154 citations as recorded by crossref.

1. Hydroclimatic processes as the primary drivers of the Early Khvalynian transgression of the Caspian Sea: new developments A. Gelfan et al. 10.5194/hess-28-241-2024
2. A RESPONSE TO COMMUNITY QUESTIONS ON THE MARINE20 RADIOCARBON AGE CALIBRATION CURVE: MARINE RESERVOIR AGES AND THE CALIBRATION OF 14C SAMPLES FROM THE OCEANS T. Heaton et al. 10.1017/RDC.2022.66
3. Rapid Laurentide Ice Sheet growth preceding the Last Glacial Maximum due to summer snowfall L. Niu et al. 10.1038/s41561-024-01419-z
4. 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
5. Global Climate Classification and Comparison to Mid-Holocene and Last Glacial Maximum Climates, with Added Aridity Information and a Hypertropical Class B. Hanberry 10.3390/earth4030029
6. Glacial Warming in the Eastern Pacific Warm Pool D. Meegan Kumar et al. 10.1029/2022GL098830
7. Constraining Clouds and Convective Parameterizations in a Climate Model Using Paleoclimate Data R. Ramos et al. 10.1029/2021MS002893
8. Changes in Atmospheric Dynamics Over Dansgaard‐Oeschger Climate Oscillations Around 40 ka and Their Impact on Europe K. Stadelmaier et al. 10.1029/2023JD040247
9. Climate and ice sheet evolutions from the last glacial maximum to the pre-industrial period with an ice-sheet–climate coupled model A. Quiquet et al. 10.5194/cp-17-2179-2021
10. Evolution of Atlantic Meridional Overturning Circulation since the last glaciation: model simulations and relevance to present and future Z. Liu 10.1098/rsta.2022.0190
11. Multicentennial-scale coupling of the East Asian monsoon to North Atlantic climates during the Last Glacial Maximum Y. Cui et al. 10.1016/j.palaeo.2024.112445
12. High-resolution LGM climate of Europe and the Alpine region using the regional climate model WRF E. Russo et al. 10.5194/cp-20-449-2024
13. 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
14. 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
15. New dating indicates intermittent human occupation of the Nwya Devu Paleolithic site on the high-altitude central Tibetan Plateau during the past 45,000 years J. Ge et al. 10.1007/s11430-022-1225-7
16. The Hydrologic Cycle and Atmospheric Rivers in CESM2 Simulations of the Last Glacial Maximum J. Lora et al. 10.1029/2023GL104805
17. Dynamic processes determine precipitation variability in Eastern Central Europe since the Last Glacial Maximum S. Warken et al. 10.1038/s43247-024-01876-9
18. Russian Climate Research in 2019–2022 I. Mokhov 10.1134/S0001433823150100
19. Continuous synchronization of the Greenland ice-core and U–Th timescales using probabilistic inversion F. Muschitiello & M. Aquino-Lopez 10.5194/cp-20-1415-2024
20. Evaluating seasonal sea-ice cover over the Southern Ocean at the Last Glacial Maximum R. Green et al. 10.5194/cp-18-845-2022
21. Revisiting Western United States Hydroclimate During the Last Deglaciation M. Fu 10.1029/2022GL101997
22. 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
23. The warm winter paradox in the Pliocene northern high latitudes J. Tindall et al. 10.5194/cp-18-1385-2022
24. Atmospheric and oceanic circulation altered by global mean sea-level rise Z. Zhang et al. 10.1038/s41561-023-01153-y
25. Atmospheric River Contributions to Ice Sheet Hydroclimate at the Last Glacial Maximum C. Skinner et al. 10.1029/2022GL101750
26. A global Data Assimilation of Moisture Patterns from 21 000–0 BP (DAMP-21ka) using lake level proxy records C. Hancock et al. 10.5194/cp-20-2663-2024
27. Past foraminiferal acclimatization capacity is limited during future warming R. Ying et al. 10.1038/s41586-024-08029-0
28. A Modeling Perspective on the Lingering Glacial Sea Surface Temperature Conundrum S. Krätschmer et al. 10.1029/2022GL100378
29. Causes of the weak emergent constraint on climate sensitivity at the Last Glacial Maximum M. Renoult et al. 10.5194/cp-19-323-2023
30. Coupled climate-glacier modelling of the last glaciation in the Alps G. Jouvet et al. 10.1017/jog.2023.74
31. Changes to population-based emergence of climate change from CMIP5 to CMIP6 H. Douglas et al. 10.1088/1748-9326/aca91e
