Linked from

The 12 pages that link to Greenland ice core, each with the reason it gives.

• Last Glacial MaximumRelated: Its annual and chemical records help track abrupt climate variability surrounding the LGM.

• Younger DryasRelated: Its isotope measurements provide a finely resolved record of the temperature shift.

• Little Ice AgeRelated: Ice chemistry helps reconstruct volcanic activity and climate changes during the period.

• Norse GreenlandRelated: They help reconstruct environmental change during the settlements’ lifetime.

• Allerød oscillationRelated: Ice-core records help compare Allerød timing with abrupt changes in Greenland.

• Bølling oscillationRelated: Its isotope records provide a detailed chronology of the abrupt temperature rise.

• Holocene climatic optimumRelated: Ice-isotope records show early-Holocene warmth followed by cooling in Greenland.

• Older DryasRelated: Ice-core records help track abrupt temperature changes across the deglacial sequence.

• Roman Warm PeriodRelated: Greenland records provide North Atlantic context but are geographically distant from much of Europe.