(Q59091139)

English

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

scientific article published in Nature

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scholarly article

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

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inferred from title

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object named as

E. Jansen

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author name string

T. Veum

2

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language of work or name

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publication date

February 1990

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343

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6259

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612-616

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https://scigraph.springernature.com/pub.10.1038/343612a0

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Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continent

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Structure and timing of the last deglaciation: Oxygen-isotope evidence

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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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Does the ocean–atmosphere system have more than one stable mode of operation?

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The impact of cold North Atlantic sea surface temperatures on climate: implications for the Younger Dryas cooling (11–10 k)

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

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Variations in the Earth's Orbit: Pacemaker of the Ice Ages

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Matuyama 41,000-year cycles: North Atlantic Ocean and northern hemisphere ice sheets

1 reference

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Climate change in the circum-North Atlantic region during the last deglaciation

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Can the Greenland Climatic Jumps be Identified in Records from Ocean and Land?

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Direct dating of the oxygen-isotope record of the last deglaciation by 14C accelerator mass spectrometry

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Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometry

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Reconstruction of the last deglaciation: deconvolved records of ?18O profiles, micropaleontological variations and accelerator mass spectrometric14C dating

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Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode

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Evidence from Fram Strait (78° N) for early deglaciation

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Oxygen isotopes and sea level

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Variations in mode of formation and temperature of oceanic deep waters over the past 125,000 years

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Ocean circulation in the Norwegian sea during the last deglaciation: Isotopic evidence

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Lake Sediments as Continental δ18O Records from the Glacial/Post-Glacial Transition

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The last deglaciation (20,000 to 11,000 B. P.) on Andoya, northern Norway

1 reference

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Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence

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North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature

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Late Pliocene variation in northern hemisphere ice sheets and North Atlantic deep water circulation

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inferred from DOI database lookup

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10.1038/343612A0

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