164 citations as recorded by crossref.

1. Reduced Stability of the Atlantic Meridional Overturning Circulation due to Wind Stress Feedback during Glacial Times O. Arzel et al. 10.1175/2008JCLI2291.1
2. Wetland methane emissions during the Last Glacial Maximum estimated from PMIP2 simulations: Climate, vegetation, and geographic controls S. Weber et al. 10.1029/2009JD012110
3. Modelling the enigmatic Late Pliocene Glacial Event — Marine Isotope Stage M2 A. Dolan et al. 10.1016/j.gloplacha.2015.02.001
4. Simulated effects of interactions between ocean acidification, marine organism calcification, and organic carbon export on ocean carbon and oxygen cycles H. Zhang & L. Cao 10.1007/s11430-017-9173-y
5. On the relationships between features of the depth–latitude meridional overturning streamfunctions across global coupled climate models Y. Plancherel 10.1007/s00382-013-1984-5
6. Ancient divergence and recent population expansion in a leaf frog endemic to the southern Brazilian Atlantic forest T. Brunes et al. 10.1007/s13127-015-0228-4
7. 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
8. Multicentury Instability of the Atlantic Meridional Circulation in Rapid Warming Simulations With GISS ModelE2 D. Rind et al. 10.1029/2017JD027149
9. Are paleoclimate model ensembles consistent with the MARGO data synthesis? J. Hargreaves et al. 10.5194/cp-7-917-2011
10. Carbon-nitrogen feedbacks in the UVic ESCM R. Wania et al. 10.5194/gmd-5-1137-2012
11. Signature of the Gold Cove event (10.2 ka) in the Labrador Sea H. Rashid et al. 10.1016/j.quaint.2014.06.063
12. 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
13. Interaction of ice sheets and climate during the past 800 000 years L. Stap et al. 10.5194/cp-10-2135-2014
14. Set-up of the PMIP3 paleoclimate experiments conducted using an Earth system model, MIROC-ESM T. Sueyoshi et al. 10.5194/gmd-6-819-2013
15. A grip on ice-age ocean circulation J. Marotzke 10.1038/485180a
16. Lifetime of Anthropogenic Climate Change: Millennial Time Scales of Potential CO2 and Surface Temperature Perturbations M. Eby et al. 10.1175/2008JCLI2554.1
17. Icebergs not the trigger for North Atlantic cold events S. Barker et al. 10.1038/nature14330
18. Impacts of land surface properties and atmospheric CO<sub>2</sub> on the Last Glacial Maximum climate: a factor separation analysis A. Henrot et al. 10.5194/cp-5-183-2009
19. Recent Contributions of Theory to Our Understanding of the Atlantic Meridional Overturning Circulation H. Johnson et al. 10.1029/2019JC015330
20. North Atlantic Deep Water Production during the Last Glacial Maximum J. Howe et al. 10.1038/ncomms11765
21. Can you step twice into the same river? Climate change through time: Abridged text of the inaugural address as professor in Climate Modelling and Analysis at the Faculty of Geosciences of Utrecht University held on 29 February 2008 S. Weber 10.1017/S0016774600023325
22. Antarctic intermediate water circulation in the South Atlantic over the past 25,000 years J. Howe et al. 10.1002/2016PA002975
23. Atmosphere and ocean dynamics: contributors to the European Little Ice Age? V. Palastanga et al. 10.1007/s00382-010-0751-0
24. Simulating atmospheric CO2, 13C and the marine carbon cycle during the Last Glacial–Interglacial cycle: possible role for a deepening of the mean remineralization depth and an increase in the oceanic nutrient inventory L. Menviel et al. 10.1016/j.quascirev.2012.09.012
25. Surface wind‐stress threshold for glacial Atlantic overturning M. Montoya & A. Levermann 10.1029/2007GL032560
26. The Time-Dependent Response of a Two-Basin Ocean to a Sudden Surface Temperature Change C. Chang & M. Jansen 10.1175/JCLI-D-21-0821.1