32. Elevated Southern Hemisphere moisture availability during glacial periods R. Weij et al. 10.1038/s41586-023-06989-3
33. Multiple thermal Atlantic Meridional Overturning Circulation thresholds in the intermediate complexity model Bern3D M. Adloff et al. 10.5194/cp-20-1233-2024
34. Last Glacial Maximum pattern effects reduce climate sensitivity estimates V. Cooper et al. 10.1126/sciadv.adk9461
35. Impact of Dust on Climate and AMOC During the Last Glacial Maximum Simulated by CESM1.2 M. Zhang et al. 10.1029/2021GL096672
36. Last Glacial Maximum climate and atmospheric circulation over the Australian region from climate models Y. Du et al. 10.5194/cp-20-393-2024
37. Continental shelf area inundation drove reduced temperature seasonality in East Asia during the last deglaciation Y. Ma et al. 10.1038/s41612-025-01091-z
38. Into the Holocene, anatomy of the Younger Dryas cold reversal and preboreal oscillation J. Velay-Vitow et al. 10.1038/s41598-024-53591-2
39. Uncertainty in Reconstructing Paleo‐Elevation of the Antarctic Ice Sheet From Temperature‐Sensitive Ice Core Records J. Badgeley et al. 10.1029/2022GL100334
40. Russian Climate Research in 2019–2022 I. Mokhov 10.31857/S0002351523070106
41. Evolution of winter precipitation in the Nile river watershed since the last glacial V. Meyer et al. 10.5194/cp-20-523-2024
42. Stronger Gulf Stream during the last ice age 10.1038/d41586-024-02407-4
43. The deglacial forest conundrum A. Dallmeyer et al. 10.1038/s41467-022-33646-6
44. Increasingly Sophisticated Climate Models Need the Out‐Of‐Sample Tests Paleoclimates Provide N. Burls & N. Sagoo 10.1029/2022MS003389
45. Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
46. Plankton reveal past climate M. Robinson 10.1038/s41561-023-01343-8
47. Globally resolved surface temperatures since the Last Glacial Maximum M. Osman et al. 10.1038/s41586-021-03984-4
48. To the theory of the Pliocene – Pleistocene and Holocene climate A. Kislov 10.31857/S2949178923010061
49. Surface buoyancy control of millennial-scale variations in the Atlantic meridional ocean circulation M. Willeit et al. 10.5194/cp-20-2719-2024
50. The Ice Core Gas Age‐Ice Age Difference as a Proxy for Surface Temperature C. Buizert 10.1029/2021GL094241
51. Towards robust community assessments of the Earth's climate sensitivity K. Marvel & M. Webb 10.5194/esd-16-317-2025
52. Last Glacial Maximum cooling induced positive moisture balance and maintained stable human populations in Australia H. Cadd et al. 10.1038/s43247-024-01204-1
53. The role of land cover in the climate of glacial Europe P. Velasquez et al. 10.5194/cp-17-1161-2021
54. MARINE RADIOCARBON CALIBRATION IN POLAR REGIONS: A SIMPLE APPROXIMATE APPROACH USING MARINE20 T. Heaton et al. 10.1017/RDC.2023.42
55. Proxy System Biases partially resolve long-standing paleoclimate data-model discrepancies in Tropical East Africa C. Marshall et al. 10.1016/j.quascirev.2025.109426
56. 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
57. An overview of the connection between Earth’s climate evolution and mass extinction events M. Montero-Martínez & M. Andrade-Velázquez 10.15446/esrj.v26n4.103152
58. Optically stimulated luminescence dating of Paleolithic sites reveals population shifts in North China during the last glacial period J. Ge et al. 10.1016/j.gloplacha.2023.104339
59. pastclim 1.2: an R package to easily access and use paleoclimatic reconstructions M. Leonardi et al. 10.1111/ecog.06481
60. Water budget of the Caspian Sea by numerical experiments with ocean circulation model INMIO-CICE in the last glacial maximum and pre-industrial period P. Morozova et al. 10.31857/S2686739724040131
61. Strong temperature gradients in the ice age North Atlantic Ocean revealed by plankton biogeography L. Jonkers et al. 10.1038/s41561-023-01328-7
62. Habitat suitability modeling of a nearly extinct rosewood species (Dalbergia odorifera) under current, and future climate conditions J. Lai et al. 10.1007/s11676-025-01853-8
63. Hydrometeorological Conditions of the Volga Flow Generation into the Caspian Sea during the Last Glacial Maximum A. Kalugin & P. Morozova 10.3390/cli11020036
