FN Archimer Export Format
PT J
TI Interannual sea–air CO2 flux variability from an observation-driven ocean mixed-layer scheme
BT 
AF ROEDENBECK, C.
   BAKKER, D. C. E.
   METZL, N.
   OLSEN, A.
   SABINE, C.
   CASSAR, N.
   REUM, F.
   KEELING, R. F.
   HEIMANN, M.
AS 1:1;2:2;3:3;4:4,5,6,7;5:8;6:9;7:1;8:10;9:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;
C1 Max Planck Inst Biogeochem, D-07745 Jena, Germany.
   Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England.
   CNRS, LOCEAN IPSL, Paris, France.
   Univ Bergen, Inst Geophys, Bergen, Norway.
   Bjerknes Ctr Climate Res, Bergen, Norway.
   Uni Res AS, Uni Climate, Bergen, Norway.
   Bjerknes Ctr Climate Res, Bergen, Norway.
   NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA.
   Duke Univ, Div Earth & Ocean Sci, Durham, NC 27706 USA.
   Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA.
C2 MAX PLANCK INST BIOGEOCHEM, GERMANY
   UNIV E ANGLIA, UK
   CNRS, FRANCE
   UNIV BERGEN, NORWAY
   BCCR, NORWAY
   UNI RES AS, NORWAY
   BCCR, NORWAY
   NOAA, USA
   UNIV DUKE, USA
   UNIV CALIF SAN DIEGO, USA
IN DOAJ
IF 3.978
TC 99
UR https://archimer.ifremer.fr/doc/00295/40594/39529.pdf
   https://archimer.ifremer.fr/doc/00295/40594/39530.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 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 Interannual anomalies in the sea–air carbon dioxide (CO2) exchange have been estimated from surface-ocean CO2 partial pressure measurements. Available data are sufficient to constrain these anomalies in large parts of the tropical and North Pacific and in the North Atlantic, in some areas covering the period from the mid 1980s to 2011. Global interannual variability is estimated as about 0.31 Pg C yr−1 (temporal standard deviation 1993–2008). The tropical Pacific accounts for a large fraction of this global variability, closely tied to El Niño–Southern Oscillation (ENSO). Anomalies occur more than 6 months later in the east than in the west. The estimated amplitude and ENSO response are roughly consistent with independent information from atmospheric oxygen data. This both supports the variability estimated from surface-ocean carbon data and demonstrates the potential of the atmospheric oxygen signal to constrain ocean biogeochemical processes. The ocean variability estimated from surface-ocean carbon data can be used to improve land CO2 flux estimates from atmospheric inversions.
PY 2014
SO Biogeosciences
SN 1726-4170
PU Copernicus Gesellschaft Mbh
VL 11
IS 17
UT 000342116000002
BP 4599
EP 4613
DI 10.5194/bg-11-4599-2014
ID 40594
ER

EF