Author/Authors :
Sicre، نويسنده , , M.-A. and Weckstrِm، نويسنده , , K. and Seidenkrantz، نويسنده , , M.-S. and Kuijpers، نويسنده , , A. and Benetti، نويسنده , , M. and Massé، نويسنده , , G. and Ezat، نويسنده , , U. and Schmidt، نويسنده , , S. and Bouloubassi، نويسنده , , I. I. Olsen، نويسنده , , J. and Khodri، نويسنده , , M. and Mignot، نويسنده , , J.، نويسنده ,
Abstract :
The ice-loaded Labrador Current (LC) is an important component of the western North Atlantic circulation that influences the position and strength of the northern limb of the North Atlantic Current (NAC). This flow of cold and fresh Polar Waters originating from the Arctic has a marked impact on the North Atlantic climate, yet little is known about its variability beyond the instrumental period. In this study, we present the first sub-decadal alkenone-based 2000-year long sea-surface temperature (SST) records from the western Labrador Sea, a climatically crucial region at the boundary between the LC and the NAC. Our results show a clear link between the LC strength and the Northern Annular Mode (NAM), with a stronger NAM and a more vigorous LC during the Medieval Climate Anomaly (MCA). This suggests enhanced LC activity upon future global warming with implications for the Atlantic meridional overturning circulation (AMOC).
Keywords :
last millennia , Ocean variability , Labrador Sea , Newfoundland , northern annular mode , Temperature proxy