64. Deglacial climate changes as forced by different ice sheet reconstructions N. Bouttes et al. 10.5194/cp-19-1027-2023
65. Rapid communication: Nonlinear sensitivity of the El Niño–Southern Oscillation across climate states G. Pontes et al. 10.5194/cp-21-1079-2025
66. Last glacial maximum cooling of 9 °C in continental Europe from a 40 kyr-long noble gas paleothermometry record D. Bekaert et al. 10.1016/j.quascirev.2023.108123
67. The Impact of Different Atmospheric CO2 Concentrations on Large Scale Miocene Temperature Signatures A. Hossain et al. 10.1029/2022PA004438
68. The Role of Wet Processes in Extratropical Thermal Stratification During the Glacial Period Z. Xie et al. 10.1029/2023GL106400
69. A stretched polar vortex increased mid-latitude climate variability during the Last Glacial Maximum Y. Zhang et al. 10.5194/cp-21-67-2025
70. Modeling the timing of Patagonian Ice Sheet retreat in the Chilean Lake District from 22–10 ka J. Cuzzone et al. 10.5194/tc-18-1381-2024
71. Seasonal aridity in the Indo-Pacific Warm Pool during the Late Glacial driven by El Niño-like conditions P. Hällberg et al. 10.5194/cp-18-1655-2022
72. Mechanisms Associated With Tropospheric Dry Static Stability Change During the Last Glacial Maximum Z. Xie et al. 10.1029/2023JD038900
73. 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
74. Indian Ocean variability changes in the Paleoclimate Modelling Intercomparison Project C. Brierley et al. 10.5194/cp-19-681-2023
75. Ice sheet model simulations reveal that polythermal ice conditions existed across the northeastern USA during the Last Glacial Maximum J. Cuzzone et al. 10.5194/tc-19-1559-2025
76. Variability and extremes: statistical validation of the Alfred Wegener Institute Earth System Model (AWI-ESM) J. Contzen et al. 10.5194/gmd-15-1803-2022
77. Testing the reliability of global surface temperature reconstructions of the Last Glacial Cycle with pseudo-proxy experiments J. Baudouin et al. 10.5194/cp-21-381-2025
78. Last Glacial loess in Europe: luminescence database and chronology of deposition M. Bosq et al. 10.5194/essd-15-4689-2023
79. Lessons from paleoclimates for recent and future climate change: opportunities and insights M. Kageyama et al. 10.3389/fclim.2024.1511997
80. 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
81. Design and performance of ELSA v2.0: an isochronal model for ice-sheet layer tracing T. Rieckh et al. 10.5194/gmd-17-6987-2024
82. Westerly aridity in the western Tarim Basin driven by global cooling since the mid-Pleistocene transition H. Liu et al. 10.1016/j.quascirev.2023.108412
83. 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
84. Advances in Paleoclimate Data Assimilation J. Tierney et al. 10.1146/annurev-earth-032320-064209
85. Retreating ice sheet caused a transition from cold-dry to cold-humid conditions in arid Central Asia L. Cheng et al. 10.1016/j.quascirev.2024.109057
86. 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
87. De‐Tuning Albedo Parameters in a Coupled Climate Ice Sheet Model to Simulate the North American Ice Sheet at the Last Glacial Maximum N. Gandy et al. 10.1029/2023JF007250
88. Western Caucasus regional hydroclimate controlled by cold-season temperature variability since the Last Glacial Maximum A. Wolf et al. 10.1038/s43247-023-01151-3
89. A resilient ice cover over the southernmost Mendeleev Ridge during the late Quaternary T. Song et al. 10.1111/bor.12632
90. Cenozoic History of the Indonesian Gateway S. Gallagher et al. 10.1146/annurev-earth-040722-111322
91. Moisture amplification of the high-altitude deglacial warming E. Legrain et al. 10.1016/j.quascirev.2023.108303
92. Greenland Ice Core Record of Last Glacial Dust Sources and Atmospheric Circulation G. Újvári et al. 10.1029/2022JD036597
93. Simulated stable water isotopes during the mid-Holocene and pre-industrial periods using AWI-ESM-2.1-wiso X. Shi et al. 10.5194/gmd-16-5153-2023
94. A new global surface temperature reconstruction for the Last Glacial Maximum J. Annan et al. 10.5194/cp-18-1883-2022
95. Atlantic inflow and low sea-ice cover in the Nordic Seas promoted Fennoscandian Ice Sheet growth during the Last Glacial Maximum M. Simon et al. 10.1038/s43247-023-01032-9
