Premium
Estimates of anthropogenic carbon in the Indian Ocean with allowance for mixing and time‐varying air‐sea CO 2 disequilibrium
Author(s) -
Hall Timothy M.,
Waugh Darryn W.,
Haine Thomas W. N.,
Robbins Paul E.,
Khatiwala Samar
Publication year - 2004
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2003gb002120
Subject(s) - advection , environmental science , mixing (physics) , flux (metallurgy) , atmospheric sciences , range (aeronautics) , disequilibrium , residence time (fluid dynamics) , seawater , oceanography , climatology , geology , chemistry , physics , materials science , medicine , organic chemistry , quantum mechanics , thermodynamics , geotechnical engineering , ophthalmology , composite material
We apply to the Indian Ocean a novel technique to estimate the distribution, total mass, and net air‐sea flux of anthropogenic carbon. Chlorofluorocarbon data are used to constrain distributions of transit times from the surface to the interior that are constructed to accommodate a range of mixing scenarios, from no mixing (pure bulk advection) to strong mixing. The transit time distributions are then used to propagate to the interior the surface water history of anthropogenic carbon estimated in a way that includes temporal variation in CO 2 air‐sea disequilibrium. By allowing for mixing in transport and for variable air‐sea disequilibrium, we remove two sources of positive bias common in other studies. We estimate that the anthropogenic carbon mass in the Indian Ocean was 14.3–20.5 Gt in 2000, and the net air‐sea flux was 0.26–0.36 Gt/yr. The upper bound of this range, the no‐mixing limit, generally coincides with previous studies, while the lower bound, the strong‐mixing limit, is significantly below previous studies.