Articles | Volume 18, issue 4
https://doi.org/10.5194/os-18-1055-2022
https://doi.org/10.5194/os-18-1055-2022
Research article
 | 
15 Jul 2022
Research article |  | 15 Jul 2022

Deep through-flow in the Bight Fracture Zone

Tillys Petit, Virginie Thierry, and Herlé Mercier

Data sets

Reykjanes Ridge Experiment (RREX) dataset V. Thierry, H. Mercier, T. Petit, P. Branellec, K. Balem, and P. Lherminier https://doi.org/10.17882/55445

Carbon Dioxide, Hydrographic, and Chemical Data Obtained During the R/V Sarmiento de Gamboa Cruise in the North Atlantic Ocean on CLIVAR Repeat Hydrography Section OVIDE-2016-BOCATS F. F. Pérez, M. I. García-Ibáñez, M. Fontela, P. Lherminier, P. Branellec, P. Zunino, F. Alonso Pérez, M. de la Paz, and X. A. Padín https://digital.csic.es/handle/10261/154341

GO-SHIP A25 - OVIDE 2018 Cruise data P. Lherminier, F. F. Perez, P. Branellec, H. Mercier, A. Velo, M. Messias, M. Castrillejo, G. Reverdin, M. Fontela, and F. Baurand https://doi.org/10.17882/87394

Argo float data and metadata from Global Data Assembly Centre (Argo GDAC) Argo https://doi.org/10.17882/42182

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Short summary
The Iceland–Scotland Overflow Water is a dense water carried within the lower limb of the Atlantic Meridional Overturning Circulation. From a combination of ship-based and Deep-Argo data gathered between 2015 and 2018, our study analyzes the pathways and evolution of its properties as it flows through a main fracture of the Reykjanes Ridge, the Bight Fracture Zone (BFZ). We show that 0.8 ± 0.2 Sv of ISOW flows through the BFZ and is mainly homogenized within the rift valley of the ridge.