131 citations as recorded by crossref.

1. Simulating the mid-Pleistocene transition through regolith removal C. Tabor & C. Poulsen 10.1016/j.epsl.2015.11.034
2. The Effect of Obliquity‐Driven Changes on Paleoclimate Sensitivity During the Late Pleistocene P. Köhler et al. 10.1029/2018GL077717
3. Toward generalized Milankovitch theory (GMT) A. Ganopolski 10.5194/cp-20-151-2024
4. The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
5. Milankovitch tuning of deep-sea records: Implications for maximum rates of change of sea level W. Berger 10.1016/j.gloplacha.2012.10.013
6. Ice Sheets and the Anthropocene E. Wolff 10.1144/SP395.10
7. 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
8. On the mechanism of the Middle Pleistocene Transition V. Bol’shakov 10.1134/S0869593815050019
9. Interglacial analogues of the Holocene and its natural near future Q. Yin & A. Berger 10.1016/j.quascirev.2015.04.008
10. Closure of the Bering Strait caused Mid-Pleistocene Transition cooling S. Kender et al. 10.1038/s41467-018-07828-0
11. A Late Pleistocene sea level stack R. Spratt & L. Lisiecki 10.5194/cp-12-1079-2016
12. On the effect of orbital forcing on mid-Pliocene climate, vegetation and ice sheets M. Willeit et al. 10.5194/cp-9-1749-2013
13. Nonlinear response of the Antarctic Ice Sheet to late Quaternary sea level and climate forcing M. Tigchelaar et al. 10.5194/tc-13-2615-2019
14. Effects of eustatic sea-level change, ocean dynamics, and nutrient utilization on atmospheric <i>p</i>CO<sub>2</sub> and seawater composition over the last 130 000 years: a model study K. Wallmann et al. 10.5194/cp-12-339-2016
15. Mediterranean winter rainfall in phase with African monsoons during the past 1.36 million years B. Wagner et al. 10.1038/s41586-019-1529-0
16. Uncertainties originating from GCM downscaling and bias correction with application to the MIS-11c Greenland Ice Sheet B. Crow et al. 10.5194/cp-20-281-2024
17. Modulation of ice ages via precession and dust-albedo feedbacks R. Ellis & M. Palmer 10.1016/j.gsf.2016.04.004
18. The “missing glaciations” of the Middle Pleistocene P. Hughes et al. 10.1017/qua.2019.76
19. Effects of atmospheric CO<sub>2</sub> variability of the past 800 kyr on the biomes of southeast Africa L. Dupont et al. 10.5194/cp-15-1083-2019
20. Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka N. Bouttes et al. 10.1029/2019PA003776
21. The importance of snow albedo for ice sheet evolution over the last glacial cycle M. Willeit & A. Ganopolski 10.5194/cp-14-697-2018
22. The transient impact of the African monsoon on Plio-Pleistocene Mediterranean sediments B. de Boer et al. 10.5194/cp-17-331-2021
23. Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments A. Abe-Ouchi et al. 10.5194/gmd-8-3621-2015
24. Response of the carbon cycle in an intermediate complexity model to the different climate configurations of the last nine interglacials N. Bouttes et al. 10.5194/cp-14-239-2018
25. The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle J. Liakka et al. 10.5194/cp-12-1225-2016
26. Quaternary glaciations: from observations to theories D. Paillard 10.1016/j.quascirev.2014.10.002
27. Driving factors of interglacial paleosol formation on the Chinese loess plateau and the effect of precession and ice sheets K. Ranathunga et al. 10.1016/j.quascirev.2022.107911
28. Coupled Northern Hemisphere permafrost–ice-sheet evolution over the last glacial cycle M. Willeit & A. Ganopolski 10.5194/cp-11-1165-2015
29. Dynamic boreal summer atmospheric circulation response as negative feedback to Greenland melt during the MIS-11 interglacial B. Crow et al. 10.5194/cp-18-775-2022
30. Oscillations in a simple climate–vegetation model J. Rombouts & M. Ghil 10.5194/npg-22-275-2015
31. The role of orbital forcing in the Early Middle Pleistocene Transition M. Maslin & C. Brierley 10.1016/j.quaint.2015.01.047
32. Strong middepth warming and weak radiocarbon imprints in the equatorial Atlantic during Heinrich 1 and Younger Dryas S. Weldeab et al. 10.1002/2016PA002957
33. О НЕКОРРЕКТНОМ ОПРЕДЕЛЕНИИ ПОНЯТИЯ “ТЕОРИЯ МИЛАНКОВИЧА” И ЕГО ВЛИЯНИИ НА РАЗВИТИЕ ОРБИТАЛЬНОЙ ТЕОРИИ ПАЛЕОКЛИМАТА, "Вестник Российской академии наук" В. Большаков 10.7868/S0869587317070064
34. Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume A. Abe-Ouchi et al. 10.1038/nature12374
35. Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al. 10.1038/s43247-023-00765-x
36. Simulating Marine Isotope Stage 7 with a coupled climate–ice sheet model D. Choudhury et al. 10.5194/cp-16-2183-2020
37. On the ill-defined notion of the Milankovitch Theory and its influence on the development of the orbital theory of the paleoclimate V. Bol’shakov 10.1134/S1019331617040025
38. The role of CO2 decline for the onset of Northern Hemisphere glaciation M. Willeit et al. 10.1016/j.quascirev.2015.04.015
39. The “MIS 11 paradox” and ocean circulation: Role of millennial scale events N. Vázquez Riveiros et al. 10.1016/j.epsl.2013.03.036
40. On the Milankovitch sensitivity of the Quaternary deep-sea record W. Berger 10.5194/cp-9-2003-2013
41. The Earth system model CLIMBER-X v1.0 – Part 2: The global carbon cycle M. Willeit et al. 10.5194/gmd-16-3501-2023
42. Nonlinear climate sensitivity and its implications for future greenhouse warming T. Friedrich et al. 10.1126/sciadv.1501923
43. Glacial state of the global carbon cycle: time-slice simulations for the last glacial maximum with an Earth-system model T. Kurahashi-Nakamura et al. 10.5194/cp-18-1997-2022
44. Polar synchronization and the synchronized climatic history of Greenland and Antarctica J. Oh et al. 10.1016/j.quascirev.2013.10.025
45. Diverse manifestations of the mid-Pleistocene climate transition Y. Sun et al. 10.1038/s41467-018-08257-9
46. Precession and atmospheric CO2 modulated variability of sea ice in the central Okhotsk Sea since 130,000 years ago L. Lo et al. 10.1016/j.epsl.2018.02.005
47. Predictable ice ages on a chaotic planet D. Paillard 10.1038/542419a
48. Modelled interglacial carbon cycle dynamics during the Holocene, the Eemian and Marine Isotope Stage (MIS) 11 T. Kleinen et al. 10.5194/cp-12-2145-2016
49. Modeling Obliquity and CO2 Effects on Southern Hemisphere Climate during the Past 408 ka* A. Timmermann et al. 10.1175/JCLI-D-13-00311.1
50. Ice sheet dynamics within an earth system model: downscaling, coupling and first results D. Barbi et al. 10.5194/gmd-7-2003-2014
51. Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions F. Ziemen et al. 10.5194/cp-10-1817-2014
52. Numerical modeling of methane hydrates dissociation in the submarine permafrost V. Malakhova 10.1088/1755-1315/1040/1/012022
53. Beyond bifurcation: using complex models to understand and predict abrupt climate change S. Bathiany et al. 10.1093/climsys/dzw004
54. Exploring the MIS M2 glaciation occurring during a warm and high atmospheric CO2 Pliocene background climate N. Tan et al. 10.1016/j.epsl.2017.04.050
55. Reconstructing the last interglacial at Summit, Greenland: Insights from GISP2 A. Yau et al. 10.1073/pnas.1524766113
56. Modeled Influence of Land Ice and CO2 on Polar Amplification and Paleoclimate Sensitivity During the Past 5 Million Years L. Stap et al. 10.1002/2017PA003313
57. Reconstructing the evolution of ice sheets, sea level, and atmospheric CO<sub>2</sub> during the past 3.6 million years C. Berends et al. 10.5194/cp-17-361-2021
58. Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years R. Uemura et al. 10.1038/s41467-018-03328-3
59. An ice sheet model of reduced complexity for paleoclimate studies B. Neff et al. 10.5194/esd-7-397-2016
60. Evolution of the Laurentide and Innuitian ice sheets prior to the Last Glacial Maximum (115 ka to 25 ka) A. Dalton et al. 10.1016/j.earscirev.2021.103875
61. Using Late Pleistocene sea surface temperature reconstructions to constrain future greenhouse warming T. Friedrich & A. Timmermann 10.1016/j.epsl.2019.115911
62. Bifurcations and strange nonchaotic attractors in a phase oscillator model of glacial–interglacial cycles T. Mitsui et al. 10.1016/j.physd.2015.05.007
63. MIS-11 duration key to disappearance of the Greenland ice sheet A. Robinson et al. 10.1038/ncomms16008
64. Critical insolation–CO2 relation for diagnosing past and future glacial inception A. Ganopolski et al. 10.1038/nature16494
65. The spatial-temporal patterns of East Asian climate in response to insolation, CO2 and ice sheets during MIS-5 A. Lyu & Q. Yin 10.1016/j.quascirev.2022.107689
66. The relative contribution of orbital forcing and greenhouse gases to the North American deglaciation L. Gregoire et al. 10.1002/2015GL066005
67. Evolution of global temperature over the past two million years C. Snyder 10.1038/nature19798
