83 citations as recorded by crossref.

1. A brief history of climate – the northern seas from the Last Glacial Maximum to global warming T. Eldevik et al. 10.1016/j.quascirev.2014.06.028
2. Tightened constraints on the time-lag between Antarctic temperature and CO<sub>2</sub> during the last deglaciation J. Pedro et al. 10.5194/cp-8-1213-2012
3. Ice core evidence for decoupling between midlatitude atmospheric water cycle and Greenland temperature during the last deglaciation A. Landais et al. 10.5194/cp-14-1405-2018
4. Assessment of the Greenland ice sheet–atmosphere feedbacks for the next century with a regional atmospheric model coupled to an ice sheet model S. Le clec'h et al. 10.5194/tc-13-373-2019
5. Growth of the Laurentide and Innuitian ice sheets during MIS 5 recorded in distal marine sediment J. Andrews et al. 10.1016/j.quascirev.2024.108532
6. Topography's crucial role in Heinrich Events W. Roberts et al. 10.1073/pnas.1414882111
7. An assessment of basal melt parameterisations for Antarctic ice shelves C. Burgard et al. 10.5194/tc-16-4931-2022
8. Constraint on the penultimate glacial maximum Northern Hemisphere ice topography (≈140 kyrs BP) F. Colleoni et al. 10.1016/j.quascirev.2016.01.024
9. Late Pleistocene boreal molluscs in the Gulf of Cadiz: Past and current oceanographic implications J. Urra et al. 10.1016/j.quascirev.2023.108196
10. Heterogenous westerly shifts linked to Atlantic meridional overturning circulation slowdowns C. Gai et al. 10.1038/s43247-023-00987-z
11. Late Quaternary glaciations in Far NE Russia; combining moraines, topography and chronology to assess regional and global glaciation synchrony I. Barr & C. Clark 10.1016/j.quascirev.2012.08.004
12. Baffin Bay paleoenvironments in the LGM and HS1: Resolving the ice-shelf question A. Jennings et al. 10.1016/j.margeo.2017.09.002
13. Evolution of the central Nordic Seas over the last 20 thousand years M. Telesiński et al. 10.1016/j.quascirev.2015.05.013
14. Ice melt, sea level rise and superstorms: evidence from paleoclimate data, climate modeling, and modern observations that 2 °C global warming could be dangerous J. Hansen et al. 10.5194/acp-16-3761-2016
15. Iceberg discharges of the last glacial period driven by oceanic circulation changes J. Alvarez-Solas et al. 10.1073/pnas.1306622110
16. Ocean-driven millennial-scale variability of the Eurasian ice sheet during the last glacial period simulated with a hybrid ice-sheet–shelf model J. Alvarez-Solas et al. 10.5194/cp-15-957-2019
17. Heinrich event ice discharge and the fate of the Atlantic Meridional Overturning Circulation Y. Zhou & J. McManus 10.1126/science.adh8369
18. The role of ice stream dynamics in deglaciation A. Robel & E. Tziperman 10.1002/2016JF003937
19. Heinrich events show two-stage climate response in transient glacial simulations F. Ziemen et al. 10.5194/cp-15-153-2019
20. Brief communication "Can recent ice discharges following the Larsen-B ice-shelf collapse be used to infer the driving mechanisms of millennial-scale variations of the Laurentide ice sheet?" J. Alvarez-Solas et al. 10.5194/tc-6-687-2012
21. The timing of Mediterranean sapropel deposition relative to insolation, sea-level and African monsoon changes K. Grant et al. 10.1016/j.quascirev.2016.03.026
22. Hydrological responses of the Chihuahua Desert of Mexico to possible Heinrich Stadials J. Quiroz-Jimenez et al. 10.1016/j.jsames.2016.11.001
23. Sedimentary architecture and glacial hydrodynamic significance of the stratified Oak Ridges Moraine, southern Ontario, Canada D. Sharpe & H. Russell 10.1111/bor.12612
24. Modeling the Production of Heinrich Layers With a Sediment‐Enabled Iceberg Model M. Fendrock et al. 10.1029/2022PA004583