27. Northern-sourced water dominated the Atlantic Ocean during the Last Glacial Maximum F. Pöppelmeier et al. 10.1130/G47628.1
28. PMIP4 experiments using MIROC-ES2L Earth system model R. Ohgaito et al. 10.5194/gmd-14-1195-2021
29. Effects of the Bering Strait closure on AMOC and global climate under different background climates A. Hu et al. 10.1016/j.pocean.2014.02.004
30. A review of recent developments in climate change science. Part I: Understanding of future change in the large-scale climate system P. Good et al. 10.1177/0309133311407651
31. 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
32. Crossing the threshold 10.1038/nclimate1288
33. On the glacial and interglacial thermohaline circulation and the associated transports of heat and freshwater M. Ballarotta et al. 10.5194/os-10-907-2014
34. Transient Simulation of Last Deglaciation with a New Mechanism for Bølling-Allerød Warming Z. Liu et al. 10.1126/science.1171041
35. Rain driven by receding ice sheets as a cause of past climate change I. Eisenman et al. 10.1029/2009PA001778
36. Mechanisms controlling export production at the LGM: Effects of changes in oceanic physical fields and atmospheric dust deposition A. Oka et al. 10.1029/2009GB003628
37. Evaluating Southern Ocean sea-ice for the Last Glacial Maximum and pre-industrial climates: PMIP-2 models and data evidence D. Roche et al. 10.1016/j.quascirev.2012.09.020
38. Last glacial maximum (LGM) primary productivity in the northern North Atlantic OceanThis article is one of a series of papers published in this Special Issue on the theme Polar Climate Stability Network. P. Hollings et al. 10.1139/E08-059
39. The Impact of Wind Stress Feedback on the Stability of the Atlantic Meridional Overturning Circulation O. Arzel et al. 10.1175/2010JCLI3137.1
40. The Role of African Dust in Atlantic Climate During Heinrich Events L. Murphy et al. 10.1002/2017PA003150
41. A perspective on model-data surface temperature comparison at the Last Glacial Maximum J. Annan & J. Hargreaves 10.1016/j.quascirev.2014.09.019
42. A salty deep ocean as a prerequisite for glacial termination G. Knorr et al. 10.1038/s41561-021-00857-3
43. The utility of Earth system Models of Intermediate Complexity (EMICs) S. Weber 10.1002/wcc.24
44. Transient versus Equilibrium Response of the Ocean’s Overturning Circulation to Warming M. Jansen et al. 10.1175/JCLI-D-17-0797.1
45. 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
46. Glacial ocean circulation and stratification explained by reduced atmospheric temperature M. Jansen 10.1073/pnas.1610438113
47. Response of Thermohaline Circulation to Freshwater Forcing under Present-Day and LGM Conditions A. Hu et al. 10.1175/2007JCLI1985.1
48. Helium isotopic constraints on simulated ocean circulations: implications for abyssal theories J. Dutay et al. 10.1007/s10652-009-9159-y
49. Transient and Equilibrium Responses of the Atlantic Overturning Circulation to Warming in Coupled Climate Models: The Role of Temperature and Salinity D. Bonan et al. 10.1175/JCLI-D-21-0912.1
50. Response of the South Atlantic circulation to an abrupt collapse of the Atlantic meridional overturning circulation A. Laurian & S. Drijfhout 10.1007/s00382-010-0890-3
51. Sensitivity of the glacial ocean to Heinrich events from different iceberg sources, as modeled by a coupled atmosphere‐iceberg‐ocean model R. Levine & G. Bigg 10.1029/2008PA001613
52. Last Glacial Maximum ocean thermohaline circulation: PMIP2 model intercomparisons and data constraints B. Otto‐Bliesner et al. 10.1029/2007GL029475
53. Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle, precipitation A. Laîné et al. 10.1007/s00382-008-0391-9
54. Ocean methane hydrates as a slow tipping point in the global carbon cycle D. Archer et al. 10.1073/pnas.0800885105
