McCall Glacier record of Arctic climate change: Interpreting a northern Alaska ice core with regional water isotopes
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文摘

Reconstructed temperatures show a warming trend at McCall over the past ∼65 years.

McCall isotopes exhibit a bidecadal periodicity coherent with the NPI.

The NPI correlation is negative with δ18O, but positive with d-excess.

McCall moisture sources switched decadally with shifts in the Aleutian Low.

Open northern ocean water input to terrestrial Arctic precipitation is increasing.

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