Holocene sea ice variability driven by wind and polynya efficiency in the Ross Sea.

Nat Commun · 2017 · PMC5673891 · PMID 29109395

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Contrasted behaviours are also observed in the δ 18 O records, with TY decreasing throughout the Holocene and TALDICE exhibiting relative high values during the early Holocene followed by a minimum at ~8 ka, with an increasing trend from 8 to 1.5 ka and again lower values during the last millennium.

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