88 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. https://doi.org/10.1016/j.quascirev.2014.06.028
2. Tightened constraints on the time-lag between Antarctic temperature and CO2 during the last deglaciation J. Pedro et al. https://doi.org/10.5194/cp-8-1213-2012
3. Growth of the Laurentide and Innuitian ice sheets during MIS 5 recorded in distal marine sediment J. Andrews et al. https://doi.org/10.1016/j.quascirev.2024.108532
4. An assessment of basal melt parameterisations for Antarctic ice shelves C. Burgard et al. https://doi.org/10.5194/tc-16-4931-2022
5. Constraint on the penultimate glacial maximum Northern Hemisphere ice topography (≈140 kyrs BP) F. Colleoni et al. https://doi.org/10.1016/j.quascirev.2016.01.024
6. Heterogenous westerly shifts linked to Atlantic meridional overturning circulation slowdowns C. Gai et al. https://doi.org/10.1038/s43247-023-00987-z
7. 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. https://doi.org/10.5194/acp-16-3761-2016
8. 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. https://doi.org/10.5194/cp-15-957-2019
9. Millennial-to multi-centennial-scale Asian summer monsoon variability during Termination I: Evidence from stalagmite δ18O in Wanxiang Cave, northwestern China H. Shi et al. https://doi.org/10.1016/j.quascirev.2026.110168
10. Heinrich events show two-stage climate response in transient glacial simulations F. Ziemen et al. https://doi.org/10.5194/cp-15-153-2019
11. 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. https://doi.org/10.5194/tc-6-687-2012
12. Ocean circulation, ice shelf, and sea ice interactions explain Dansgaard–Oeschger cycles N. Boers et al. https://doi.org/10.1073/pnas.1802573115
13. Geochronological database and classification system for age uncertainties in Neotropical pollen records S. Flantua et al. https://doi.org/10.5194/cp-12-387-2016
14. The Atlantic Meridional Overturning Circulation and Abrupt Climate Change J. Lynch-Stieglitz https://doi.org/10.1146/annurev-marine-010816-060415
15. Pre-LGM Northern Hemisphere ice sheet topography J. Kleman et al. https://doi.org/10.5194/cp-9-2365-2013
16. Representing icebergs in the iLOVECLIM model (version 1.0) – a sensitivity study M. Bügelmayer et al. https://doi.org/10.5194/gmd-8-2139-2015
17. Ocean-ice sheet interaction along the SE Nordic Seas margin from 35 to 15 ka BP L. Becker et al. https://doi.org/10.1016/j.margeo.2017.09.003
18. The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. https://doi.org/10.1029/2020PA004068
19. 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. https://doi.org/10.1016/j.gloplacha.2018.08.006
20. Influence of climate on the late Pleistocene depositional history of the Gulf of Gemlik (Sea of Marmara) K. Eriş et al. https://doi.org/10.1007/s00367-019-00568-0
21. Geomorphology of the northeast Sardinian continental shelf between Olbia and Posada (Italy) M. De Luca et al. https://doi.org/10.1080/17445647.2024.2446249
22. Oldest Dryas hydroclimate reorganization in the eastern Iberian Peninsula after the iceberg discharges of Heinrich Event 1 C. Pérez-Mejías et al. https://doi.org/10.1017/qua.2020.112
23. An East Siberian ice shelf during the Late Pleistocene glaciations: Numerical reconstructions F. Colleoni et al. https://doi.org/10.1016/j.quascirev.2015.12.023
24. Sensitivity of a Greenland ice sheet model to atmospheric forcing fields A. Quiquet et al. https://doi.org/10.5194/tc-6-999-2012
25. 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. https://doi.org/10.5194/cp-17-1919-2021
26. A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets R. Banderas et al. https://doi.org/10.5194/gmd-11-2299-2018
27. State dependence of climatic instability over the past 720,000 years from Antarctic ice cores and climate modeling K. Kawamura et al. https://doi.org/10.1126/sciadv.1600446
28. Glacial onset predated Late Ordovician climate cooling A. Pohl et al. https://doi.org/10.1002/2016PA002928
29. Termination II, Last Glacial Maximum, and Lateglacial chronologies and paleoclimate from Big Cottonwood Canyon, Wasatch Mountains, Utah B. Quirk et al. https://doi.org/10.1130/B31967.1
30. A multi‐proxy analysis of late Quaternary palaeoenvironments, Sekhokong Range, eastern Lesotho J. Fitchett et al. https://doi.org/10.1002/jqs.2902
