99 citations as recorded by crossref.

1. Abrupt climate changes in the last two deglaciations simulated with different Northern ice sheet discharge and insolation T. Obase et al. 10.1038/s41598-021-01651-2
2. Stratospheric Ozone in the Last Glacial Maximum M. Wang et al. 10.1029/2020JD032929
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. The Brewer‐Dobson Circulation During the Last Glacial Maximum Q. Fu et al. 10.1029/2019GL086271
5. An Assessment of Earth's Climate Sensitivity Using Multiple Lines of Evidence S. Sherwood et al. 10.1029/2019RG000678
6. Influence of glacial ice sheets on the Atlantic meridional overturning circulation through surface wind change S. Sherriff-Tadano et al. 10.1007/s00382-017-3780-0
7. Abrupt Bølling‐Allerød Warming Simulated under Gradual Forcing of the Last Deglaciation T. Obase & A. Abe‐Ouchi 10.1029/2019GL084675
8. Glacial deep ocean deoxygenation driven by biologically mediated air–sea disequilibrium E. Cliff et al. 10.1038/s41561-020-00667-z
9. Influence of Large‐Scale Atmospheric Dynamics on Precipitation Seasonality of the Tibetan Plateau and Central Asia in Cold and Warm Climates During the Late Cenozoic S. Botsyun et al. 10.1029/2021JD035810
10. Estimates of late Cenozoic climate change relevant to Earth surface processes in tectonically active orogens S. Mutz et al. 10.5194/esurf-6-271-2018
11. Increased interglacial atmospheric CO2 levels followed the mid-Pleistocene Transition M. Yamamoto et al. 10.1038/s41561-022-00918-1
12. Moisture amplification of the high-altitude deglacial warming E. Legrain et al. 10.1016/j.quascirev.2023.108303
13. The influence of climate on peatland extent in Western Siberia since the Last Glacial Maximum G. Alexandrov et al. 10.1038/srep24784
14. Deglacial Ice Sheet Instabilities Induced by Proglacial Lakes A. Quiquet et al. 10.1029/2020GL092141
15. Climate Noise Influences Ice Sheet Mean State L. Niu et al. 10.1029/2019GL083717
16. A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions F. Lhardy et al. 10.1029/2021PA004302
17. Strong temperature gradients in the ice age North Atlantic Ocean revealed by plankton biogeography L. Jonkers et al. 10.1038/s41561-023-01328-7
18. Responses of Basal Melting of Antarctic Ice Shelves to the Climatic Forcing of the Last Glacial Maximum and CO2 Doubling T. Obase et al. 10.1175/JCLI-D-15-0908.1
19. Relative sea level in the Western Mediterranean basin: A regional test of the ICE-7G_NA (VM7) model and a constraint on late Holocene Antarctic deglaciation K. Roy & W. Peltier 10.1016/j.quascirev.2017.12.021
20. From monsoon to marine productivity in the Arabian Sea: insights from glacial and interglacial climates P. Le Mézo et al. 10.5194/cp-13-759-2017
21. The PMIP4 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3 simulations M. Kageyama et al. 10.5194/cp-17-1065-2021
22. Interactive ocean bathymetry and coastlines for simulating the last deglaciation with the Max Planck Institute Earth System Model (MPI-ESM-v1.2) V. Meccia & U. Mikolajewicz 10.5194/gmd-11-4677-2018
23. 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
24. 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
25. Millennial‐Scale Climate Oscillations Triggered by Deglacial Meltwater Discharge in Last Glacial Maximum Simulations Y. Romé et al. 10.1029/2022PA004451
26. Modelling feedbacks between the Northern Hemisphere ice sheets and climate during the last glacial cycle M. Scherrenberg et al. 10.5194/cp-19-399-2023
27. On the Reduced North Atlantic Storminess during the Last Glacial Period: The Role of Topography in Shaping Synoptic Eddies G. Rivière et al. 10.1175/JCLI-D-17-0247.1
28. Air-sea coupling shapes North American hydroclimate response to ice sheets during the Last Glacial Maximum D. Amaya et al. 10.1016/j.epsl.2021.117271
29. Quasi-Biennial Oscillation and Sudden Stratospheric Warmings during the Last Glacial Maximum Q. Fu et al. 10.3390/atmos11090943
30. 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
31. 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
32. Stationary Wave Reflection as a Mechanism for Zonalizing the Atlantic Winter Jet at the LGM M. Löfverström et al. 10.1175/JAS-D-15-0295.1
33. Uncertainty in Reconstructing Paleo‐Elevation of the Antarctic Ice Sheet From Temperature‐Sensitive Ice Core Records J. Badgeley et al. 10.1029/2022GL100334
34. 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
