203 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
30. The Glacier‐Climate Interaction Over the Tibetan Plateau and Its Surroundings During the Last Glacial Maximum Q. Wei et al. 10.1029/2023GL103538
31. Global peatland area and carbon dynamics from the Last Glacial Maximum to the present – a process-based model investigation J. Müller & F. Joos 10.5194/bg-17-5285-2020
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37. Uncertainty in temperature and sea level datasets for the Pleistocene glacial cycles: Implications for thermal state of the subsea sediments V. Malakhova & A. Eliseev 10.1016/j.gloplacha.2020.103249
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40. A Method for Generating Coherent Spatially Explicit Maps of Seasonal Paleoclimates From Site‐Based Reconstructions S. Cleator et al. 10.1029/2019MS001630
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49. Bayesian deconstruction of climate sensitivity estimates using simple models: implicit priors and the confusion of the inverse J. Annan & J. Hargreaves 10.5194/esd-11-347-2020
50. The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
51. Cosmogenic noble gas paleothermometry M. Tremblay et al. 10.1016/j.epsl.2014.05.040
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53. Climate simulations and pollen data reveal the distribution and connectivity of temperate tree populations in eastern Asia during the Last Glacial Maximum S. Leroy et al. 10.5194/cp-16-2039-2020
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
57. The impact of ICE‐6G ice sheet topography in the oceanic carbonate system N. Leonardo et al. 10.1002/joc.8236
58. Submarine melt as a potential trigger of the North East Greenland Ice Stream margin retreat during Marine Isotope Stage 3 I. Tabone et al. 10.5194/tc-13-1911-2019
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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
77. Temperatures recorded by cosmogenic noble gases since the last glacial maximum in the Maritime Alps M. Tremblay et al. 10.1017/qua.2018.109
78. Widespread six degrees Celsius cooling on land during the Last Glacial Maximum A. Seltzer et al. 10.1038/s41586-021-03467-6
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
82. A palaeovegetation and diatom record of tropical montane forest fire, vegetation and hydroseral changes on Mount Kenya from 27,000–16,500 cal yr BP C. Courtney Mustaphi et al. 10.1016/j.palaeo.2021.110625
83. Objectively combining climate sensitivity evidence N. Lewis 10.1007/s00382-022-06468-x
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
88. The effect of greenhouse gas concentrations and ice sheets on the glacial AMOC in a coupled climate model M. Klockmann et al. 10.5194/cp-12-1829-2016
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
91. Transcriptome profiling and phytohormone responses of Arabidopsis roots to different ambient temperatures Q. Fei et al. 10.1080/17429145.2019.1634770
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93. Equilibrium simulations of Marine Isotope Stage 3 climate C. Guo et al. 10.5194/cp-15-1133-2019
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96. Paleoclimatological Context and Reference Level of the 2°C and 1.5°C Paris Agreement Long-Term Temperature Limits S. Lüning & F. Vahrenholt 10.3389/feart.2017.00104
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108. 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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114. Unraveling the complexities of the Last Glacial Maximum climate: the role of individual boundary conditions and forcings X. Shi et al. 10.5194/cp-19-2157-2023
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118. Dropstones in the Mar del Plata Canyon Area (SW Atlantic): Evidence for Provenance, Transport, Distribution, and Oceanographic Implications G. Bozzano et al. 10.1029/2020GC009333
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120. Climate Simulations of Early Mars With Estimated Precipitation, Runoff, and Erosion Rates R. Ramirez et al. 10.1029/2019JE006160
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136. Evidence for Pleistocene periglaciation in the lowlands of central Argentina (36–39°S) T. Vogt 10.1017/qua.2022.30
137. A multi-model analysis of moisture changes during the last glacial maximum S. Liu et al. 10.1016/j.quascirev.2018.05.029
138. 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
139. A Modeling Perspective on the Lingering Glacial Sea Surface Temperature Conundrum S. Krätschmer et al. 10.1029/2022GL100378
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142. Speaking about Heat Flow, Ice Fusion and Temperature Alterations M. Duque 10.1088/1755-1315/221/1/012060
143. Could cirrus clouds have warmed early Mars? R. Ramirez & J. Kasting 10.1016/j.icarus.2016.08.016
144. A physical framework for the earth system, Anthropocene equation and the great acceleration O. Bertolami & F. Francisco 10.1016/j.gloplacha.2018.07.006
145. Vegetation and climate evolution during the Last Glaciation at Tengchong in Yunnan Province, Southwest China J. Zhang et al. 10.1016/j.palaeo.2018.11.008
146. A model study of the effect of climate and sea-level change on the evolution of the Antarctic Ice Sheet from the Last Glacial Maximum to 2100 M. Maris et al. 10.1007/s00382-014-2317-z
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155. Spatial and temporal variability in sea surface temperatures and monsoon dynamics in the northwestern Arabian Sea during the last 43 kyr J. Maier et al. 10.5194/cp-21-279-2025
156. Changes in Ecologically Critical Terrestrial Climate Conditions N. Diffenbaugh & C. Field 10.1126/science.1237123
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158. 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
159. 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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174. Reconstruction of climate and ecology of Skagit Valley, Washington, from 27.7 to 19.8 ka based on plant and beetle macrofossils J. Riedel et al. 10.1017/qua.2021.50
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