A Southern Ocean trigger for Northwest Pacific ventilation during the Holocene?

Sci Rep · 2014 · PMC4027855 · PMID 24509792

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a decreasing trendno p-value reported

At precessional scales, the AAT and WAP SST records show a decreasing trend over the course of the Holocene until ~2 ka ( Fig. 6a, b ), which is thought to be primarily driven by shortening of Antarctic summers, apparently in response to declining austral spring insolation at ~65°S (ref. 49 , 57 ).

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