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

Evaporation, precipitation and atmospheric water vapor transport play an important role in maintaining North Atlantic Meridional Overturning Circulation (AMOC) through their influence on salinity (Broecker, 1989; Broecker et al., 1990; Zaucker and Broecker, 1992). Net evaporation exceeds precipitation in both the Caribbean and western North Atlantic subtropical gyre, elevating Gulf Stream sea surface salinity (SSS) as waters circulate northward through the subtropics (Broecker et al., 1990; Curry et al., 2003). The excess salt advected to the North Atlantic is critical in maintaining modern AMOC (Broecker, 1991). It is generally agreed that the abrupt climatic shifts that characterized Dansgaard-Oeschger (D-O) cycles in the Greenland ice cores were triggered by changes in North Atlantic surface water density at the sites of overturning circulation (Boyle, Figure 1: Modern N. Atlantic surface (red) and deep water (blue) circulation and location of Caribbean cores ODP 999A (12°45'N, 78°44'W; 2,827 m; 4 cm/kyr sed. rate) and VM28-122 (11.56°N, 78.41°W; 3,623 m; 4-15 cm/kyr sed. rate) and N. Atlantic subtropical gyre core ODP 1060 (30°46'N, 74°28'W; 3480 m; 20-53 cm/ kyr sed. rate). Orange circles indicate sites of deepwater formation in N. Atlantic. 2000; Oppo and Lehman, 1995; Rasmussen and Thomsen, 2004). While warm interstadials are characterized by a circulation pat-

North Atlantic salinity oscillations linked to atmospheric and ocean circulation changes over the last glacial cycle