35. Ice-sheet and sea-level reconstructions in East Antarctica since the Last Interglacial period: review and future challenges T. Ishiwa 10.5575/geosoc.2022.0041
36. The PMIP4 contribution to CMIP6 – Part 1: Overview and over-arching analysis plan M. Kageyama et al. 10.5194/gmd-11-1033-2018
37. The PMIP4 contribution to CMIP6 – Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 sensitivity experiments M. Kageyama et al. 10.5194/gmd-10-4035-2017
38. What have we learnt from palaeoclimate simulations? S. Harrison et al. 10.1002/jqs.2842
39. Climatic patterns over the European Alps during the LGM derived from inversion of the paleo-ice extent V. Višnjević et al. 10.1016/j.epsl.2020.116185
40. The Pacific-North American teleconnection in the Cenozoic Z. Li et al. 10.1016/j.gloplacha.2024.104402
41. State dependence of climatic instability over the past 720,000 years from Antarctic ice cores and climate modeling K. Kawamura et al. 10.1126/sciadv.1600446
42. Modelling the Past and Future Climate by Dr. Syukuro Manabe A. ABE-OUCHI 10.5363/tits.27.2_14
43. Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation N. Weitzel et al. 10.5194/cp-20-865-2024
44. The effects of late Cenozoic climate change on the global distribution of frost cracking H. Sharma et al. 10.5194/esurf-10-997-2022
45. Data and models reveal humid environmental conditions during MIS 3 in two of the world’s largest deserts A. Lézine et al. 10.5802/crgeos.240
46. Causes of the weak emergent constraint on climate sensitivity at the Last Glacial Maximum M. Renoult et al. 10.5194/cp-19-323-2023
47. Constraint on the penultimate glacial maximum Northern Hemisphere ice topography (≈140 kyrs BP) F. Colleoni et al. 10.1016/j.quascirev.2016.01.024
48. Two AMOC States in Response to Decreasing Greenhouse Gas Concentrations in the Coupled Climate Model MPI-ESM M. Klockmann et al. 10.1175/JCLI-D-17-0859.1
49. Reconciling glacial Antarctic water stable isotopes with ice sheet topography and the isotopic paleothermometer M. Werner et al. 10.1038/s41467-018-05430-y
50. Impacts of the PMIP4 ice sheets on Northern Hemisphere climate during the last glacial period K. Izumi et al. 10.1007/s00382-022-06456-1
51. The sensitivity of Northern Hemisphere ice sheets to atmospheric forcing during the last glacial cycle using PMIP3 models L. NIU et al. 10.1017/jog.2019.42
52. Impact of mid-glacial ice sheets on deep ocean circulation and global climate S. Sherriff-Tadano et al. 10.5194/cp-17-95-2021
53. Air-sea disequilibrium enhances ocean carbon storage during glacial periods S. Khatiwala et al. 10.1126/sciadv.aaw4981
54. Dansgaard–Oeschger events in climate models: review and baseline Marine Isotope Stage 3 (MIS3) protocol I. Malmierca-Vallet & L. Sime 10.5194/cp-19-915-2023
55. Combined Effects of Atmospheric and Seafloor Iron Fluxes to the Glacial Ocean J. Muglia et al. 10.1002/2016PA003077
56. Enhanced Mid‐depth Southward Transport in the Northeast Atlantic at the Last Glacial Maximum Despite a Weaker AMOC L. Menviel et al. 10.1029/2019PA003793
57. Transient climate simulations of the deglaciation 21–9 thousand years before present (version 1) – PMIP4 Core experiment design and boundary conditions R. Ivanovic et al. 10.5194/gmd-9-2563-2016
58. Effect of high dust amount on surface temperature during the Last Glacial Maximum: a modelling study using MIROC-ESM R. Ohgaito et al. 10.5194/cp-14-1565-2018
59. The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
60. Weak overturning circulation and high Southern Ocean nutrient utilization maximized glacial ocean carbon J. Muglia et al. 10.1016/j.epsl.2018.05.038
61. Roles of Sea Ice–Surface Wind Feedback in Maintaining the Glacial Atlantic Meridional Overturning Circulation and Climate S. Sherriff-Tadano & A. Abe-Ouchi 10.1175/JCLI-D-19-0431.1
62. Modeling the Greenland englacial stratigraphy A. Born & A. Robinson 10.5194/tc-15-4539-2021
63. Earth’s radiative imbalance from the Last Glacial Maximum to the present D. Baggenstos et al. 10.1073/pnas.1905447116
64. Comparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models J. Brown et al. 10.5194/cp-16-1777-2020
65. Enhanced Interannual Variability in Temperature during the Last Glacial Maximum J. Shi et al. 10.1175/JCLI-D-21-0739.1
66. Topography explains the distribution of genetic diversity in one of the most fragile European hotspots J. Blanco‐Pastor et al. 10.1111/ddi.12836
67. A mechanistic understanding of oxygen isotopic changes in the Western United States at the Last Glacial Maximum C. Tabor et al. 10.1016/j.quascirev.2021.107255
