FN Archimer Export Format
PT J
TI Basin-Wide Oceanographic Array Bridges the South Atlantic
BT 
AF ANSORGE, Isabelle J.
   BARINGER, Molly
   CAMPOS, Edmo J.D.
   DONG, S.
   FINE, R.A.
   GARZOLI, Silvia L.
   GONI, Gustavo
   MEINEN, Christopher S.
   PEREZ, R.C.
   PIOLA, Alberto R.
   ROBERTS, M.J.
   SPEICH, Sabrina
   SPRINTALL, J.
   TERRE TERRILLON, Thierry
   VAN DEN BERG, M.A.
AS 1:1;2:2;3:3;4:4;5:2,5;6:2,4;7:2;8:2;9:2,5;10:6,7;11:8;12:9;13:10;14:11;15:9;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:PDG-ODE-LPO-STOIS;15:;
C1 University of Cape Town, Rondebosch, South Africa
   National Oceanic and Atmospheric Administration (NOAA), Miami, Fla., USA
   University of São Paulo, São Paulo, Brazil
   University of Miami, Miami, Fla, USA
   University of Miami, Miami, Fla, USA
   Departamento de Oceanografía, Servicio de Hidrografía Naval, Buenos Aires, Argentina
   Universidad de Buenos Aires, Buenos Aires, Argentina
   Oceans and Coasts Research, Department of Environmental Affairs, Roggebaai, South Africa
   Universite de Bretagne Occidentale Brest, France
   Scripps Institution of Oceanography, University of California, San Diego, La Jolla, USA
   Ifremer,Plouzané, France
C2 UNIV CAPE TOWN, SOUTH AFRICA
   NOAA, USA
   UNIV SAO PAULO, BRAZIL
   UNIV MIAMI, USA
   UNIV MIAMI, USA
   SHN, ARGENTINA
   UNIV BUENOS AIRES, ARGENTINA
   OCEANS RES, SOUTH AFRICA
   UBO, FRANCE
   SCRIPPS INST OCEANOG, USA
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LPO
   PDG-ODE-LPO-STOIS
TC 0
UR https://archimer.ifremer.fr/doc/00175/28609/27109.pdf
LA English
DT Article
DE ;South Atlantic;Meridional Overturning Circulation;CPIES
AB The meridional overturning circulation (MOC) is a global system of surface, intermediate, and deep ocean currents. The MOC connects the surface layer of the ocean and the atmosphere with the huge reservoir of the deep sea and is the primary mechanism for transporting heat, freshwater, and carbon between ocean basins. Climate models show that past changes in the strength of the MOC were linked to historical climate variations. Further research suggests that the MOC will continue to modulate climate change scenarios on time scales ranging from decades to centuries [Latif et al., 2006].
PY 2014
PD FEB
SO Eos, Transactions American Geophysical Union
SN 0096-3941
PU American Geophysical Union
VL 95
IS 6
BP 53
EP 54
DI 10.1002/2014EO060001
ID 28609
ER

EF