FN Archimer Export Format
PT J
TI A sea change in our view of overturning in the subpolar North Atlantic
BT 
AF LOZIER, M. S.
   LI, F.
   BACON, S.
   BAHR, F.
   BOWER, A. S.
   CUNNINGHAM, S. A.
   DE JONG, M. F.
   DE STEUR, L.
   DEYOUNG, B.
   FISCHER, J.
   GARY, S. F.
   GREENAN, B. J. W.
   HOLLIDAY, N. P.
   HOUK, A.
   HOUPERT, L.
   INALL, M. E.
   JOHNS, W. E.
   JOHNSON, H. L.
   JOHNSON, C.
   KARSTENSEN, J.
   KOMAN, G.
   LE BRAS, I. A.
   LIN, X.
   MACKAY, N.
   MARSHALL, D. P.
   MERCIER, Herle
   OLTMANNS, M.
   PICKART, R. S.
   RAMSEY, A. L.
   RAYNER, D.
   STRANEO, F.
   THIERRY, Virginie
   TORRES, D. J.
   WILLIAMS, R. G.
   WILSON, C.
   YANG, J.
   YASHAYAEV, I.
   ZHAO, J.
AS 1:1;2:1;3:2;4:3;5:3;6:4;7:5,6;8:5,6;9:7;10:8;11:4;12:9;13:2;14:10;15:4;16:4,11;17:10;18:12;19:4;20:8;21:10;22:13;23:14,15,16;24:17;25:18;26:19;27:8;28:3;29:3;30:2;31:13;32:20;33:3;34:21;35:17;36:3;37:9;38:3;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:;31:;32:PDG-ODE-LOPS-OH;33:;34:;35:;36:;37:;38:;
C1 Duke Univ, Div Earth & Ocean Sci, Durham, NC 27708 USA.
   Natl Oceanog Ctr, Southampton, Hants, England.
   Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
   Scottish Assoc Marine Sci, Oban, Argyll, Scotland.
   Royal Netherlands Inst Sea Res, Texel, Netherlands.
   Univ Utrecht, Texel, Netherlands.
   Mem Univ, Dept Phys & Phys Oceanog, St John, NF, Canada.
   GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany.
   Bedford Inst Oceanog, Dartmouth, NS, Canada.
   Univ Miami, Dept Ocean Sci, Miami, FL USA.
   Univ Edinburgh, Sch Geosci, Edinburgh, Midlothian, Scotland.
   Univ Oxford, Dept Earth Sci, Oxford, England.
   UCSD, Scripps Inst Oceanog, La Jolla, CA USA.
   Ocean Univ China, Phys Oceanog Lab, Qingdao, Peoples R China.
   Ocean Univ China, Inst Adv Ocean Studies, Qingdao, Peoples R China.
   Qingdao Natl Lab Marine Sci & Technol, Qingdao, Peoples R China.
   Natl Oceanog Ctr, Liverpool, Merseyside, England.
   Univ Oxford, Dept Phys, Oxford, England.
   CNRS, Lab Oceanog Phys & Spatiale, Plouzane, France.
   IFREMER, Lab Oceanog Phys & Spatiale, Plouzane, France.
   Univ Liverpool, Dept Earth Ocean & Ecol Sci, Liverpool, Merseyside, England.
C2 UNIV DUKE, USA
   NOC, UK
   WHOI, USA
   SAMS SCOTLAND, UK
   INST SEA RESEARCH (NIOZ), NETHERLANDS
   UNIV UTRECHT, NETHERLANDS
   UNIV MEM NEWFOUNDLAND, CANADA
   IFM GEOMAR, GERMANY
   BEDFORD INST OCEANOG, CANADA
   UNIV MIAMI, USA
   UNIV EDINBURGH, UK
   UNIV OXFORD, UK
   UNIV CALIF SAN DIEGO, USA
   UNIV OCEAN CHINA, CHINA
   UNIV OCEAN CHINA, CHINA
   QNLM, CHINA
   NOC, UK
   UNIV OXFORD, UK
   CNRS, FRANCE
   IFREMER, FRANCE
   UNIV LIVERPOOL, UK
SI BREST
SE PDG-ODE-LOPS-OH
UM LOPS
IN WOS Ifremer UMR
   WOS Cotutelle UMR
   copubli-france
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 41.845
TC 322
UR https://archimer.ifremer.fr/doc/00481/59234/61940.pdf
   https://archimer.ifremer.fr/doc/00481/59234/61942.pdf
LA English
DT Article
CR OVIDE
   RREX 2015
   RREX 2017
BO Thalassa
   L'Atalante
AB To provide an observational basis for the Intergovernmental Panel on Climate Change projections of a slowing Atlantic meridional overturning circulation (MOC) in the 21st century, the Overturning in the Subpolar North Atlantic Program (OSNAP) observing system was launched in the summer of 2014. The first 21-month record reveals a highly variable overturning circulation responsible for the majority of the heat and freshwater transport across the OSNAP line. In a departure from the prevailing view that changes in deep water formation in the Labrador Sea dominate MOC variability, these results suggest that the conversion of warm, salty, shallow Atlantic waters into colder, fresher, deep waters that move southward in the Irminger and Iceland basins is largely responsible for overturning and its variability in the subpolar basin. 
PY 2019
PD FEB
SO Science
SN 0036-8075
PU Amer Assoc Advancement Science
VL 363
IS 6426
UT 000457409400046
BP 516
EP 521
DI 10.1126/science.aau6592
ID 59234
ER

EF