68. On the stability of a climate model for an Earth-like planet with land-ocean coverage T. Alberti et al. 10.1088/2399-6528/aacd8d
69. Ground-ice stable isotopes and cryostratigraphy reflect late Quaternary palaeoclimate in the Northeast Siberian Arctic (Oyogos Yar coast, Dmitry Laptev Strait) T. Opel et al. 10.5194/cp-13-587-2017
70. Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
71. Constraining the Late Pleistocene history of the Laurentide Ice Sheet by dating the Missinaibi Formation, Hudson Bay Lowlands, Canada A. Dalton et al. 10.1016/j.quascirev.2016.06.015
72. 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
73. Orbital insolation variations, intrinsic climate variability, and Quaternary glaciations K. Riechers et al. 10.5194/cp-18-863-2022
74. Carbon isotopes of n-alkanes allow for estimation of the CO2 pressure in the Early Jurassic - A case study from lacustrine shale and cannel boghead in the Dachanggou Basin, Xinjiang, Northwest China J. Wang et al. 10.1016/j.palaeo.2022.111252
75. Adding a dynamical cryosphere to <i>i</i>LOVECLIM (version 1.0): coupling with the GRISLI ice-sheet model D. Roche et al. 10.5194/gmd-7-1377-2014
76. On the Cause of the Mid‐Pleistocene Transition C. Berends et al. 10.1029/2020RG000727
77. The Roles of Orbital and Meltwater Climate Forcings on the Southern Ocean Dynamics during the Last Deglaciation G. Mandal et al. 10.3390/su14052927
78. Comparison and Synthesis of Sea‐Level and Deep‐Sea Temperature Variations Over the Past 40 Million Years E. Rohling et al. 10.1029/2022RG000775
79. Insolation-induced mid-Brunhes transition in Southern Ocean ventilation and deep-ocean temperature Q. Yin 10.1038/nature11790
80. Spiky fluctuations and scaling in high-resolution EPICA ice core dust fluxes S. Lovejoy & F. Lambert 10.5194/cp-15-1999-2019
81. Effects of orbital forcing, greenhouse gases and ice sheets on Saharan greening in past and future multi-millennia M. Duque-Villegas et al. 10.5194/cp-18-1897-2022
82. Effect of Hudson Bay closure on global and regional climate under different astronomical configurations Z. Wu et al. 10.1016/j.gloplacha.2023.104040
83. Interglacials of the last 800,000 years 10.1002/2015RG000482
84. Influence of the choice of insolation forcing on the results of a conceptual glacial cycle model G. Leloup & D. Paillard 10.5194/cp-18-547-2022
85. Eccentricity-induced expansions of Brazilian coastal upwelling zones D. Lessa et al. 10.1016/j.gloplacha.2019.05.002
86. Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach E. Bauer & A. Ganopolski 10.5194/cp-13-819-2017
87. James Croll and geological archives: testing astronomical theories of ice ages P. TZEDAKIS & E. WOLFF 10.1017/S1755691021000177
88. Increased interglacial atmospheric CO2 levels followed the mid-Pleistocene Transition M. Yamamoto et al. 10.1038/s41561-022-00918-1
89. Reduced-complexity model for the impact of anthropogenic CO<sub>2</sub> emissions on future glacial cycles S. Talento & A. Ganopolski 10.5194/esd-12-1275-2021
90. Impact of terrestrial biosphere on the atmospheric CO<sub>2</sub> concentration across Termination V G. Hes et al. 10.5194/cp-18-1429-2022
91. A statistics-based reconstruction of high-resolution global terrestrial climate for the last 800,000 years M. Krapp et al. 10.1038/s41597-021-01009-3
92. Millennial-scale shifts in the methane hydrate stability zone due to Quaternary climate change R. Davies et al. 10.1130/G39611.1
93. Synchronization phenomena observed in glacial–interglacial cycles simulated in an Earth system model of intermediate complexity T. Mitsui et al. 10.5194/esd-14-1277-2023
94. The 100 000-Year Periodicity in Glacial Cycles and Oscillations of World Ocean Level V. Bezverkhnii 10.1134/S0001433819040030
95. Coastal Mountains Amplified the Impacts of Orbital Forcing on East Asian Climate in the Late Cretaceous J. Zhang et al. 10.1029/2023GL105932
96. 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
97. Astronomical forcing of vegetation and climate change during the Late Pliocene–Early Pleistocene of the Nihewan Basin, North China Z. Zhang et al. 10.1016/j.quaint.2021.07.017
98. Dynamic regimes of the Greenland Ice Sheet emerging from interacting melt–elevation and glacial isostatic adjustment feedbacks M. Zeitz et al. 10.5194/esd-13-1077-2022
