(Q107105145)

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The age and origin of the “Younger Dryas climate event” in Greenland ice cores

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The age and origin of the “Younger Dryas climate event” in Greenland ice cores (English)

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Richard G. Fairbanks

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publication date

December 1990

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published in

Paleoceanography

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volume

5

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issue

6

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page(s)

937-948

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cites work

Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals

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Salinity history of the northern Atlantic during the last deglaciation

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The role of ocean-atmosphere reorganizations in glacial cycles

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The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas Event

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The surface of the ice-age Earth

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Tellus A: Dynamic Meteorology and Oceanography, Volume 73, Issue 1 (2021)

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A new greenland deep ice core

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The abrupt termination of the Younger Dryas climate event

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A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

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Evidence for two-step deglaciation and its impact on North Atlantic deep-water circulation

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Global sources of local precipitation as determined by the Nasa/Giss GCM

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Polar ice ablation rates measured using in situ cosmogenic 14C

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Quaternary stratigraphy of Norden, a proposal for terminology and classification

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Radiocarbon Age Calibration Back to 13,300 Years BP and the 14C Age Matching of the German Oak and US Bristlecone Pine Chronologies

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Identifiers

DOI

10.1029/PA005I006P00937

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ADS bibcode

1990PalOc...5..937F

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(Q107105145)

The age and origin of the “Younger Dryas climate event” in Greenland ice cores

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