96. 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
97. Contribution of the Southern Annular Mode to Variations in Water Isotopes of Daily Precipitation at Dome Fuji, East Antarctica K. Kino et al. 10.1029/2021JD035397
98. Coexchangeable Process Modeling for Uncertainty Quantification in Joint Climate Reconstruction L. Astfalck et al. 10.1080/01621459.2024.2325705
99. Paleoclimate data provide constraints on climate models' large-scale response to past CO2 changes D. Lunt et al. 10.1038/s43247-024-01531-3
100. Glacial–interglacial Circumpolar Deep Water temperatures during the last 800 000 years: estimates from a synthesis of bottom water temperature reconstructions D. Chandler & P. Langebroek 10.5194/cp-20-2055-2024
101. Clumped‐Isotope Constraint on Upper‐Tropospheric Cooling During the Last Glacial Maximum A. Banerjee et al. 10.1029/2022AV000688
102. Potential and limitation of 230Th-excess as a chronostratigraphic tool for late Quaternary Arctic Ocean sediment studies: An example from the Southern Lomonosov Ridge K. Purcell et al. 10.1016/j.margeo.2022.106802
103. Late Quaternary hydroclimate of the Levant: The leaf wax record from the Dead Sea J. Tierney et al. 10.1016/j.quascirev.2022.107613
104. Surging of a Hudson Strait-scale ice stream: subglacial hydrology matters but the process details mostly do not M. Drew & L. Tarasov 10.5194/tc-17-5391-2023
105. The Earth system model CLIMBER-X v1.0 – Part 1: Climate model description and validation​​​​​​​​​​​​​​ M. Willeit et al. 10.5194/gmd-15-5905-2022
106. Hydroclimate variability over East Asia linked to ocean circulation, Antarctic and Pacific temperature changes during the LGM H. Lu et al. 10.1016/j.palaeo.2025.112781
107. Calendar effects on surface air temperature and precipitation based on model-ensemble equilibrium and transient simulations from PMIP4 and PACMEDY X. Shi et al. 10.5194/cp-18-1047-2022
108. Surface mass balance and climate of the Last Glacial Maximum Northern Hemisphere ice sheets: simulations with CESM2.1 S. Bradley et al. 10.5194/cp-20-211-2024
109. Of Atlantic Meridional Overturning Circulation in the CMIP6 Project X. Gong et al. 10.1016/j.dsr2.2022.105193
110. A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum M. Prange et al. 10.1126/sciadv.adh1106
111. 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
112. Effects of Last Glacial Maximum (LGM) sea surface temperature and sea ice extent on the isotope–temperature slope at polar ice core sites A. Cauquoin et al. 10.5194/cp-19-1275-2023
113. High-resolution marine data and transient simulations support orbital forcing of ENSO amplitude since the mid-Holocene M. Carré et al. 10.1016/j.quascirev.2021.107125
114. Terrestrial amplification of past, present, and future climate change A. Seltzer et al. 10.1126/sciadv.adf8119
115. Millennial‐Scale Climate Oscillations Triggered by Deglacial Meltwater Discharge in Last Glacial Maximum Simulations Y. Romé et al. 10.1029/2022PA004451
116. The climate and vegetation of Europe, northern Africa, and the Middle East during the Last Glacial Maximum (21 000 yr BP) based on pollen data B. Davis et al. 10.5194/cp-20-1939-2024
117. Ice sheet–free West Antarctica during peak early Oligocene glaciation J. Klages et al. 10.1126/science.adj3931
118. 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
119. Investigating similarities and differences of the penultimate and last glacial terminations with a coupled ice sheet–climate model A. Quiquet & D. Roche 10.5194/cp-20-1365-2024
120. CO2 and summer insolation as drivers for the Mid-Pleistocene Transition M. Scherrenberg et al. 10.5194/cp-21-1061-2025
121. The hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2 X. Ren et al. 10.5194/cp-19-2053-2023
122. Analysing the PMIP4-CMIP6 collection: a workflow and tool (pmip_p2fvar_analyzer v1) A. Zhao et al. 10.5194/gmd-15-2475-2022
123. Tropical Precipitation Woes in the Community Earth System Model Version 2 M. Lofverstrom & J. Zhu 10.1029/2023GL104416
124. Deglaciation and abrupt events in a coupled comprehensive atmosphere–ocean–ice-sheet–solid-earth model U. Mikolajewicz et al. 10.5194/cp-21-719-2025
