| Range |
0.74×10^14 - 1.75×10^14 mol CO2/year
|
| Organism |
Biosphere |
| Reference |
Duursma EK, Boisson MPRM, Global oceanic and atmospheric oxygen stability considered in relation to the carbon-cycle and to different time scales. Oceanologica Acta (0399-1784) (Gauthier-Villars), 1994 , Vol. 17 , N. 2 , P. 117-141 link p.126 left column 2nd paragraph |
| Primary Source |
Etcheto J. and L. Merlivat (1988). Satellite determination of the carbon dioxide exchange coefficient at the ocean-atmosphere interface: a first step. J. geophys. Res., 93, 669-678 link AND Merlivat L. J. Etcheto and J. Houtin (1991). CO2 exchange at the air-sea interface: time and space variability Cospar Proceedings, Atmos. Space Res., 11, 3, 77-85 link AND Quay PD, Tilbrook B, Wong CS. Oceanic Uptake of Fossil Fuel CO2: Carbon-13 Evidence. Science. 1992 Apr 3 256(5053):74-9. DOI: 10.1126/science.256.5053.74 PubMed ID17802595
|
| Comments |
P.126 left column 2nd paragraph: "The net CO2 flux into the oceans is determined at 0.975 x 10^14 mol CO2/yr (primary source Etcheto and Merlivat, 1988), while other literature data range from 0.74 x 10^14 mol CO2/yr (cited by primary source Merlivat et al., 1991) to 1.75 x 10^14 mol CO2/yr [primary source Quay et al., 1992 (Fig. 4 A and Tab. 3 B)]." |
| Entered by |
Uri M |
| ID |
116102 |