202 citations as recorded by crossref.

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29. Clumped‐Isotope Constraint on Upper‐Tropospheric Cooling During the Last Glacial Maximum A. Banerjee et al. 10.1029/2022AV000688
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54. Climate and ice sheet dynamics in Patagonia throughout marine isotope stages 2 and 3 A. Castillo-Llarena et al. 10.5194/cp-20-1559-2024
55. Response of a comprehensive climate model to a broad range of external forcings: relevance for deep ocean ventilation and the development of late Cenozoic ice ages E. Galbraith & C. de Lavergne 10.1007/s00382-018-4157-8
56. Model-simulated hydroclimate in the East Asian summer monsoon region during past and future climate: a pilot study with a moisture source perspective A. Fremme et al. 10.5194/wcd-4-449-2023
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60. Modelling the potential for permafrost development on a radioactive waste geological disposal facility in Great Britain J. Busby et al. 10.1016/j.pgeola.2015.06.001
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66. Simple noise estimates and pseudoproxies for the last 21 000 years O. Bothe et al. 10.5194/essd-11-1129-2019
67. The response of the hydrological cycle to temperature changes in recent and distant climatic history S. Pratap & Y. Markonis 10.1186/s40645-022-00489-0
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76. Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions F. Ziemen et al. 10.5194/cp-10-1817-2014
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79. Modeled Influence of Land Ice and CO2on Polar Amplification and Paleoclimate Sensitivity During the Past 5 Million Years L. Stap et al. 10.1002/2017PA003313
80. On the relationship between climate and Neandertal fire use during the Last Glacial in south-west France A. Sorensen 10.1016/j.quaint.2016.10.003
81. Quaternary coral reef refugia preserved fish diversity L. Pellissier et al. 10.1126/science.1249853
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84. A phase space description of the Earth System in the Anthropocene O. Bertolami & F. Francisco 10.1209/0295-5075/127/59001
85. Extratropical cyclones over the North Atlantic and western Europe during the Last Glacial Maximum and implications for proxy interpretation J. Pinto & P. Ludwig 10.5194/cp-16-611-2020
86. Impact of Southern Ocean surface conditions on deep ocean circulation during the LGM: a model analysis F. Lhardy et al. 10.5194/cp-17-1139-2021
87. Using Late Pleistocene sea surface temperature reconstructions to constrain future greenhouse warming T. Friedrich & A. Timmermann 10.1016/j.epsl.2019.115911
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89. Implication of methodological uncertainties for mid-Holocene sea surface temperature reconstructions I. Hessler et al. 10.5194/cp-10-2237-2014
90. Paleoclimate Changes in the Pacific Northwest Over the Past 36,000 Years From Clumped Isotope Measurements and Model Analysis R. Lopez‐Maldonado et al. 10.1029/2021PA004266
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107. ForCenS-LGM: a dataset of planktonic foraminifera species assemblage composition for the Last Glacial Maximum L. Jonkers et al. 10.1038/s41597-024-03166-7
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119. Climate Simulations of Early Mars With Estimated Precipitation, Runoff, and Erosion Rates R. Ramirez et al. 10.1029/2019JE006160
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137. Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions M. Adloff et al. 10.5194/esd-9-413-2018
138. A Modeling Perspective on the Lingering Glacial Sea Surface Temperature Conundrum S. Krätschmer et al. 10.1029/2022GL100378
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141. Speaking about Heat Flow, Ice Fusion and Temperature Alterations M. Duque 10.1088/1755-1315/221/1/012060
142. Could cirrus clouds have warmed early Mars? R. Ramirez & J. Kasting 10.1016/j.icarus.2016.08.016
143. A physical framework for the earth system, Anthropocene equation and the great acceleration O. Bertolami & F. Francisco 10.1016/j.gloplacha.2018.07.006
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156. Atmosphere–cryosphere interactions during the last phase of the Last Glacial Maximum (21 ka) in the European Alps C. Del Gobbo et al. 10.5194/cp-19-1805-2023
157. Tropical mountain ice core δ 18 O: A Goldilocks indicator for global temperature change Z. Liu et al. 10.1126/sciadv.adi6725
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