112 citations as recorded by crossref.

1. The sensitivity of Northern Hemisphere ice sheets to atmospheric forcing during the last glacial cycle using PMIP3 models L. NIU et al.
2. Contrasting wetland CH4 emission responses to simulated glacial atmospheric CO2 in temperate bogs and fens C. Boardman et al.
3. The atmospheric bridge communicated the δ13C decline during the last deglaciation to the global upper ocean J. Shao et al.
4. Interactions between stationary waves and ice sheets: linear versus nonlinear atmospheric response J. Liakka et al.
5. Applying the Community Ice Sheet Model to evaluate PMIP3 LGM climatologies over the North American ice sheets J. Alder & S. Hostetler
6. A retrospective look at coupled ice sheet–climate modeling D. Pollard
7. Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial P. Tzedakis et al.
8. Fast and slow components of interstadial warming in the North Atlantic during the last glacial V. Margari et al.
9. Paleoglaciological reconstructions for the Tibetan Plateau during the last glacial cycle: evaluating numerical ice sheet simulations driven by GCM-ensembles N. Kirchner et al.
10. Earth surface environmental changes during the last two terminations Y. Yokoyama
11. Modeling the surface mass-balance response of the Laurentide Ice Sheet to Bølling warming and its contribution to Meltwater Pulse 1A A. Carlson et al.
12. Ice sheets as interactive components of Earth System Models: progress and challenges M. Vizcaino
13. Past rapid warmings as a constraint on greenhouse-gas climate feedbacks M. Liu et al.
14. Modelling large-scale ice-sheet–climate interactions following glacial inception J. Gregory et al.
15. Millennial-scale migration of the frozen/melted basal boundary, western Greenland ice sheet A. Stansberry et al.
16. Influence of regional parameters on the surface mass balance of the Eurasian ice sheet during the peak Saalian (140 kya) F. Colleoni et al.
17. Simulating the mid-Pleistocene transition through regolith removal C. Tabor & C. Poulsen
18. Analysis of the surface mass balance for deglacial climate simulations M. Kapsch et al.
19. Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume A. Abe-Ouchi et al.
20. Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al.
21. The sea‐level conundrum: case studies from palaeo‐archives
22. Investigating the evolution of major Northern Hemisphere ice sheets during the last glacial-interglacial cycle S. Bonelli et al.
23. A new global reconstruction of temperature changes at the Last Glacial Maximum J. Annan & J. Hargreaves
24. CO2 drawdown due to particle ballasting by glacial aeolian dust: an estimate based on the ocean carbon cycle model MPIOM/HAMOCC version 1.6.2p3 M. Heinemann et al.
25. Evolution of the large-scale atmospheric circulation in response to changing ice sheets over the last glacial cycle M. Löfverström et al.
26. Deglacial ice sheet meltdown: orbital pacemaking and CO2 effects M. Heinemann et al.
27. Coupled climate-ice sheet modelling of MIS-13 reveals a sensitive Cordilleran Ice Sheet L. Niu et al.
28. 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.
29. Impact of arithmetic asymmetries on simulated thermodynamic ice-sheet evolution F. Saito
30. On the long-term memory of the Greenland Ice Sheet I. Rogozhina et al.
31. On the limited ice intrusion in Alaska at the LGM M. Löfverström & J. Liakka
32. Numerical reconstructions of the penultimate glacial maximum Northern Hemisphere ice sheets: sensitivity to climate forcing and model parameters C. WEKERLE et al.
33. 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.
34. Millennial to orbital-scale variations of drought intensity in the Eastern Mediterranean M. Stockhecke et al.
35. Does a difference in ice sheets between Marine Isotope Stages 3 and 5a affect the duration of stadials? Implications from hosing experiments S. Sherriff-Tadano et al.
36. The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 L. Menviel et al.
37. Stalagmite-inferred European westerly drift in the early Weichselian with centennial-scale variability in marine isotope stage 5a Y. Chung et al.
38. Simulation of the last glacial cycle with a coupled climate ice-sheet model of intermediate complexity A. Ganopolski et al.
