(Q59087754)

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Deuterium excess in an East Antarctic ice core suggests higher relative humidity at the oceanic surface during the last glacial maximum

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Deuterium excess in an East Antarctic ice core suggests higher relative humidity at the oceanic surface during the last glacial maximum (English)

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Jean Jouzel

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Claude Lorius

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Claude Lorius

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Liliane Merlivat

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2

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English

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publication date

October 1982

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Nature

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299

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5885

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688-691

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https://scigraph.springernature.com/pub.10.1038/299688a0

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Isotopic Variations in Meteoric Waters

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One thousand centuries of climatic record from cAMP century on the greenland ice sheet

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Antarctic ice sheet: stable isotope analyses of byrd station cores and interhemispheric climatic implications

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Global climatic interpretation of the deuterium-oxygen 18 relationship for precipitation

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A 30,000-yr isotope climatic record from Antarctic ice

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

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The surface of the ice-age Earth

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Glacier oxygen-18 content and pleistocene ocean temperatures

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7 January 2021

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Ice age aerosol content from East Antarctic ice core samples and past wind strength

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10.1038/299688A0

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1042020253

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(Q59087754)

Deuterium excess in an East Antarctic ice core suggests higher relative humidity at the oceanic surface during the last glacial maximum

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