(Q58083611)

English

Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice cores

scholarly article

Statements

Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice cores (English)
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Eric Monnin
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Urs Siegenthaler
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Jakob Schwander
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Bernhard Stauffer
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Blandine Bellier
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July 2004
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224
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1-2
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45-54
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