FN Archimer Export Format
PT J
TI Overturning in the Subpolar North Atlantic Program: a new international ocean observing system
BT 
AF LOZIER, M. Susan
   BACON, Sheldon
   BOWER, Amy S.
   CUNNINGHAM, Stuart A.
   DE JONG, M. Femke
   DE STEUR, Laura
   DEYOUNG, Brad
   FISCHER, Juergen
   GARY, Stefan F.
   GREENAN, Blair J. W.
   HEIMBACH, Patrick
   HOLLIDAY, Naomi P.
   HOUPERT, Loic
   INALL, Mark E.
   JOHNS, William E.
   JOHNSON, Helen L.
   KARSTENSEN, Johannes
   LI, Feili
   LIN, Xiaopei
   MACKAY, Neill
   MARSHALL, David P.
   MERCIER, Herle
   MYERS, Paul G.
   PICKART, Robert S.
   PILLAR, Helen R.
   STRANEO, Fiammetta
   THIERRY, Virginie
   WELLER, Robert A.
   WILLIAMS, Richard G.
   WILSON, Chris
   YANG, Jiayan
   ZHAO, Jian
   ZIKA, Jan D.
AS 1:1;2:2;3:3;4:4;5:1,5,6;6:5,6;7:7;8:8;9:4;10:9;11:10;12:2;13:4;14:4;15:11;16:12;17:8;18:1;19:13;20:14;21:12;22:15;23:16;24:3;25:17;26:3;27:20;28:3;29:18;30:14;31:3;32:3;33:19;
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:PDG-ODE-LOPS-OH;28:;29:;30:;31:;32:;33:;
C1 Duke Univ, 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, Utrecht, Netherlands.
   Mem Univ, St John, NF, Canada.
   GEOMAR Helmholtz Ctr Ocean Res, Kiel, Germany.
   Bedford Inst Oceanog, Dartmouth, NS, Canada.
   Univ Texas Austin, Austin, TX 78712 USA.
   Univ Miami, Miami, FL USA.
   Univ Oxford, Oxford, England.
   Ocean Univ China, Qingdao Natl Labora tory Marine Sci & Technol, Qingdao, Peoples R China.
   Natl Oceanog Ctr, Liverpool, Merseyside, England.
   CNRS, Lab Ocean Phys & Satellite Oceanog, Ifremer Ctr Bretagne, Plouzane, France.
   Univ Alberta, Edmonton, AB, Canada.
   Univ Copenhagen, Niels Bohr Inst, Copenhagen, Denmark.
   Univ Liverpool, Liverpool, Merseyside, England.
   Imperial Coll London, London, England.
C2 UNIV DUKE, USA
   NOC, UK
   WHOI, USA
   SAMS SCOTLAND, UK
   INST SEA RESEARCH (NIOZ), NETHERLANDS
   UNIV UTRECHT, NETHERLANDS
   UNIV MEM NEWFOUNDLAND, CANADA
   GEOMAR HELMHOLTZ CTR OCEAN RES, GERMANY
   BEDFORD INST OCEANOG, CANADA
   UNIV TEXAS AUSTIN, USA
   UNIV MIAMI, USA
   UNIV OXFORD, UK
   UNIV OCEAN CHINA, CHINA
   NOC, UK
   CNRS, FRANCE
   UNIV ALBERTA, CANADA
   UNIV COPENHAGEN, DENMARK
   UNIV LIVERPOOL, UK
   IMPERIAL COLL LONDON, UK
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LOPS-OH
UM LOPS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 7.804
TC 166
UR https://archimer.ifremer.fr/doc/00358/46881/46764.pdf
LA English
DT Article
CR RREX 2015
BO Thalassa
AB A new ocean observing system has been launched in the North Atlantic in order to understand the linkage between the meridional overturning circulation and deep water formation.  For decades oceanographers have understood the Atlantic Meridional Overturning Circulation (AMOC) to be primarily driven by changes in the production of deep water formation in the subpolar and subarctic North Atlantic. Indeed, current IPCC projections of an AMOC slowdown in the 21st century based on climate models are attributed to the inhibition of deep convection in the North Atlantic. However, observational evidence for this linkage has been elusive: there has been no clear demonstration of AMOC variability in response to changes in deep water formation. The motivation for understanding this linkage is compelling since the overturning circulation has been shown to sequester heat and anthropogenic carbon in the deep ocean. Furthermore, AMOC variability is expected to impact this sequestration as well as have consequences for regional and global climates through its effect on the poleward transport of warm water. Motivated by the need for a mechanistic understanding of the AMOC, an international community has assembled an observing system, Overturning in the Subpolar North Atlantic (OSNAP), to provide a continuous record of the trans-basin fluxes of heat, mass and freshwater and to link that record to convective activity and water mass transformation at high latitudes. OSNAP, in conjunction with the RAPID/MOCHA array at 26°N and other observational elements, will provide a comprehensive measure of the three-dimensional AMOC and an understanding of what drives its variability. The OSNAP observing system was fully deployed in the summer of 2014 and the first OSNAP data products are expected in the fall of 2017.
PY 2017
PD APR
SO Bulletin Of The American Meteorological Society
SN 0003-0007
PU Amer Meteorological Soc
VL 98
IS 4
UT 000400293700009
BP 737
EP 752
DI 10.1175/BAMS-D-16-0057.1
ID 46881
ER

EF