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5. Extreme climate after massive eruption of Alaska’s Okmok volcano in 43 BCE and effects on the late Roman Republic and Ptolemaic Kingdom

8. Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion

9. Origin of silty basal ice in Greenland

11. A 120,000-year long climate record from a NW-Greenland deep ice core at ultra-high resolution

14. Ice-core data used for the construction of the Greenland Ice-Core Chronology 2005 and 2021 (GICC05 and GICC21)

15. New insights on Greenland ice sheet basal processes: modelling the evolution of a biological signature and diffusion processes

16. Detection of ice core particles via deep neural networks

17. Ice-core data used for the construction of the Greenland Ice-Core Chronology 2005 and 2021 (GICC05 and GICC21)

18. Detection of ice core particles via deep neural networks

19. A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy

20. Visual Stratigraphy of the EastGRIP Ice Core - Of the Lost Ice Core Orientation, Deformation Structures, Extreme Warm Events, and Trapped Ancient Air

21. Ice-core data used for the construction of the Greenland Ice-Core Chronology 2005 and 2021 (GICC05 and GICC21).

23. Supplementary material to "Detection of ice core particles via deep neural networks"

24. Detection of ice core particles via deep neural networks

25. Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)

26. Volcanism and the Greenland ice cores:A new tephrochronological framework for the last glacial-interglacial transition (LGIT) based on cryptotephra deposits in three ice cores

27. Evaluating in situ microbial production of greenhouse gases in subglacial environments of Greenland Ice Sheet: new insights from the Camp Century basal ice section

30. Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)

31. High-Resolution Greenland Ice Core Data Show Abrupt Climate Change Happens in Few Years

32. Ancient Biomolecules from Deep Ice Cores Reveal a Forested Southern Greenland

33. Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)

34. Supplementary material to "Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)"

35. Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)

37. A multimillion-year-old record of Greenland vegetation and glacial history preserved in sediment beneath 1.4 km of ice at Camp Century

40. Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period

41. Supplementary material to 'Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period'

42. Geological, geochemical and cosmogenic nuclides constraints from the NEEM core basal sediments, Greenland

43. Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period

44. Supplementary material to "Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period"

45. Theoretical and Experimental Analysis for Cleaning Ice Cores from Estisol TM 140 Drill Liquid.

46. Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion

47. Synchronous volcanic eruptions and abrupt climate change ~17.7 ka plausibly linked by stratospheric ozone depletion

49. Stable oxygen isotope variability in two contrasting glacier river catchments in Greenland

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