39. Rapid Laurentide Ice Sheet growth preceding the Last Glacial Maximum due to summer snowfall L. Niu et al.
40. Dynamic Effect of Last Glacial Maximum Ice Sheet Topography on the East Asian Summer Monsoon Y. Gao et al.
41. Modeling Northern Hemisphere ice-sheet distribution during MIS 5 and MIS 7 glacial inceptions F. Colleoni et al.
42. Clumped‐Isotope Constraint on Upper‐Tropospheric Cooling During the Last Glacial Maximum A. Banerjee et al.
43. “Island” steppes and climate continentality Northeast Asia A. Alfimov & D. Berman
44. The impact of topographically forced stationary waves on local ice-sheet climate J. Liakka & J. Nilsson
45. Dependence of slope lapse rate over the Greenland ice sheet on background climate O. EROKHINA et al.
46. Roles of Sea Ice–Surface Wind Feedback in Maintaining the Glacial Atlantic Meridional Overturning Circulation and Climate S. Sherriff-Tadano & A. Abe-Ouchi
47. A model intercomparison of radiocarbon-based marine reservoir ages during the last 55 kyr including abrupt changes in the Atlantic Meridional Overturning Circulation P. Köhler et al.
48. Present State and Prospects of Ice Sheet and Glacier Modelling H. Blatter et al.
49. Surface‐melt driven Laurentide Ice Sheet retreat during the early Holocene A. Carlson et al.
50. Contrasting the Penultimate Glacial Maximum and the Last Glacial Maximum (140 and 21 ka) using coupled climate–ice sheet modelling V. Patterson et al.
51. Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments A. Abe-Ouchi et al.
52. On the state dependency of the equilibrium climate sensitivity during the last 5 million years P. Köhler et al.
53. Hindcasting the continuum of Dansgaard–Oeschger variability: mechanisms, patterns and timing L. Menviel et al.
54. Quantifying the uncertainty in the Eurasian ice-sheet geometry at the Penultimate Glacial Maximum (Marine Isotope Stage 6) O. Pollard et al.
55. A Comparison of Climate Feedback Strength between CO2 Doubling and LGM Experiments M. Yoshimori et al.
56. The role and potential of Quaternary research in constraining future climate sensitivity M. Yoshimori & A. Abe-Ouchi
57. Atlantic-Pacific seesaw and its role in outgassing CO2during Heinrich events L. Menviel et al.
58. Modeling the evolution of the Juneau Icefield between 1971 and 2100 using the Parallel Ice Sheet Model (PISM) F. ZIEMEN et al.
59. Ice-sheet model sensitivities to environmental forcing and their use in projecting future sea level (the SeaRISE project) R. Bindschadler et al.
60. On the definition of seasons in paleoclimate simulations with orbital forcing O. Timm et al.
61. Abrupt intrinsic and extrinsic responses of southwestern Iberian vegetation to millennial‐scale variability over the past 28 ka A. Cutmore et al.
62. Hypersensitivity of glacial summer temperatures in Siberia P. Bakker et al.
63. Palaeoceanography: motivations and challenges for the future L. Robinson & M. Siddall
64. Enhanced Mid‐depth Southward Transport in the Northeast Atlantic at the Last Glacial Maximum Despite a Weaker AMOC L. Menviel et al.
65. A global analysis of pollen-based reconstructions of land climate changes during Dansgaard–Oeschger events M. Liu et al.
66. Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions M. Petrini et al.
67. Exploring the oxygen isotope fingerprint of Dansgaard-Oeschger variability and Heinrich events W. Bagniewski et al.
68. Modeling Northern Hemispheric Ice Sheet Dynamics, Sea Level Change, and Solid Earth Deformation Through the Last Glacial Cycle H. Han et al.
69. Modelling feedbacks between the Northern Hemisphere ice sheets and climate during the last glacial cycle M. Scherrenberg et al.
70. Interactions between topographically and thermally forced stationary waves: implications for ice-sheet evolution J. Liakka
71. Climate Noise Influences Ice Sheet Mean State L. Niu et al.
72. Equilibrium simulations of Marine Isotope Stage 3 climate C. Guo et al.
73. The impact of model resolution on the simulated Holocene retreat of the southwestern Greenland ice sheet using the Ice Sheet System Model (ISSM) J. Cuzzone et al.
