FN Archimer Export Format
PT J
TI Subpolar North Atlantic western boundary density anomalies and the Meridional Overturning Circulation
BT 
AF Li, F.
   Lozier, M. S.
   Bacon, S.
   Bower, A. S.
   Cunningham, S. A.
   de Jong, M. F.
   deYoung, B.
   Fraser, N.
   Fried, N.
   Han, G.
   Holliday, N. P.
   Holte, J.
   Houpert, L.
   Inall, M. E.
   Johns, W. E.
   Jones, S.
   Johnson, C.
   Karstensen, J.
   Le Bras, I. A.
   Lherminier, Pascale
   Lin, X.
   Mercier, Herle
   Oltmanns, M.
   Pacini, A.
   Petit, T.
   Pickart, R. S.
   Rayner, D.
   Straneo, F.
   Thierry, Virginie
   Visbeck, M.
   Yashayaev, I.
   Zhou, C.
AS 1:1,2;2:2;3:3;4:4;5:5;6:6;7:7;8:5;9:6;10:8,9;11:3;12:10;13:3;14:5,11;15:12;16:5;17:5;18:13;19:4,10;20:14;21:15;22:16;23:13;24:4;25:2;26:4;27:3;28:10;29:14;30:13;31:17;32:15;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:PDG-ODE-LOPS-OH;21:;22:;23:;24:;25:;26:;27:;28:;29:PDG-ODE-LOPS-OH;30:;31:;32:;
C1 State Key Laboratory of Marine Environmental Science & College of Ocean and Earth Sciences, Xiamen University, Xiamen, China
   School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USA
   National Oceanography Centre, Southampton, UK
   Woods Hole Oceanographic Institution, Woods Hole, MA, USA
   Scottish Association for Marine Science, Oban, UK
   NIOZ Royal Netherlands Institute for Sea Research, Texel, Netherlands
   Department of Physics and Physical Oceanography, Memorial University, St. John’s, NL, Canada
   Fisheries and Oceans Canada, Institute of Ocean Sciences, Sidney, BC, Canada
   Fisheries and Oceans Canada, Northwest Atlantic Fisheries Centre, St. John’s, NL, Canada
   Scripps Institution of Oceanography, UCSD, La Jolla, CA, USA
   School of Geosciences, Edinburgh University, Edinburgh, UK
   Department of Ocean Sciences, University of Miami, Miami, FL, USA
   GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
   Univ. Brest, Ifremer, CNRS, IRD, Laboratoire d’Océanographie Physique et Spatiale, Plouzané, France
   Frontier Science Center for Deep Ocean Multispheres and Earth System and Physical Oceanography Laboratory, Ocean University of China, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
   CNRS, Laboratoire d’Océanographie Physique et Spatiale, Plouzané, France
   Bedford Institute of Oceanography, Dartmouth, NS, Canada
C2 UNIV XIAMEN, CHINA
   GEORGIA INST TECHNOL, USA
   NOC, UK
   WHOI, USA
   SAMS SCOTLAND, UK
   INST SEA RESEARCH (NIOZ), NETHERLANDS
   UNIV MEM NEWFOUNDLAND, CANADA
   MPO, CANADA
   MPO, CANADA
   UNIV CALIF SAN DIEGO, USA
   UNIV EDINBURGH, UK
   UNIV MIAMI, USA
   IFM GEOMAR, GERMANY
   IFREMER, FRANCE
   UNIV OCEAN CHINA, CHINA
   CNRS, FRANCE
   BEDFORD INST OCEANOG, CANADA
SI BREST
SE PDG-ODE-LOPS-OH
UM LOPS
IN WOS Ifremer UMR
   WOS Cotutelle UMR
   DOAJ
   copubli-france
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 17.694
TC 58
UR https://archimer.ifremer.fr/doc/00697/80879/84607.pdf
   https://archimer.ifremer.fr/doc/00697/80879/84608.pdf
   https://archimer.ifremer.fr/doc/00697/80879/91343.pdf
LA English
DT Article
CR OVIDE
   OVIDE 2018
BO Thalassa
AB Changes in the Atlantic Meridional Overturning Circulation, which have the potential to drive societally-important climate impacts, have traditionally been linked to the strength of deep water formation in the subpolar North Atlantic. Yet there is neither clear observational evidence nor agreement among models about how changes in deep water formation influence overturning. Here, we use data from a trans-basin mooring array (OSNAP—Overturning in the Subpolar North Atlantic Program) to show that winter convection during 2014–2018 in the interior basin had minimal impact on density changes in the deep western boundary currents in the subpolar basins. Contrary to previous modeling studies, we find no discernable relationship between western boundary changes and subpolar overturning variability over the observational time scales. Our results require a reconsideration of the notion of deep western boundary changes representing overturning characteristics, with implications for constraining the source of overturning variability within and downstream of the subpolar region. 
PY 2021
PD MAY
SO Nature Communications
SN 2041-1723
PU Springer Science and Business Media LLC
VL 12
IS 1
UT 000658768100001
DI 10.1038/s41467-021-23350-2
ID 80879
ER

EF