FN Archimer Export Format
PT J
TI Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania
BT 
AF BORGES, A. V.
   TILBROOK, B.
   METZL, N.
   LENTON, A.
   DELILLE, B.
AS 1:1;2:2,3;3:4;4:4;5:1;
FF 1:;2:;3:;4:;5:;
C1 Univ Liege, Inst Phys B5, Interfacultary Ctr Marine Res, Unit Oceanog Chim, B-4000 Liege, Belgium.
   CSIRO, Hobart, Tas 7001, Australia.
   Ecosyst Cooperat Res Ctr, Hobart, Tas 7001, Australia.
   Univ Paris 06, CNRS, Inst Pierre Simon Laplace, Oceanog Lab,UMR 7159, F-75252 Paris 5, France.
C2 UNIV LIEGE, BELGIUM
   CSIRO, AUSTRALIA
   ACE CRC, AUSTRALIA
   UNIV PARIS 06, FRANCE
IN DOAJ
IF 3.445
TC 37
UR https://archimer.ifremer.fr/doc/00238/34889/33141.pdf
LA English
DT Article
CR MINERVE 96
   MINERVE 97
   OISO3-NIVMER98
   VT 60 / CARAUS - OISO 10
BO Marion Dufresne
   L'Astrolabe
AB We compiled a large data-set from 22 cruises spanning from 1991 to 2003, of the partial pressure of CO2 (pCO(2)) in surface waters over the continental shelf (CS) and adjacent open ocean (43 degrees to 46 degrees S; 145 degrees to 150 degrees E), south of Tasmania. Climatological seasonal cycles of pCO(2) in the CS, the subtropical zone (STZ) and the subAntarctic zone (SAZ) are described and used to determine monthly pCO(2) anomalies. These are used in combination with monthly anomalies of sea surface temperature (SST) to investigate inter-annual variations of SST and pCO(2). Monthly anomalies of SST (as intense as 2 degrees C) are apparent in the CS, STZ and SAZ, and are indicative of strong inter-annual variability that seems to be related to large-scale coupled atmosphere-ocean oscillations. Anomalies of pCO(2) normalized to a constant temperature are negatively related to SST anomalies. A reduced winter-time vertical input of dissolved inorganic carbon (DIC) during phases of positive SST anomalies, related to a poleward shift of westerly winds, and a concomitant local decrease in wind stress is the likely cause of the negative relationship between pCO(2) and SST anomalies. The observed pattern is an increase of the sink for atmospheric CO2 associated with positive SST anomalies, although strongly modulated by inter-annual variability of wind speed. Assuming that phases of positive SST anomalies are indicative of the future evolution of regional ocean biogeochemistry under global warming, we show using a purely observational based approach that some provinces of the Southern Ocean could provide a potential negative feedback on increasing atmospheric CO2.
PY 2008
SO Biogeosciences
SN 1726-4170
PU Copernicus Publications
VL 5
IS 1
UT 000253673100002
BP 141
EP 155
DI 10.5194/bg-5-141-2008
ID 34889
ER

EF