Published in

Stockholm University Press, Tellus B: Chemical and Physical Meteorology, 2(55), p. 649-656, 2003

DOI: 10.1034/j.1600-0889.2003.00043.x

Links

Tools

Export citation

Search in Google Scholar

Two decades of ocean CO2 sink and variability

This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

Full text: Download

Green circle
Preprint: archiving allowed
Green circle
Postprint: archiving allowed
Green circle
Published version: archiving allowed
Data provided by SHERPA/RoMEO

Abstract

Atmospheric CO 2 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 CO 2 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 -1 larger 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 O 2 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.