N Daniault, H Mercier, P Lherminier, A Sarafanov… - Progress in …, 2016 - Elsevier
The decadal mean circulation in the northern North Atlantic was assessed for the early 21st century from repeated ship-based measurements along the Greenland-Portugal OVIDE line …
MS Lozier, S Bacon, AS Bower… - Bulletin of the …, 2017 - journals.ametsoc.org
Overturning in the Subpolar North Atlantic Program: A New International Ocean Observing System in: Bulletin of the American Meteorological Society Volume 98 Issue 4 (2017) Jump …
MS Lozier - Annual review of marine science, 2012 - annualreviews.org
The global overturning of ocean waters involves the equatorward transport of cold, deep waters and the poleward transport of warm, near-surface waters. Such movement creates a …
D Kieke, I Yashayaev - Progress in Oceanography, 2015 - Elsevier
Abstract Labrador Sea Water (LSW), the lightest contribution to North Atlantic Deep Water (NADW) and one of the most prominent water masses of the subpolar North Atlantic, has …
In this study 36 hydrographic transects occupied between 1991 and 2007 in the vicinity of the WOCE A1E/AR7E section are used to investigate various aspects of the Irminger Gyre, a …
R Zhang, M Thomas - Communications Earth & Environment, 2021 - nature.com
Abstract The Greenland Sea is often viewed as the northern terminus of the Atlantic Meridional Overturning Circulation. It has also been proposed that the shutdown of open …
A Sarafanov, A Falina, H Mercier… - Journal of …, 2012 - Wiley Online Library
A mean state of the full‐depth summer circulation in the Atlantic Ocean in the region in between Cape Farewell (Greenland), Scotland and the Greenland‐Scotland Ridge (GSR) is …
A Köhl, D Stammer - Journal of Physical Oceanography, 2008 - journals.ametsoc.org
Variability of the Meridional Overturning in the North Atlantic from the 50-Year GECCO State Estimation in: Journal of Physical Oceanography Volume 38 Issue 9 (2008) Jump to …
Abstract The Labrador Sea in the North Atlantic Ocean is one of the few regions globally where oxygen from the atmosphere can reach the deep ocean directly. This is the result of …