25. North Pacific freshwater events linked to changes in glacial ocean circulation E. Maier et al. 10.1038/s41586-018-0276-y
26. The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. 10.5194/cp-18-1579-2022
27. Ocean circulation, ice shelf, and sea ice interactions explain Dansgaard–Oeschger cycles N. Boers et al. 10.1073/pnas.1802573115
28. A new constraint on the size of Heinrich Events from an iceberg/sediment model W. Roberts et al. 10.1016/j.epsl.2013.10.020
29. Frozen fringe explains sediment freeze-on during Heinrich events C. Meyer et al. 10.1016/j.epsl.2019.115725
30. Geochronological database and classification system for age uncertainties in Neotropical pollen records S. Flantua et al. 10.5194/cp-12-387-2016
31. The Atlantic Meridional Overturning Circulation and Abrupt Climate Change J. Lynch-Stieglitz 10.1146/annurev-marine-010816-060415
32. Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day C. Batchelor et al. 10.1038/s41586-023-05876-1
33. Pre-LGM Northern Hemisphere ice sheet topography J. Kleman et al. 10.5194/cp-9-2365-2013
34. Destabilization of glacial climate by the radiative impact of Atlantic Meridional Overturning Circulation disruptions E. Galbraith et al. 10.1002/2016GL069846
35. Subsurface ocean warming preceded Heinrich Events L. Max et al. 10.1038/s41467-022-31754-x
36. Representing icebergs in the <i>i</i>LOVECLIM model (version 1.0) – a sensitivity study M. Bügelmayer et al. 10.5194/gmd-8-2139-2015
37. The role of basal hydrology in the surging of the Laurentide Ice Sheet W. Roberts et al. 10.5194/cp-12-1601-2016
38. Greenland ice sheet contribution to sea level rise during the last interglacial period: a modelling study driven and constrained by ice core data A. Quiquet et al. 10.5194/cp-9-353-2013
39. Ocean-ice sheet interaction along the SE Nordic Seas margin from 35 to 15 ka BP L. Becker et al. 10.1016/j.margeo.2017.09.003
40. Impact of Fjord Geometry on Grounding Line Stability H. Åkesson et al. 10.3389/feart.2018.00071
41. 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
42. The Last Glacial Maximum and Heinrich event I on the Iberian Peninsula: A regional climate modelling study for understanding human settlement patterns P. Ludwig et al. 10.1016/j.gloplacha.2018.08.006
43. Influence of climate on the late Pleistocene depositional history of the Gulf of Gemlik (Sea of Marmara) K. Eriş et al. 10.1007/s00367-019-00568-0
44. Oldest Dryas hydroclimate reorganization in the eastern Iberian Peninsula after the iceberg discharges of Heinrich Event 1 C. Pérez-Mejías et al. 10.1017/qua.2020.112
45. An East Siberian ice shelf during the Late Pleistocene glaciations: Numerical reconstructions F. Colleoni et al. 10.1016/j.quascirev.2015.12.023
46. Relationship between Magdalenian subsistence and environmental change: The mammalian evidence from El Mirón (Spain) G. Cuenca-Bescós et al. 10.1016/j.quaint.2012.04.035
47. Disentangling the roles of late Miocene palaeogeography and vegetation – Implications for climate sensitivity C. Bradshaw et al. 10.1016/j.palaeo.2014.10.003
48. Instability of the Atlantic overturning circulation during Marine Isotope Stage 3 X. Zhang et al. 10.1002/2014GL060321
49. Sensitivity of a Greenland ice sheet model to atmospheric forcing fields A. Quiquet et al. 10.5194/tc-6-999-2012
50. The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing I. Tabone et al. 10.5194/cp-14-455-2018
51. Labrador Current fluctuation during the last glacial cycle L. Mao et al. 10.1016/j.margeo.2017.10.012
52. 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. 10.5194/cp-17-1919-2021
53. 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
54. Ice sheets as interactive components of Earth System Models: progress and challenges M. Vizcaino 10.1002/wcc.285