31. Simulated last deglaciation of the Barents Sea Ice Sheet primarily driven by oceanic conditions M. Petrini et al. https://doi.org/10.1016/j.quascirev.2020.106314
32. Sensitivity of Heinrich-type ice-sheet surge characteristics to boundary forcing perturbations C. Schannwell et al. https://doi.org/10.5194/cp-19-179-2023
33. Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum M. Seidenkrantz et al. https://doi.org/10.1038/s41598-021-86224-z
34. The role of land cover in the climate of glacial Europe P. Velasquez et al. https://doi.org/10.5194/cp-17-1161-2021
35. Evidence for an extensive ice shelf in northern Baffin Bay during the Last Glacial Maximum P. Couette et al. https://doi.org/10.1038/s43247-022-00559-7
36. Modelling North American palaeo-subglacial lakes and their meltwater drainage pathways S. Livingstone et al. https://doi.org/10.1016/j.epsl.2013.04.017
37. Temperature-dependent ocean–atmosphere equilibration of carbon isotopes in surface and intermediate waters over the deglaciation J. Lynch-Stieglitz et al. https://doi.org/10.1016/j.epsl.2018.11.024
38. Multi‐Proxy Evidence for Atlantic Meridional Overturning Circulation (AMOC) Weakening During Deglaciations of the Past 150,000 Years M. Garity & D. Lund https://doi.org/10.1029/2023PA004629
39. An investigation of the possibility of non-Laurentide ice stream contributions to Heinrich event 3 J. Velay-Vitow et al. https://doi.org/10.1017/qua.2020.84
40. 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. https://doi.org/10.5194/gmd-9-2563-2016
41. A high‐resolution Lateglacial and Holocene palaeoceanographic record from the Greenland Sea M. Telesiński et al. https://doi.org/10.1111/bor.12045
42. Ice core evidence for decoupling between midlatitude atmospheric water cycle and Greenland temperature during the last deglaciation A. Landais et al. https://doi.org/10.5194/cp-14-1405-2018
43. 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. https://doi.org/10.5194/tc-13-373-2019
44. Topography's crucial role in Heinrich Events W. Roberts et al. https://doi.org/10.1073/pnas.1414882111
45. Late Pleistocene boreal molluscs in the Gulf of Cadiz: Past and current oceanographic implications J. Urra et al. https://doi.org/10.1016/j.quascirev.2023.108196
46. Late Quaternary glaciations in Far NE Russia; combining moraines, topography and chronology to assess regional and global glaciation synchrony I. Barr & C. Clark https://doi.org/10.1016/j.quascirev.2012.08.004
47. Baffin Bay paleoenvironments in the LGM and HS1: Resolving the ice-shelf question A. Jennings et al. https://doi.org/10.1016/j.margeo.2017.09.002
48. Evolution of the central Nordic Seas over the last 20 thousand years M. Telesiński et al. https://doi.org/10.1016/j.quascirev.2015.05.013
49. Iceberg discharges of the last glacial period driven by oceanic circulation changes J. Alvarez-Solas et al. https://doi.org/10.1073/pnas.1306622110
50. Heinrich event ice discharge and the fate of the Atlantic Meridional Overturning Circulation Y. Zhou & J. McManus https://doi.org/10.1126/science.adh8369
51. The role of ice stream dynamics in deglaciation A. Robel & E. Tziperman https://doi.org/10.1002/2016JF003937
52. The timing of Mediterranean sapropel deposition relative to insolation, sea-level and African monsoon changes K. Grant et al. https://doi.org/10.1016/j.quascirev.2016.03.026
53. Hydrological responses of the Chihuahua Desert of Mexico to possible Heinrich Stadials J. Quiroz-Jimenez et al. https://doi.org/10.1016/j.jsames.2016.11.001
54. Sedimentary architecture and glacial hydrodynamic significance of the stratified Oak Ridges Moraine, southern Ontario, Canada D. Sharpe & H. Russell https://doi.org/10.1111/bor.12612
55. Modeling the Production of Heinrich Layers With a Sediment‐Enabled Iceberg Model M. Fendrock et al. https://doi.org/10.1029/2022PA004583
56. North Pacific freshwater events linked to changes in glacial ocean circulation E. Maier et al. https://doi.org/10.1038/s41586-018-0276-y
57. The role of ice-sheet topography in the Alpine hydro-climate at glacial times P. Velasquez et al. https://doi.org/10.5194/cp-18-1579-2022
58. A new constraint on the size of Heinrich Events from an iceberg/sediment model W. Roberts et al. https://doi.org/10.1016/j.epsl.2013.10.020
59. Frozen fringe explains sediment freeze-on during Heinrich events C. Meyer et al. https://doi.org/10.1016/j.epsl.2019.115725