125. ZEMBA v1.0: an energy and moisture balance climate model to investigate Quaternary climate D. Gunning et al. 10.5194/gmd-18-2479-2025
126. Warming‐Induced Northwestward Migration of the Asian Summer Monsoon in the Geological Past: Evidence From Climate Simulations and Geological Reconstructions X. Huang et al. 10.1029/2021JD035190
127. Equilibrium line altitudes of alpine glaciers in Alaska suggest Last Glacial Maximum summer temperature was 2–5 °C lower than during the pre-industrial C. Walcott et al. 10.5194/cp-20-91-2024
128. Identifying Global‐Scale Patterns of Vegetation Change During the Last Deglaciation From Paleoclimate Networks M. Adam et al. 10.1029/2021PA004265
129. The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
130. The response of wildfire regimes to Last Glacial Maximum carbon dioxide and climate O. Haas et al. 10.5194/bg-20-3981-2023
131. Glacial isostatic adjustment: physical models and observational constraints W. Peltier et al. 10.1088/1361-6633/ac805b
132. Water Balance of the Caspian Sea in the Last Glacial Maximum and Pre-Industrial Conditions Based on the Experiments with the INMIO-CICE General Sea Circulation Model P. Morozova et al. 10.1134/S1028334X23603620
133. Modelling Mediterranean ocean biogeochemistry of the Last Glacial Maximum K. Six et al. 10.5194/cp-20-1785-2024
134. Challenging the hypothesis of an Arctic Ocean lake during recent glacial episodes C. Hillaire‐Marcel et al. 10.1002/jqs.3421
135. The Glacier‐Climate Interaction Over the Tibetan Plateau and Its Surroundings During the Last Glacial Maximum Q. Wei et al. 10.1029/2023GL103538
136. Contrasting the Penultimate Glacial Maximum and the Last Glacial Maximum (140 and 21 ka) using coupled climate–ice sheet modelling V. Patterson et al. 10.5194/cp-20-2191-2024
137. Environmental evolution of western Tierra del Fuego (∼54°S) since ice-free conditions and its zonal/hemispheric implications P. Moreno et al. 10.1016/j.quascirev.2023.108387
138. A chronological database assessing the late Quaternary palaeoenvironmental record from fluvial sediments in southwestern Africa E. Walsh et al. 10.1016/j.earscirev.2022.104288
139. Modeling the Production of Heinrich Layers With a Sediment‐Enabled Iceberg Model M. Fendrock et al. 10.1029/2022PA004583
140. Glacial AMOC shoaling despite vigorous tidal dissipation: vertical stratification matters Y. Chen et al. 10.5194/cp-20-2001-2024
141. The influence of diagenesis on carbon and oxygen isotope values in shallow water carbonates from the Atlantic and Pacific: Implications for the interpretation of the global carbon cycle M. Smith & P. Swart 10.1016/j.sedgeo.2022.106147
142. 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
143. A new perspective on permafrost boundaries in France during the Last Glacial Maximum K. Stadelmaier et al. 10.5194/cp-17-2559-2021
144. Antarctic surface temperature and elevation during the Last Glacial Maximum C. Buizert et al. 10.1126/science.abd2897
145. A model-based comparison of paleo-physical processes in the Bay of Bengal M. Khan et al. 10.1007/s40808-024-02165-2
146. Analysis of the surface mass balance for deglacial climate simulations M. Kapsch et al. 10.5194/tc-15-1131-2021
147. PMIP4 experiments using MIROC-ES2L Earth system model R. Ohgaito et al. 10.5194/gmd-14-1195-2021
148. Poleward Shift in the Southern Hemisphere Westerly Winds Synchronous With the Deglacial Rise in CO2 W. Gray et al. 10.1029/2023PA004666
149. 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
150. A global climatology of the ocean surface during the Last Glacial Maximum mapped on a regular grid (GLOMAP) A. Paul et al. 10.5194/cp-17-805-2021
151. 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
152. Hysteresis of the Glacial Atlantic Meridional Overturning Circulation Controlled by Thermal Feedbacks T. Ando & A. Oka 10.1029/2021GL095809
153. Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution M. Kapsch et al. 10.1029/2021GL096767
154. A new bias-correction method for precipitation over complex terrain suitable for different climate states: a case study using WRF (version 3.8.1) P. Velasquez et al. 10.5194/gmd-13-5007-2020