EGU26-10681, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-10681
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 04 May, 08:50–09:00 (CEST)
 
Room N1
Underestimation of the anthropogenic carbon inventory of the Western South Atlantic Ocean linked to Antarctic Bottom Water characterization
Blanca Marigómez-Roldán1,2, Marcos Fontela1, Xosé A. Padín1, Antón Velo1, and Fiz F.Pérez1
Blanca Marigómez-Roldán et al.
  • 1Insitituto de Investigacións Mariñas, Procesos oceánicos en cambio global, Spain (bmarigomez@iim.csic.es)
  • 2Universidade de Vigo

The western South Atlantic Ocean is an important sink of anthropogenic carbon dioxide (Cant), whose deepest layers are influenced by Antarctic Bottom Water (AABW) formed at high latitudes, while also receives Cant transported by the Atlantic Meridional Overturning Circulation (AMOC) towards the Southern Ocean. The mismatch between observation and model-based estimations is a long-standing issue in the current global carbon budget but regional assessments of interior ocean Cant inventories are still limited. Recent analyses have shown that Global Ocean Biogeochemical Models (GOBMs) predictions underestimate the rates of increase of Cant in the western South Atlantic, especially in the Brazilian Basin. We contrast full-depth Cant inventories based on observations (Global Ocean Data Analysis Project, GLODAPv2.2023) against state-of-the-art GOBMs (RECCAP2) and Ocean Circulation Inverse model (OCIM) outputs. Here, we show that most the observation-based approaches, either methods that use transient tracers’ data (TRACE) or marine-carbonate-system data (Φ-method, eMLR(C*)), yield higher Cant inventories—by up to 50%—than the mean outputs from GOBMs and OCIM. The annual trend in the storage of Cant per unit area is higher in observation-based approaches (1.08 ± 0.12 mol m-2 year-1 for Φ-method, 1.18 ± 0.06 mol m-2 year-1 for eMLR(C*) and 0.66 ± 0.03 mol m-2 year-1 for TRACE) than the mean outputs from GOBMS and OCIM (0.55 ± 0.01 mol m-2 year-1). We identify the inaccurate characterization of AABW Cant concentration and extent as the main reason of disagreement. Furthermore, a limited advection of Cant from the North Atlantic to the South Atlantic by the AMOC also affects intermediate layers. This study confirms that GOBMs systematically underestimate Cant inventory in the western South Atlantic and reaffirm that high-quality deep ocean carbon observations are a requirement to avoid overlook the contribution of AABW to the global budget.

How to cite: Marigómez-Roldán, B., Fontela, M., A. Padín, X., Velo, A., and F.Pérez, F.: Underestimation of the anthropogenic carbon inventory of the Western South Atlantic Ocean linked to Antarctic Bottom Water characterization, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-10681, https://doi.org/10.5194/egusphere-egu26-10681, 2026.