Global hydroclimatic response to tropical volcanic eruptions over the last millennium.

Proc Natl Acad Sci U S A · 2021 · PMC8000584 · PMID 33798096

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barely significantno p-value reported

Despite being weak and barely significant, the apparent posteruption cooling in the tropical Pacific does persist for almost a decade in PHYDA and is one potential feedback mechanism for extending radiatively induced cooling by maintaining anomalously cold conditions in the tropical Pacific and the consequent cold extension through the global tropics ( 42 ).

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