74. Sources of Spread in Multimodel Projections of the Greenland Ice Sheet Surface Mass Balance M. Yoshimori & A. Abe-Ouchi
75. The role of regional feedbacks in glacial inception on Baffin Island: the interaction of ice flow and meteorology L. Birch et al.
76. The North American Cordillera—An Impediment to Growing the Continent-Wide Laurentide Ice Sheet M. Löfverström et al.
77. 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.
78. Poorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data‐model comparison study L. Menviel et al.
79. Impact of mid-glacial ice sheets on deep ocean circulation and global climate S. Sherriff-Tadano et al.
80. Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach E. Bauer & A. Ganopolski
81. The Glimmer community ice sheet model I. Rutt et al.
82. Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks M. Willeit et al.
83. The effect of climate forcing on numerical simulations of the Cordilleran ice sheet at the Last Glacial Maximum J. Seguinot et al.
84. Promotion of glacial ice sheet buildup 60-115 kyr B.P. by precessionally paced Northern Hemispheric meltwater pulses A. Timmermann et al.
85. CO2 radiative forcing and Intertropical Convergence Zone influences on western Pacific warm pool climate over the past 400ka K. Tachikawa et al.
86. A data-calibrated distribution of deglacial chronologies for the North American ice complex from glaciological modeling L. Tarasov et al.
87. Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise L. Menviel et al.
88. GREB-ISM v1.0: A coupled ice sheet model for the Globally Resolved Energy Balance model for global simulations on timescales of 100 kyr Z. Xie et al.
89. Simulating the Early Holocene demise of the Laurentide Ice Sheet with BISICLES (public trunk revision 3298) I. Matero et al.
90. The sensitivity of the Late Saalian (140 ka) and LGM (21 ka) Eurasian ice sheets to sea surface conditions F. Colleoni et al.
91. Attribution of Last Glacial Maximum precipitation change in Northern Hemisphere monsoon and arid regions J. Lei et al.
92. Differences between the last two glacial maxima and implications for ice-sheet, δ18O, and sea-level reconstructions E. Rohling et al.
93. Influence of dynamic vegetation on climate change and terrestrial carbon storage in the Last Glacial Maximum R. O'ishi & A. Abe-Ouchi
94. Western Greenland ice sheet retreat history reveals elevated precipitation during the Holocene thermal maximum J. Downs et al.
95. Eemian Greenland SMB strongly sensitive to model choice A. Plach et al.
96. Millennial atmospheric CO2 changes linked to ocean ventilation modes over past 150,000 years J. Yu et al.
97. Greenland‐Wide Seasonal Temperatures During the Last Deglaciation C. Buizert et al.
98. Modelling the Past and Future Climate by Dr. Syukuro Manabe A. ABE-OUCHI
99. Contribution of enhanced Antarctic Bottom Water formation to Antarctic warm events and millennial-scale atmospheric CO2 increase L. Menviel et al.
100. Mending Milankovitch's theory: obliquity amplification by surface feedbacks C. Tabor et al.
101. Assessing the impact of Laurentide Ice Sheet topography on glacial climate D. Ullman et al.
102. How obliquity cycles powered early Pleistocene global ice‐volume variability C. Tabor et al.
103. High-latitude climate sensitivity to ice-sheet forcing over the last 120kyr J. Singarayer & P. Valdes
104. Modelled response of the volume and thickness of the Antarctic ice sheet to the advance of the grounded area F. Saito & A. Abe-Ouchi
105. Influence of ablation-related processes in the build-up of simulated Northern Hemisphere ice sheets during the last glacial cycle S. Charbit et al.
106. Coupled ice sheet–climate modeling under glacial and pre-industrial boundary conditions F. Ziemen et al.
107. Pre-LGM Northern Hemisphere ice sheet topography J. Kleman et al.
108. A Theory of Orbital-Forced Glacial Cycles: Resolving Pleistocene Puzzles H. Ou
109. Deglacial rapid sea level rises caused by ice-sheet saddle collapses L. Gregoire et al.
110. 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.
111. Influence of glacial ice sheets on the Atlantic meridional overturning circulation through surface wind change S. Sherriff-Tadano et al.
112. The importance of snow albedo for ice sheet evolution over the last glacial cycle M. Willeit & A. Ganopolski