55. The simulated climate of the Last Glacial Maximum and insights into the global marine carbon cycle P. Buchanan et al. 10.5194/cp-12-2271-2016
56. 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
57. Geometry of the Meridional Overturning Circulation at the Last Glacial Maximum F. Pavia et al. 10.1175/JCLI-D-21-0671.1
58. Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO<sub>2</sub> decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al. 10.5194/cp-15-1039-2019
59. Using Single-Forcing GCM Simulations to Reconstruct and Interpret Quaternary Climate Change M. Erb et al. 10.1175/JCLI-D-15-0329.1
60. Atlantic overturning responses to Late Pleistocene climate forcings L. Lisiecki et al. 10.1038/nature07425
61. Assessing the potential capability of reconstructing glacial Atlantic water masses and AMOC using multiple proxies in CESM S. Gu et al. 10.1016/j.epsl.2020.116294
62. Antarctic density stratification and the strength of the circumpolar current during the Last Glacial Maximum J. Lynch-Stieglitz et al. 10.1002/2015PA002915
63. Poorly ventilated deep ocean at the Last Glacial Maximum inferred from carbon isotopes: A data‐model comparison study L. Menviel et al. 10.1002/2016PA003024
64. Modelling abrupt glacial North Atlantic freshening: Rates of change and their implications for Heinrich events G. Bigg et al. 10.1016/j.gloplacha.2010.11.001
65. Hydrographic biases in global coupled climate models and their relation to the meridional overturning circulation Y. Plancherel 10.1007/s00382-014-2263-9
66. Causes of the weak emergent constraint on climate sensitivity at the Last Glacial Maximum M. Renoult et al. 10.5194/cp-19-323-2023
67. Impact of transient freshwater releases in the Southern Ocean on the AMOC and climate D. Swingedouw et al. 10.1007/s00382-008-0496-1
68. Arctic Oscillation during the Mid-Holocene and Last Glacial Maximum from PMIP2 Coupled Model Simulations J. Lü et al. 10.1175/2010JCLI3331.1
69. Overlooked possibility of a collapsed Atlantic Meridional Overturning Circulation in warming climate W. Liu et al. 10.1126/sciadv.1601666
70. Modeling the climatic implications and indicative senses of the Guliya δ<sup>18</sup>O-temperature proxy record to the ocean–atmosphere system during the past 130 ka D. Xiao et al. 10.5194/cp-9-735-2013
71. East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum Z. Song et al. 10.1029/2019GL082960
72. The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. 10.1029/2020PA004068
73. Setting cumulative emissions targets to reduce the risk of dangerous climate change K. Zickfeld et al. 10.1073/pnas.0805800106
74. Assessing the stability of the Atlantic meridional overturning circulation of the past, present, and future W. Liu & Z. Liu 10.1007/s13351-014-4006-6
75. 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
76. 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
77. Why is the AMOC Monostable in Coupled General Circulation Models? W. Liu et al. 10.1175/JCLI-D-13-00264.1
78. 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
79. Evolution of the Asian–African Monsoonal Precipitation over the last 21 kyr and the Associated Dynamic Mechanisms J. Shi & Q. Yan 10.1175/JCLI-D-19-0074.1
80. Heinrich events show two-stage climate response in transient glacial simulations F. Ziemen et al. 10.5194/cp-15-153-2019
81. Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using <i>δ</i><sup>13</sup>C A. Morée et al. 10.5194/cp-17-753-2021
82. Circulation adjustment in the Arctic and Atlantic in response to Greenland and Antarctic mass loss J. Berk et al. 10.1007/s00382-021-05755-3
83. On the stability of the Atlantic meridional overturning circulation M. Hofmann & S. Rahmstorf 10.1073/pnas.0909146106
84. Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? M. Ballarotta et al. 10.5194/cp-9-2669-2013
85. 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
86. Glacial mode shift of the Atlantic meridional overturning circulation by warming over the Southern Ocean A. Oka et al. 10.1038/s43247-021-00226-3
87. Potential climatic transitions with profound impact on Europe A. Levermann et al. 10.1007/s10584-011-0126-5
88. Instability of Atlantic Meridional Overturning Circulation: Observations, Modelling and Relevance to Present and Future Z. Liu 10.3390/atmos14061011
89. Modelling the Antarctic marine cryosphere at the Last Glacial Maximum K. Kusahara et al. 10.3189/2015AoG69A792
90. Stability of the Atlantic Meridional Overturning Circulation: A Review and Synthesis W. Weijer et al. 10.1029/2019JC015083
91. Elemental proxies for paleosalinity analysis of ancient shales and mudrocks W. Wei & T. Algeo 10.1016/j.gca.2019.06.034
92. Separating Direct Heat Flux Forcing and Freshwater Feedback on AMOC Change Under Global Warming Q. Wen et al. 10.1029/2023GL105478
93. CO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilization D. Lunt et al. 10.1130/G31184.1
94. Paleophysical Oceanography with an Emphasis on Transport Rates P. Huybers & C. Wunsch 10.1146/annurev-marine-120308-081056
95. The LGM surface climate and atmospheric circulation over East Asia and the North Pacific in the PMIP2 coupled model simulations W. Yanase & A. Abe-Ouchi 10.5194/cp-3-439-2007
96. Parameterizing the fresh-water flux from land ice to ocean with interactive icebergs in a coupled climate model T. Martin & A. Adcroft 10.1016/j.ocemod.2010.05.001
97. Global climate simulations at 3000-year intervals for the last 21 000 years with the GENMOM coupled atmosphere–ocean model J. Alder & S. Hostetler 10.5194/cp-11-449-2015
98. A comparison of PMIP2 model simulations and the MARGO proxy reconstruction for tropical sea surface temperatures at last glacial maximum B. Otto-Bliesner et al. 10.1007/s00382-008-0509-0
99. Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 1: experiments and large-scale features P. Braconnot et al. 10.5194/cp-3-261-2007
100. Quantifying the ocean's role in glacial CO<sub>2</sub> reductions M. Chikamoto et al. 10.5194/cp-8-545-2012
101. Simulated CO2-induced ocean acidification for ocean in the East China: historical conditions since preindustrial time and future scenarios H. Zhang & K. Wang 10.1038/s41598-019-54861-0
102. How much did Glacial North Atlantic Water shoal? G. Gebbie 10.1002/2013PA002557
103. Atmospheric Lifetime of Fossil Fuel Carbon Dioxide D. Archer et al. 10.1146/annurev.earth.031208.100206
104. Glacial climate sensitivity to different states of the Atlantic Meridional Overturning Circulation: results from the IPSL model M. Kageyama et al. 10.5194/cp-5-551-2009
105. A Dynamical Reconstruction of the Global Monthly Mean Oxygen Isotopic Composition of Seawater C. Breitkreuz et al. 10.1029/2018JC014300
106. Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation X. Zhang et al. 10.5194/cp-9-2319-2013
107. Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study H. Zhang et al. 10.1088/2515-7620/aca9ac
108. Deglacial change of Antarctic Bottom Water in transient simulations C. Zhu 10.1016/j.aosl.2023.100333
109. How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? – Perspectives from equilibrium simulations C. Van Meerbeeck et al. 10.5194/cp-5-33-2009
110. Extreme deepening of the Atlantic overturning circulation during deglaciation S. Barker et al. 10.1038/ngeo921
111. Nonlinear Response of Global Monsoon Precipitation to Atlantic Overturning Strength Variations During Marine Isotope Stage 3 X. Zhang et al. 10.1029/2023JD038521