99. Snyder replies C. Snyder 10.1038/nature22804
100. Ice Complex formation on Bol'shoy Lyakhovsky Island (New Siberian Archipelago, East Siberian Arctic) since about 200 ka S. Wetterich et al. 10.1017/qua.2019.6
101. On Quaternary glaciations, observations and theories D. Paillard 10.1016/j.quascirev.2015.05.017
102. Deglacial ice sheet meltdown: orbital pacemaking and CO<sub>2</sub> effects M. Heinemann et al. 10.5194/cp-10-1567-2014
103. Drivers of river reactivation in North Africa during the last glacial cycle C. Blanchet et al. 10.1038/s41561-020-00671-3
104. Interaction of ice sheets and climate during the past 800 000 years L. Stap et al. 10.5194/cp-10-2135-2014
105. A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets R. Banderas et al. 10.5194/gmd-11-2299-2018
106. Comment on “Quaternary glaciations: from observations to theories” by D. Paillard [Quat. Sci. Rev. 107 (2015), 11–24] V. Bol'shakov & Y. Kuzmin 10.1016/j.quascirev.2015.03.001
107. Exponential feedback effects in a parametric resonance climate model M. Caccamo & S. Magazù 10.1038/s41598-023-50350-7
108. The influence of ice sheets on temperature during the past 38 million years inferred from a one-dimensional ice sheet–climate model L. Stap et al. 10.5194/cp-13-1243-2017
109. Northeast Siberian Permafrost Ice‐Wedge Stable Isotopes Depict Pronounced Last Glacial Maximum Winter Cooling S. Wetterich et al. 10.1029/2020GL092087
110. Modeling the Greenland englacial stratigraphy A. Born & A. Robinson 10.5194/tc-15-4539-2021
111. Mid-Pleistocene transition in glacial cycles explained by declining CO 2 and regolith removal M. Willeit et al. 10.1126/sciadv.aav7337
112. 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
113. The importance of insolation changes for paleo ice sheet modeling A. Robinson & H. Goelzer 10.5194/tc-8-1419-2014
114. Simulating the Greenland ice sheet under present-day and palaeo constraints including a new discharge parameterization R. Calov et al. 10.5194/tc-9-179-2015
115. Revised estimates of paleoclimate sensitivity over the past 800,000 years C. Snyder 10.1007/s10584-019-02536-0
116. Hydrographic variations in deep ocean temperature over the mid-Pleistocene transition S. Bates et al. 10.1016/j.quascirev.2014.01.020
117. Sensitivity simulations with direct shortwave radiative forcing by aeolian dust during glacial cycles E. Bauer & A. Ganopolski 10.5194/cp-10-1333-2014
118. Causes of ice age intensification across the Mid-Pleistocene Transition T. Chalk et al. 10.1073/pnas.1702143114
119. Hemisphere differences in response of sea surface temperature and sea ice to precession and obliquity Z. Wu et al. 10.1016/j.gloplacha.2020.103223
120. The role of regional feedbacks in glacial inception on Baffin Island: the interaction of ice flow and meteorology L. Birch et al. 10.5194/cp-14-1441-2018
121. Orbital Asian summer monsoon dynamics revealed using an isotope-enabled global climate model T. Caley et al. 10.1038/ncomms6371
122. Simulation of the future sea level contribution of Greenland with a new glacial system model R. Calov et al. 10.5194/tc-12-3097-2018
123. Millennial to orbital-scale variations of drought intensity in the Eastern Mediterranean M. Stockhecke et al. 10.1016/j.quascirev.2015.12.016
124. Orbital forcing of aridity/humidity fluctuations in the Hexi Corridor and Alxa Plateau, NW China, during the last 1.8 million years D. Chen et al. 10.1016/j.palaeo.2024.112204
125. A simple rule to determine which insolation cycles lead to interglacials P. Tzedakis et al. 10.1038/nature21364
126. Simulation of climate, ice sheets and CO<sub>2</sub> evolution during the last four glacial cycles with an Earth system model of intermediate complexity A. Ganopolski & V. Brovkin 10.5194/cp-13-1695-2017
127. Forcing of late Pleistocene ice volume by spatially variable summer energy K. Haaga et al. 10.1038/s41598-018-29916-3
128. Bispectra of climate cycles show how ice ages are fuelled D. Liebrand & A. de Bakker 10.5194/cp-15-1959-2019
129. Different environmental variables predict body and brain size evolution in Homo M. Will et al. 10.1038/s41467-021-24290-7
130. Late Pleistocene climate drivers of early human migration A. Timmermann & T. Friedrich 10.1038/nature19365
131. Palaeoceanography: motivations and challenges for the future L. Robinson & M. Siddall 10.1098/rsta.2012.0396