Sensitivity analysis of the main methods (ΔC*, ΦCTO, TTD) used to infer the anthropogenic carbon (Cant) along the RAPID line (26°N North Atlantic latitudinal transect) on 2010.

Tobia Tudino1, Marie-Jose Messias1, Benjamin Mills2, Ute Schuster3 and Andrew J. Watson3, (1)University of Exeter, Geography, Exeter, United Kingdom, (2)University of Bristol, School of Geographical Sciences, United Kingdom, (3)University of Exeter, Exeter, United Kingdom
Abstract:
Since the beginning of the industrial revolution, human activities have represented a source for atmospheric CO2 (Cant), leading the increase of this gas from 280 to 400 ppm. Currently, the global ocean is sequestrating a quarter of this emission (~2.2 PgC/yr), particularly in key areas, such as the North Atlantic. However, a direct Cant measurement is not possible owing to its small fraction compared to the natural background. Several methods have been, then, evolved (ΔC*, ΦCTO, TTD) to derive this variable from other carbon-related measurements (alkalinity, DIC, nutrients) or using the transient tracers (CFCs and sulphur hexafluoride (SF6)). All of these methods rely on assumptions (e.g.: oceanic steady state, constant Redfield’s ratios) that introduce an uncertainty estimated as 20%. Here, a double approach based on the one at a time (OAT) and the variance-based sensitivity (VBSA) analyses has been used to assess this uncertainty and compare it among the three methods. Overall, the back-calculations (ΔC*, ΦCTO) result driven by alkalinity, DIC, temperature and oxygen with low inter parameter interactions. Their influence on the Cant distribution displays an inversion for temperature lower than 9°C, although the ΦCTO compensates this challenge using an optimum multi parameters analysis below 5°C. By contrast, the TTD approach shows constancy in the predictive parameter influence along the water column, a strong dependency on the CO2 inferred from the transit time distributions with high inter parameter interactions. To quantify the resulting variation on the Cant estimates, each predictive factor influence has been correlated with the respective analysis precision and the maximum influence determined as a percentage variation on the Cant distribution. Results display that only the DIC, alkalinity and nutrients have an influence on the back-calculations comparable with the method uncertainty, highlighting the TTD approach as the most promising in the Cant studies.