68. Reassessing the Value of Regional Climate Modeling Using Paleoclimate Simulations E. Armstrong et al. 10.1029/2019GL085127
69. Holocene warmth explains the Little Ice Age advance of Sermeq Kujalleq K. Kajanto et al. 10.1016/j.quascirev.2024.108840
70. Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography T. Jones et al. 10.1038/nature24669
71. LGM Paleoclimate Constraints Inform Cloud Parameterizations and Equilibrium Climate Sensitivity in CESM2 J. Zhu et al. 10.1029/2021MS002776
72. Developing a new testate amoeba hydrological transfer function for permafrost peatlands of NW Siberia A. Halaś et al. 10.1016/j.quascirev.2023.108067
73. Postglacial relative sea level change in Norway R. Creel et al. 10.1016/j.quascirev.2022.107422
74. Comparison of spatial downscaling methods of general circulation model results to study climate variability during the Last Glacial Maximum G. Latombe et al. 10.5194/gmd-11-2563-2018
75. 1-km resolution rebound surfaces and paleotopography of glaciated North America since the Last Glacial Maximum P. Godbout et al. 10.1038/s41597-023-02566-5
76. Metric-Dependent Tendency of Tropical Belt Width Changes during the Last Glacial Maximum N. Wang et al. 10.1175/JCLI-D-18-0199.1
77. Arctic warming induced by the Laurentide Ice Sheet topography J. Liakka & M. Lofverstrom 10.5194/cp-14-887-2018
78. A 1.8 million year history of Amazon vegetation A. Kern et al. 10.1016/j.quascirev.2022.107867
79. Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions J. Blasco et al. 10.5194/tc-15-215-2021
80. Detection and explanation of spatiotemporal patterns in Late Cenozoic palaeoclimate change relevant to Earth surface processes S. Mutz & T. Ehlers 10.5194/esurf-7-663-2019
81. Space-geodetic and water level gauge constraints on continental uplift and tilting over North America: regional convergence of the ICE-6G_C (VM5a/VM6) models K. Roy & W. Peltier 10.1093/gji/ggx156
82. Distorted Pacific–North American teleconnection at the Last Glacial Maximum Y. Hu et al. 10.5194/cp-16-199-2020
83. A review of past changes in extratropical cyclones in the northern hemisphere and what can be learned for the future C. Raible et al. 10.1002/wcc.680
84. Late Pleistocene glacial terminations accelerated by proglacial lakes M. Scherrenberg et al. 10.5194/cp-20-1761-2024
85. Antarctic surface temperature and elevation during the Last Glacial Maximum C. Buizert et al. 10.1126/science.abd2897
86. Coupled atmosphere-ice-ocean dynamics in Dansgaard-Oeschger events C. Li & A. Born 10.1016/j.quascirev.2018.10.031
87. Mapping Sea-Level Change in Time, Space, and Probability B. Horton et al. 10.1146/annurev-environ-102017-025826
88. Applying the Community Ice Sheet Model to evaluate PMIP3 LGM climatologies over the North American ice sheets J. Alder & S. Hostetler 10.1007/s00382-019-04663-x
89. Circumpolar ocean stability on Mars 3 Gy ago F. Schmidt et al. 10.1073/pnas.2112930118
90. Relative importance of the mechanisms triggering the Eurasian ice sheet deglaciation in the GRISLI2.0 ice sheet model V. van Aalderen et al. 10.5194/cp-20-187-2024
91. Differences between the last two glacial maxima and implications for ice-sheet, δ18O, and sea-level reconstructions E. Rohling et al. 10.1016/j.quascirev.2017.09.009
92. Stratosphere‐Troposphere Exchanges of Air Mass and Ozone Concentration in the Last Glacial Maximum M. Wang et al. 10.1029/2021JD036327
93. Numerical reconstructions of the penultimate glacial maximum Northern Hemisphere ice sheets: sensitivity to climate forcing and model parameters C. WEKERLE et al. 10.1017/jog.2016.45
94. Glacial Atlantic overturning increased by wind stress in climate models J. Muglia & A. Schmittner 10.1002/2015GL064583
95. What drives LGM precipitation over the western Mediterranean? A study focused on the Iberian Peninsula and northern Morocco P. Beghin et al. 10.1007/s00382-015-2720-0
96. Tropical cyclone genesis potential across palaeoclimates J. Koh & C. Brierley 10.5194/cp-11-1433-2015
97. How might the North American ice sheet influence the northwestern Eurasian climate? P. Beghin et al. 10.5194/cp-11-1467-2015
98. On the limited ice intrusion in Alaska at the LGM M. Löfverström & J. Liakka 10.1002/2016GL071012
99. The contrasting effects of thermodynamic and dynamic processes on East Asian summer monsoon precipitation during the Last Glacial Maximum: a data-model comparison Y. Sun et al. 10.1007/s00382-020-05533-7