60. Millennial-scale surface hydrological variability in the tropical eastern Indian Ocean linked to Northern Hemisphere high latitudes R. Cui et al. https://doi.org/10.3389/fmars.2025.1570375
61. Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day C. Batchelor et al. https://doi.org/10.1038/s41586-023-05876-1
62. Destabilization of glacial climate by the radiative impact of Atlantic Meridional Overturning Circulation disruptions E. Galbraith et al. https://doi.org/10.1002/2016GL069846
63. Subsurface ocean warming preceded Heinrich Events L. Max et al. https://doi.org/10.1038/s41467-022-31754-x
64. The role of basal hydrology in the surging of the Laurentide Ice Sheet W. Roberts et al. https://doi.org/10.5194/cp-12-1601-2016
65. 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. https://doi.org/10.5194/cp-9-353-2013
66. Impact of Fjord Geometry on Grounding Line Stability H. Åkesson et al. https://doi.org/10.3389/feart.2018.00071
67. The Baffin Bay Ice Shelf stabilized three adjacent ice sheets during the last glacial period S. Klotsko et al. https://doi.org/10.1038/s41561-026-02126-7
68. Relationship between Magdalenian subsistence and environmental change: The mammalian evidence from El Mirón (Spain) G. Cuenca-Bescós et al. https://doi.org/10.1016/j.quaint.2012.04.035
69. Disentangling the roles of late Miocene palaeogeography and vegetation – Implications for climate sensitivity C. Bradshaw et al. https://doi.org/10.1016/j.palaeo.2014.10.003
70. The comparative role of physical system processes in Hudson Strait ice stream cycling: a comprehensive model-based test of Heinrich event hypotheses K. Hank & L. Tarasov https://doi.org/10.5194/cp-20-2499-2024
71. Instability of the Atlantic overturning circulation during Marine Isotope Stage 3 X. Zhang et al. https://doi.org/10.1002/2014GL060321
72. The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing I. Tabone et al. https://doi.org/10.5194/cp-14-455-2018
73. Labrador Current fluctuation during the last glacial cycle L. Mao et al. https://doi.org/10.1016/j.margeo.2017.10.012
74. Numerical reconstructions of the penultimate glacial maximum Northern Hemisphere ice sheets: sensitivity to climate forcing and model parameters C. WEKERLE et al. https://doi.org/10.1017/jog.2016.45
75. Ice sheets as interactive components of Earth System Models: progress and challenges M. Vizcaino https://doi.org/10.1002/wcc.285
76. Modeling Northern Hemisphere ice-sheet distribution during MIS 5 and MIS 7 glacial inceptions F. Colleoni et al. https://doi.org/10.5194/cp-10-269-2014
77. Dansgaard‐Oeschger cycles: Interactions between ocean and sea ice intrinsic to the Nordic seas T. Dokken et al. https://doi.org/10.1002/palo.20042
78. Accumulation of remineralised carbon and nutrients in the mid-depth Atlantic during Heinrich Stadial 1 and the Younger Dryas J. Stewart et al. https://doi.org/10.1016/j.epsl.2026.119866
79. Interglacials of the last 800,000 years https://doi.org/10.1002/2015RG000482
80. Similarities and dissimilarities between the last two deglaciations and interglaciations in the North Atlantic region B. Martrat et al. https://doi.org/10.1016/j.quascirev.2014.06.016
81. Rainfall response to orbital and millennial forcing in northern Peru over the last 18 ka E. Mollier-Vogel et al. https://doi.org/10.1016/j.quascirev.2013.06.021
82. 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. https://doi.org/10.1016/j.gloplacha.2020.103227
83. Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions F. Colleoni et al. https://doi.org/10.1038/s41598-018-29718-7
84. Spatial fingerprint and magnitude of changes in the Atlantic meridional overturning circulation during marine isotope stage 3 X. Zhang et al. https://doi.org/10.1002/2014GL063003
85. Exploring the MIS M2 glaciation occurring during a warm and high atmospheric CO2 Pliocene background climate N. Tan et al. https://doi.org/10.1016/j.epsl.2017.04.050
86. Anatomy of Heinrich Layer 1 and its role in the last deglaciation D. Hodell et al. https://doi.org/10.1002/2016PA003028
87. Heinrich Events D. Faust et al. https://doi.org/10.1017/qua.2021.2
88. Shelf-break glaciation and an extensive ice shelf beyond northwest Greenland at the Last Glacial Maximum C. Batchelor et al. https://doi.org/10.1016/j.margeo.2024.107375