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

. High-resolution climate model simulations for the last millenniumwere used to elucidate the main winter Northern Hemisphere atmosphericpattern during enhanced Eastern Mediterranean Transient (EMT-type) events, asituation in which an additional overturning cell is detected in theMediterranean at the Aegean Sea. The differential upward heat flux betweenthe Aegean Basin and the Gulf of Lion was taken as a proxy of EMT-typeevents and correlated with winter mean geopotential height at 500 mbar in theNorthern Hemisphere (20–90∘ N and100∘ W–80∘ E). Correlations revealed apattern similar to the East Atlantic/Western Russian (EA/WR) mode asthe main driver of EMT-type events, with the past 1000 years of EA/WR-like modesimulations being enhanced during insolation minima. Our model results areconsistent with alkenone sea surface temperature (SST) reconstructions thatdocumented an increase in the west–east basin gradients during EMT-typeevents.

Northern Hemisphere atmospheric pattern enhancing Eastern Mediterranean Transient-type events during the past 1000 years