55. A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets R. Banderas et al. 10.5194/gmd-11-2299-2018
56. 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
57. Glacial onset predated Late Ordovician climate cooling A. Pohl et al. 10.1002/2016PA002928
58. Termination II, Last Glacial Maximum, and Lateglacial chronologies and paleoclimate from Big Cottonwood Canyon, Wasatch Mountains, Utah B. Quirk et al. 10.1130/B31967.1
59. A multi‐proxy analysis of late Quaternary palaeoenvironments, Sekhokong Range, eastern Lesotho J. Fitchett et al. 10.1002/jqs.2902
60. Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions M. Petrini et al. 10.1016/j.quascirev.2020.106314
61. Modeling Northern Hemisphere ice-sheet distribution during MIS 5 and MIS 7 glacial inceptions F. Colleoni et al. 10.5194/cp-10-269-2014
62. Sensitivity of Heinrich-type ice-sheet surge characteristics to boundary forcing perturbations C. Schannwell et al. 10.5194/cp-19-179-2023
63. Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum M. Seidenkrantz et al. 10.1038/s41598-021-86224-z
64. Dansgaard‐Oeschger cycles: Interactions between ocean and sea ice intrinsic to the Nordic seas T. Dokken et al. 10.1002/palo.20042
65. The role of land cover in the climate of glacial Europe P. Velasquez et al. 10.5194/cp-17-1161-2021
66. Interglacials of the last 800,000 years 10.1002/2015RG000482
67. Similarities and dissimilarities between the last two deglaciations and interglaciations in the North Atlantic region B. Martrat et al. 10.1016/j.quascirev.2014.06.016
68. Evidence for an extensive ice shelf in northern Baffin Bay during the Last Glacial Maximum P. Couette et al. 10.1038/s43247-022-00559-7
69. Rainfall response to orbital and millennial forcing in northern Peru over the last 18 ka E. Mollier-Vogel et al. 10.1016/j.quascirev.2013.06.021
70. Regional and global changes during Heinrich Event 1 affecting macrobenthic habitat: Ichnological evidence of sea-bottom conditions at the Galicia Interior Basin F. Rodríguez-Tovar et al. 10.1016/j.gloplacha.2020.103227
71. Modelling North American palaeo-subglacial lakes and their meltwater drainage pathways S. Livingstone et al. 10.1016/j.epsl.2013.04.017
72. Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions F. Colleoni et al. 10.1038/s41598-018-29718-7
73. Temperature-dependent ocean–atmosphere equilibration of carbon isotopes in surface and intermediate waters over the deglaciation J. Lynch-Stieglitz et al. 10.1016/j.epsl.2018.11.024
74. Spatial fingerprint and magnitude of changes in the Atlantic meridional overturning circulation during marine isotope stage 3 X. Zhang et al. 10.1002/2014GL063003
75. Multi‐Proxy Evidence for Atlantic Meridional Overturning Circulation (AMOC) Weakening During Deglaciations of the Past 150,000 Years M. Garity & D. Lund 10.1029/2023PA004629
76. An investigation of the possibility of non-Laurentide ice stream contributions to Heinrich event 3 J. Velay-Vitow et al. 10.1017/qua.2020.84
77. 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
78. 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
79. Anatomy of Heinrich Layer 1 and its role in the last deglaciation D. Hodell et al. 10.1002/2016PA003028
80. Heinrich Events D. Faust et al. 10.1017/qua.2021.2
81. A high‐resolution Lateglacial and Holocene palaeoceanographic record from the Greenland Sea M. Telesiński et al. 10.1111/bor.12045
82. Simulating Heinrich event 1 with interactive icebergs J. Jongma et al. 10.1007/s00382-012-1421-1
83. Capabilities and limitations of numerical ice sheet models: a discussion for Earth-scientists and modelers N. Kirchner et al. 10.1016/j.quascirev.2011.09.012