112. The roles of barriers, refugia, and chromosomal clines underlying diversification in Atlantic Forest social wasps R. Menezes et al. 10.1038/s41598-017-07776-7
113. High-latitude climate sensitivity to ice-sheet forcing over the last 120kyr J. Singarayer & P. Valdes 10.1016/j.quascirev.2009.10.011
114. Bathymetric controls on Pliocene North Atlantic and Arctic sea surface temperature and deepwater production M. Robinson et al. 10.1016/j.palaeo.2011.01.004
115. On the stability of the Atlantic meridional overturning circulation during the last deglaciation W. Liu et al. 10.1007/s00382-014-2153-1
116. Impact of a realistic river routing in coupled ocean–atmosphere simulations of the Last Glacial Maximum climate R. Alkama et al. 10.1007/s00382-007-0330-1
117. Control of the glacial carbon budget by topographically induced mixing A. De Boer & A. Hogg 10.1002/2014GL059963
118. Impact of Freshwater Release in the North Atlantic under Different Climate Conditions in an OAGCM D. Swingedouw et al. 10.1175/2009JCLI3028.1
119. Evaluating climate model performance with various parameter sets using observations over the recent past M. Loutre et al. 10.5194/cp-7-511-2011
120. The key role of topography in altering North Atlantic atmospheric circulation during the last glacial period F. Pausata et al. 10.5194/cp-7-1089-2011
121. Description of the Earth system model of intermediate complexity LOVECLIM version 1.2 H. Goosse et al. 10.5194/gmd-3-603-2010
122. 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
123. A Coupled Dynamical Ocean–Energy Balance Atmosphere Model for Paleoclimate Studies S. Ritz et al. 10.1175/2010JCLI3351.1
124. Early Interglacial Legacy of Deglacial Climate Instability S. Barker et al. 10.1029/2019PA003661
125. Oxygen stable isotopes during the Last Glacial Maximum climate: perspectives from data–model (<i>i</i>LOVECLIM) comparison T. Caley et al. 10.5194/cp-10-1939-2014
126. Observable, low-order dynamical controls on thresholds of the Atlantic meridional overturning circulation R. Wood et al. 10.1007/s00382-019-04956-1
127. Responses of the summer Asian-Pacific zonal thermal contrast and the associated evolution of atmospheric circulation to transient orbital changes during the Holocene D. Xiao et al. 10.1038/srep35816
128. Atlantic overturning responses to obliquity and precession over the last 3 Myr L. Lisiecki 10.1002/2013PA002505
129. Lowering of glacial atmospheric CO2 in response to changes in oceanic circulation and marine biogeochemistry V. Brovkin et al. 10.1029/2006PA001380
130. Ocean carbon uptake and storage influenced by wind bias in global climate models N. Swart & J. Fyfe 10.1038/nclimate1289
131. A Diagnostic Indicator of the Stability of the Atlantic Meridional Overturning Circulation in CCSM3 W. Liu & Z. Liu 10.1175/JCLI-D-11-00681.1
132. Assessing the impact of Laurentide Ice Sheet topography on glacial climate D. Ullman et al. 10.5194/cp-10-487-2014
133. Global-Scale Energy and Freshwater Balance in Glacial Climate: A Comparison of Three PMIP2 LGM Simulations S. Murakami et al. 10.1175/2008JCLI2104.1
134. Can we use ice sheet reconstructions to constrain meltwater for deglacial simulations? I. Bethke et al. 10.1029/2011PA002258
135. Stability of the Atlantic Meridional Overturning Circulation in the Last Glacial Maximum climate S. Weber & S. Drijfhout 10.1029/2007GL031437
136. Evaluation of climate models using palaeoclimatic data P. Braconnot et al. 10.1038/nclimate1456
137. Dansgaard‐Oeschger oscillations predicted in a comprehensive model of glacial climate: A “kicked” salt oscillator in the Atlantic W. Peltier & G. Vettoretti 10.1002/2014GL061413
