The ocean carbon sink estimate in the Global Carbon Budget 2019

Hauck, Judith; Zeising, Moritz; Quéré, Corinne Le; Gruber, Nicolas; Bakker, Dorothee C E; Bopp, Laurent; Chau, Thi Tuyet Trang; Gürses, Özgür; Ilyina, Tatiana; Landschützer, Peter; Lenton, Andrew; Resplandy, Laure; Rödenbeck, Christian; Schwinger, Jörg; Séférian, Roland

doi:10.1594/pangaea.920753

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“…Air-sea CO 2 fluxes from global ocean biogeochemistry models are available from ref. 74 . MERRA2 reanalysis data are downloaded from the NASA Goddard Earth Sciences Data and Information Services Center at https://disc.gsfc.nasa.gov/datasets?project=MERRA-2 .…”

Section: Data Materials and Software Availabilitymentioning

confidence: 99%

Improved atmospheric constraints on Southern Ocean CO ₂ exchange

Jin,

Keeling,

Stephens

et al. 2024

Proc. Natl. Acad. Sci. U.S.A.

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We present improved estimates of air–sea CO 2 exchange over three latitude bands of the Southern Ocean using atmospheric CO 2 measurements from global airborne campaigns and an atmospheric 4-box inverse model based on a mass-indexed isentropic coordinate (M θe ). These flux estimates show two features not clearly resolved in previous estimates based on inverting surface CO 2 measurements: a weak winter-time outgassing in the polar region and a sharp phase transition of the seasonal flux cycles between polar/subpolar and subtropical regions. The estimates suggest much stronger summer-time uptake in the polar/subpolar regions than estimates derived through neural-network interpolation of pCO 2 data obtained with profiling floats but somewhat weaker uptake than a recent study by Long et al. [ Science 374 , 1275–1280 (2021)], who used the same airborne data and multiple atmospheric transport models (ATMs) to constrain surface fluxes. Our study also uses moist static energy (MSE) budgets from reanalyses to show that most ATMs tend to have excessive diabatic mixing (transport across moist isentrope, θ e , or M θe surfaces) at high southern latitudes in the austral summer, which leads to biases in estimates of air–sea CO 2 exchange. Furthermore, we show that the MSE-based constraint is consistent with an independent constraint on atmospheric mixing based on combining airborne and surface CO 2 observations.

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Section: Data Materials and Software Availabilitymentioning

confidence: 99%