FN Archimer Export Format
PT J
TI The reinvigoration of the Southern Ocean carbon sink
BT 
AF LANDSCHUTZER, Peter
   GRUBER, Nicolas
   HAUMANN, Alexander
   RODENBECK, Christian
   BAKKER, Dorothee C. E.
   VAN HEUVEN, Steven
   HOPPEMA, Mario
   METZL, Nicolas
   SWEENEY, Colm
   TAKAHASHI, Taro
   TILBROOK, Bronte
   WANNINKHOF, Rik
AS 1:1;2:1,2;3:1,2;4:3;5:4;6:5;7:5;8:6;9:7,8;10:9;11:10,11;12:12;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;
C1 ETH, Inst Biogeochem & Pollutant Dynam, Environm Phys, Zurich, Switzerland.
   ETH, C2SM, Zurich, Switzerland.
   Max Planck Inst Biogeochem, D-07745 Jena, Germany.
   Univ E Anglia, Sch Environm Sci, Ctr Ocean & Atmospher Sci, Norwich NR4 7TJ, Norfolk, England.
   Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany.
   Univ Paris 06, Univ Paris 04, CNRS, IRD,MNHN,LOCEAN,IPSL Lab, F-75005 Paris, France.
   Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA.
   NOAA, Earth Syst Res Lab, Boulder, CO USA.
   Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA.
   CSIRO, Hobart, Tas, Australia.
   Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas, Australia.
   NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.
C2 ETH ZURICH, SWITZERLAND
   ETH ZURICH, SWITZERLAND
   MAX PLANCK INST, GERMANY
   UNIV E ANGLIA, UK
   INST A WEGENER, GERMANY
   UNIV PARIS 06, FRANCE
   UNIV COLORADO, USA
   NOAA, USA
   UNIV COLUMBIA, USA
   CSIRO, AUSTRALIA
   ACE CRC, AUSTRALIA
   NOAA, USA
IF 34.661
TC 307
UR https://archimer.ifremer.fr/doc/00292/40366/38974.pdf
   https://archimer.ifremer.fr/doc/00292/40366/38975.pdf
LA English
DT Article
CR OISO 8
   OISO1
   OISO2
   OISO3-NIVMER98
   OISO4 (VT 46)
   OISO5 (VT 49)
   VT 105 / OISO 17
   VT 108 / OISO-18
   VT 114 / OISO-19
   VT 117 / OISO-20
   VT 120 / OISO-21
   VT 127 / OISO-22
   VT 136 / OISO-23
   VT 142 / OISO-24
   VT 51 / OISO 6
   VT 57 / OISO 9
   VT 60 / CARAUS - OISO 10
   VT 62 / CARAUS - OISO 11
   VT 79 / OISO 12
   VT 80 / OISO 13
   VT 81 / OISO 14
   VT 85 / OISO 15
   VT 94 / OISO 16
BO Marion Dufresne
AB Several studies have suggested that the carbon sink in the Southern Ocean-the ocean's strongest region for the uptake of anthropogenic CO2-has weakened in recent decades. We demonstrated, on the basis of multidecadal analyses of surface ocean CO2 observations, that this weakening trend stopped around 2002, and by 2012 the Southern Ocean had regained its expected strength based on the growth of atmospheric CO2. All three Southern Ocean sectors have contributed to this reinvigoration of the carbon sink, yet differences in the processes between sectors exist, related to a tendency toward a zonally more asymmetric atmospheric circulation. The large decadal variations in the Southern Ocean carbon sink suggest a rather dynamic ocean carbon cycle that varies more in time than previously recognized.
PY 2015
PD SEP
SO Science
SN 0036-8075
PU Amer Assoc Advancement Science
VL 349
IS 6253
UT 000360968400042
BP 1221
EP 1224
DI 10.1126/science.aab2620
ID 40366
ER

EF