138. Glacial Atlantic overturning increased by wind stress in climate models J. Muglia & A. Schmittner 10.1002/2015GL064583
139. Glacial Ice Sheet Extent Effects on Modeled Tidal Mixing and the Global Overturning Circulation S. Wilmes et al. 10.1029/2019PA003644
140. Quantitative estimate of the paleo‐Agulhas leakage T. Caley et al. 10.1002/2014GL059278
141. Impact of mid-glacial ice sheets on deep ocean circulation and global climate S. Sherriff-Tadano et al. 10.5194/cp-17-95-2021
142. An Indicator of the Multiple Equilibria Regime of the Atlantic Meridional Overturning Circulation S. Huisman et al. 10.1175/2009JPO4215.1
143. Higher Laurentide and Greenland ice sheets strengthen the North Atlantic ocean circulation X. Gong et al. 10.1007/s00382-015-2502-8
144. Modeling water isotopologues during the last glacial: Implications for quantitative paleosalinity reconstruction T. Caley & D. Roche 10.1002/2014PA002720
145. A probabilistic calibration of climate sensitivity and terrestrial carbon change in GENIE-1 P. Holden et al. 10.1007/s00382-009-0630-8
146. The Stability of the AMOC During Heinrich Events Is Not Dependent on the AMOC Strength in an Intermediate Complexity Earth System Model Ensemble M. Goes et al. 10.1029/2019PA003580
147. Direct astronomical influence on abrupt climate variability X. Zhang et al. 10.1038/s41561-021-00846-6
148. The Ordovician ocean circulation: a modern synthesis based on data and models A. Pohl et al. 10.1144/SP532-2022-1
149. Modeled seasonality of glacial abrupt climate events J. Flückiger et al. 10.1007/s00382-008-0373-y
150. Can sparse proxy data constrain the strength of the Atlantic meridional overturning circulation? T. Kurahashi-Nakamura et al. 10.5194/gmd-7-419-2014
151. The stability of the MOC as diagnosed from model projections for pre-industrial, present and future climates S. Drijfhout et al. 10.1007/s00382-010-0930-z
152. The Southern Annular Mode (SAM) in PMIP2 simulations of the last glacial maximum S. Kim et al. 10.1007/s00376-013-3179-8
153. Plankton reveal past climate M. Robinson 10.1038/s41561-023-01343-8
154. How well would modern‐day oceanic property distributions be known with paleoceanographic‐like observations? G. Gebbie et al. 10.1002/2015PA002917
155. How cold was Europe at the Last Glacial Maximum? A synthesis of the progress achieved since the first PMIP model-data comparison G. Ramstein et al. 10.5194/cp-3-331-2007
156. Carbon‐cycle feedbacks of changes in the Atlantic meridional overturning circulation under future atmospheric CO2 K. Zickfeld et al. 10.1029/2007GB003118
157. Fast Physics and Slow Physics in the Nonlinear Dansgaard–Oeschger Relaxation Oscillation G. Vettoretti & W. Peltier 10.1175/JCLI-D-17-0559.1
158. LGM hosing approach to Heinrich Event 1: results and perspectives from data–model integration using water isotopes D. Roche et al. 10.1016/j.quascirev.2014.07.020
159. Phylogeography of endemic toads and post-Pliocene persistence of the Brazilian Atlantic Forest M. Thomé et al. 10.1016/j.ympev.2010.02.003
160. Comparing transient, accelerated, and equilibrium simulations of the last 30 000 years with the GENIE-1 model D. Lunt et al. 10.5194/cp-2-221-2006
161. Long term climate implications of 2050 emission reduction targets A. Weaver et al. 10.1029/2007GL031018
162. Assessing the sensitivity of the North Atlantic Ocean circulation to freshwater perturbation in various glacial climate states C. Van Meerbeeck et al. 10.1007/s00382-011-1043-z
163. A systematic study of the impact of freshwater pulses with respect to different geographical locations D. Roche et al. 10.1007/s00382-009-0578-8
164. Climate of the Last Glacial Maximum: sensitivity studies and model-data comparison with the LOVECLIM coupled model D. Roche et al. 10.5194/cp-3-205-2007