity of the Palaeocene–Eocene Thermal Maximum climate to cloud properties J. Kiehl & C. Shields 10.1098/rsta.2013.0093
25. A model–model and data–model comparison for the early Eocene hydrological cycle M. Carmichael et al. 10.5194/cp-12-455-2016
26. Climate Sensitivity on Geological Timescales Controlled by Nonlinear Feedbacks and Ocean Circulation A. Farnsworth et al. 10.1029/2019GL083574
27. Simulating the climate response to atmospheric oxygen variability in the Phanerozoic: a focus on the Holocene, Cretaceous and Permian D. Wade et al. 10.5194/cp-15-1463-2019
28. Eocene greenhouse climate revealed by coupled clumped isotope-Mg/Ca thermometry D. Evans et al. 10.1073/pnas.1714744115
29. On the mechanisms of warming the mid-Pliocene and the inference of a hierarchy of climate sensitivities with relevance to the understanding of climate futures D. Chandan & W. Peltier 10.5194/cp-14-825-2018
30. South American Climate during the Early Eocene: Impact of a Narrower Atlantic and Higher Atmospheric CO2 X. Liu et al. 10.1175/JCLI-D-19-0170.1
31. Simulating Miocene Warmth: Insights From an Opportunistic Multi‐Model Ensemble (MioMIP1) N. Burls et al. 10.1029/2020PA004054
32. Warm mid-Pliocene conditions without high climate sensitivity: the CCSM4-Utrecht (CESM 1.0.5) contribution to the PlioMIP2 M. Baatsen et al. 10.5194/cp-18-657-2022
33. A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2 J. Sinninghe Damsté et al. 10.1016/j.epsl.2010.02.027
34. Influence of ocean tides on the general ocean circulation in the early Eocene T. Weber & M. Thomas 10.1002/2016PA002997
35. Impacts of ocean gateway and basin width on Tertiary tropical climate variability in a prototype model S. An et al. 10.1007/s00704-011-0469-x
36. The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum M. Stärz et al. 10.5194/cp-12-151-2016
37. The Early Eocene equable climate problem: can perturbations of climate model parameters identify possible solutions? N. Sagoo et al. 10.1098/rsta.2013.0123
38. Mid-Pliocene not analogous to high-CO2 climate when considering Northern Hemisphere winter variability A. Oldeman et al. 10.5194/wcd-5-395-2024
39. Eocene monsoons M. Huber & A. Goldner 10.1016/j.jseaes.2011.09.014
40. DeepMIP-Eocene-p1: multi-model dataset and interactive web application for Eocene climate research S. Steinig et al. 10.1038/s41597-024-03773-4
41. Using results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm Period A. Dolan et al. 10.5194/cp-11-403-2015
42. High temperatures in the terrestrial mid-latitudes during the early Palaeogene B. Naafs et al. 10.1038/s41561-018-0199-0
43. The early Eocene equable climate problem revisited M. Huber & R. Caballero 10.5194/cp-7-603-2011
44. On the connection between tropical circulation, convective mixing, and climate sensitivity L. Tomassini et al. 10.1002/qj.2450
45. Simulation of Eocene extreme warmth and high climate sensitivity through cloud feedbacks J. Zhu et al. 10.1126/sciadv.aax1874
46. On the causes of mid-Pliocene warmth and polar amplification D. Lunt et al. 10.1016/j.epsl.2011.12.042
47. Ocean biogeochemistry in the warm climate of the late Paleocene M. Heinze & T. Ilyina 10.5194/cp-11-63-2015
48. Stripping back the modern to reveal the Cenomanian–Turonian climate and temperature gradient underneath M. Laugié et al. 10.5194/cp-16-953-2020
49. DeepMIP: model intercomparison of early Eocene climatic optimum (EECO) large-scale climate features and comparison with proxy data D. Lunt et al. 10.5194/cp-17-203-2021
50. The Middle Miocene climate as modelled in an atmosphere-ocean-biosphere model M. Krapp & J. Jungclaus 10.5194/cp-7-1169-2011
51. Meridional Heat Transport in the DeepMIP Eocene Ensemble: Non‐CO2 and CO2 Effects F. Kelemen et al. 10.1029/2022PA004607
52. Climate Variations in the Past 250 Million Years and Contributing Factors X. Li et al. 10.1029/2022PA004503
53. Investigating vegetation–climate feedbacks during the early Eocene C. Loptson et al. 10.5194/cp-10-419-2014
54. Terrestrial environmental change across the onset of the PETM and the associated impact on biomarker proxies: A cautionary tale G. Inglis et al. 10.1016/j.gloplacha.2019.102991
55. The role of ocean gateways on cooling climate on long time scales W. Sijp et al. 10.1016/j.gloplacha.2014.04.004
56. Warm Terrestrial Subtropics During the Paleocene and Eocene: Carbonate Clumped Isotope (Δ47) Evidence From the Tornillo Basin, Texas (USA) J. Kelson et al. 10.1029/2018PA003391
57. Eocene seasonality and seawater alkaline earth reconstruction using shallow-dwelling large benthic foraminifera D. Evans et al. 10.1016/j.epsl.2013.08.035
58. Simulation of the Climate and the Ocean Circulations in the Middle Miocene Climate Optimum by a Coupled Model Fgoals-G3 J. Wei et al. 10.2139/ssrn.4104022
59. Climate Sensitivity in the Geologic Past D. Royer 10.1146/annurev-earth-100815-024150
60. The impact of climate‐vegetation interactions on the onset of the Antarctic ice sheet J. Liakka et al. 10.1002/2013GL058994
61. Developments in the MPI‐M Earth System Model version 1.2 (MPI‐ESM1.2) and Its Response to Increasing CO2 T. Mauritsen et al. 10.1029/2018MS001400
62. Southern ocean warming, sea level and hydrological change during the Paleocene-Eocene thermal maximum A. Sluijs et al. 10.5194/cp-7-47-2011
63. Tracing the Snowball bifurcation of aquaplanets through time reveals a fundamental shift in critical-state dynamics G. Feulner et al. 10.5194/esd-14-533-2023
64. Was the Arctic Eocene ‘rainforest’ monsoonal? Estimates of seasonal precipitation from early Eocene megafloras from Ellesmere Island, Nunavut C. West et al. 10.1016/j.epsl.2015.06.036
65. Radiative forcing and feedback by forests in warm climates – a sensitivity study U. Port et al. 10.5194/esd-7-535-2016
66. Tropical seaways played a more important role than high latitude seaways in Cenozoic cooling Z. Zhang et al. 10.5194/cp-7-801-2011
67. Does Antarctic glaciation cool the world? A. Goldner et al. 10.5194/cp-9-173-2013
68. On the sensitivity of ocean circulation to arctic freshwater input during the Paleocene/Eocene Thermal Maximum J. Cope & A. Winguth 10.1016/j.palaeo.2011.03.032
69. The transition from the present-day climate to a modern Snowball Earth A. Voigt & J. Marotzke 10.1007/s00382-009-0633-5
70. Early Eocene Asian climate dominated by desert and steppe with limited monsoons Z. Zhang et al. 10.1016/j.jseaes.2011.05.013