Two decades of ocean CO2 sink and variability

2003

Article référencé dans le Web of Science WOS:000182698400048

Le Quéré C., Aumont Olivier, Bopp L., Bousquet P., Ciais P., Francey R., Heimann M., Keeling C.D., Keeling R.F., Khesghi H., Peylin P., Piper S.C., Prentice I.C., Rayner P.J.

Tellus B : Chemical and Physical Meteorology, 2003, 55B, p. 649-656 ISSN 2352-9385

International Carbon Dioxide Conference, 6., Sendaï (JPN), 2011/10/01-05

Atmospheric CO2 has increased at a nearly identical average rate of 3.3 and 3.2 Pg C yr-1 for the decades of the 1980s and the 1990s, in spite of a large increase in fossil fuel emissions from 5.4 to 6.3 Pg C yr-1 Thus, the sum of the ocean and land CO2 sinks was 1 Pg C yr-1 larger in the 1990s than in to the 1980s. Here we quantify the ocean and land sinks for these two decades using recent atmospheric inversions and ocean models. The ocean and land sinks are estimated to be, respectively, 0.3 (0.1 to 0.6) and 0.7 (0.4 to 0.9) Pg C yr-1larger in the 1990s than in the 1980s. When variability less than 5 yr is removed, all estimates show a global oceanic sink more or less steadily increasing with time, and a large anomaly in the land sink during 1990-1994. For year-to-year variability, all estimates show 1/3 to 1/2 less variability in the ocean than on land, but the amplitude and phase of the oceanic variability remain poorly determined. A mean oceanic sink of 1.9 Pg C yr-1 for the 1990s based on O2 observations corrected for ocean outgassing is supported by these estimates, but an uncertainty on the mean value of the order of +/-0.7 Pg C yr-1 remains. The difference between the two decades appears to be more robust than the absolute value of either of the two decades.

Climatologie / Météorologie [032CLIMET]

CLIMATOLOGIE ; INTERACTION OCEAN ATMOSPHERE ; GAZ CARBONIQUE ; VARIABILITE ; CYCLE BIOGEOCHIMIQUE ; PUITS ; MODELISATION

Fonds IRD [F B010078384]

fdi:010078384