Counteracting Contributions of the Upper and Lower Meridional Overturning Limbs to the North Atlantic Nutrient Budgets: Enhanced Imbalance in 2010. Issue 6 (11th June 2021)

• Record Type: Journal Article
• Authors: Carracedo, L. I.; Mercier, H.; McDonagh, E.; Rosón, G.; Sanders, R.; Moore, C. M.; Torres‐Valdés, S.; Brown, P.; Lherminier, P.; Pérez, F. F.
• Is Part Of: Global biogeochemical cycles. Volume 35:Issue 6(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-06-11
• Subjects: Carbon cycle -- North Atlantic -- Nutrient and oxygen transports -- Nutrient budgets -- Nutrient cycles -- Overturning circulation; Biogeochemical cycles -- Periodicals; Electronic journals; 577.1405
• DOI: 10.1029/2020GB006898
• Languages: English
• ISSNs: 0886-6236

Abstract

Abstract: The North Atlantic Basin is a major sink for atmospheric carbon dioxide (CO2 ) due in part to the extensive plankton blooms which form there supported by nutrients supplied by the three‐dimensional ocean circulation. Hence, changes in ocean circulation and/or stratification may influence primary production and biological carbon export. In this study, we assess this possibility by evaluating inorganic nutrient budgets for 2004 and 2010 in the North Atlantic based on observations from the transatlantic A05‐24.5°N and the Greenland‐Portugal OVIDE hydrographic sections, to which we applied a box inverse model to solve the circulation and estimate the across‐section nutrient transports. Full water column nutrient budgets were split into upper and lower meridional overturning circulation (MOC) limbs. According to our results, anomalous circulation in early 2010, linked to extreme negative NAO conditions, led to an enhanced northward advection of more nutrient‐rich waters by the upper overturning limb, which resulted in a significant nitrate and phosphate convergence north of 24.5°N. Combined with heaving of the isopycnals, this anomalous circulation event in 2010 favored an enhancement of the nutrient consumption (5.7 ± 4.1 kmol‐P s −1 ) and associated biological CO2 uptake (0.25 ± 0.18 Pg‐C yr −1, upper‐bound estimate), which represents a 50% of the mean annual sea–air CO2 flux in the region. Our results also suggest a transient state of deep silicate divergence in both years. Both results are indicative of a MOC‐driven modulation of the biological carbon uptake (by the upper MOC limb) and nutrient inventories (by the lower MOC limb) in the North Atlantic. Key Points: The overturning circulation lower limb drives a net southward transport of oxygen and nutrients from the North to the South Atlantic Anomalous circulation in 2010 enhanced nutrient convergence by the overturning upper limb, boosting North Atlantic biological CO2 uptake We observed a deep silicate divergence in the North Atlantic in 2004 and 2010 compatible with a transient response to reduced overturning