A probabilistic assessment of calcium carbonate export and dissolution in the modern ocean

• Published in: Biogeosciences
• Main Authors: G. Battaglia, M. Steinacher, F. Joos
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2016
• Subjects: Ecology; QH540-549.5; Life; QH501-531; Geology; QE1-996.5; Pacific; Southern Ocean
• Online Access: https://doi.org/10.5194/bg-13-2823-2016; https://doaj.org/article/2e979bc700f74adf8fee65c799cf8bb6

The marine cycle of calcium carbonate (CaCO 3 ) is an important element of the carbon cycle and co-governs the distribution of carbon and alkalinity within the ocean. However, CaCO 3 export fluxes and mechanisms governing CaCO 3 dissolution are highly uncertain. We present an observationally constrained, probabilistic assessment of the global and regional CaCO 3 budgets. Parameters governing pelagic CaCO 3 export fluxes and dissolution rates are sampled using a Monte Carlo scheme to construct a 1000-member ensemble with the Bern3D ocean model. Ensemble results are constrained by comparing simulated and observation-based fields of excess dissolved calcium carbonate (TA*). The minerals calcite and aragonite are modelled explicitly and ocean–sediment fluxes are considered. For local dissolution rates, either a strong or a weak dependency on CaCO 3 saturation is assumed. In addition, there is the option to have saturation-independent dissolution above the saturation horizon. The median (and 68 % confidence interval) of the constrained model ensemble for global biogenic CaCO 3 export is 0.90 (0.72–1.05) Gt C yr −1 , that is within the lower half of previously published estimates (0.4–1.8 Gt C yr −1 ). The spatial pattern of CaCO 3 export is broadly consistent with earlier assessments. Export is large in the Southern Ocean, the tropical Indo–Pacific, the northern Pacific and relatively small in the Atlantic. The constrained results are robust across a range of diapycnal mixing coefficients and, thus, ocean circulation strengths. Modelled ocean circulation and transport timescales for the different set-ups were further evaluated with CFC11 and radiocarbon observations. Parameters and mechanisms governing dissolution are hardly constrained by either the TA* data or the current compilation of CaCO 3 flux measurements such that model realisations with and without saturation-dependent dissolution achieve skill. We suggest applying saturation-independent dissolution rates in Earth system models to minimise computational ...