English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

the rapid warming transitions into the Bølling-Allerød interstadial and Holocene interglacial are striking examples of nonlinearities in the climate system. A leading hypothesis for the trigger of these events has been changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC) (McManus et al. 2004). However, records from the North Pacific and other distant locations document equally abrupt climate changes as those observed in the North Atlantic (Hendy and Kennett 1999; Wang et al. 2001; Praetorius and Mix 2014). this calls into question whether these are teleconnected responses to changes in the AMOC, or whether they involve orchestration of northern hemisphere climate dynamics and reflect critical transitions in the climate system, possibly involving multiple “tipping elements” (Lenton et al. 2008).

Did synchronized ocean warming in the North Pacific and North Atlantic trigger a deglacial tipping point in the Northern Hemisphere?