The northern North Atlantic Ocean mean circulation in the early 21st Century

• Published in: Progress in Oceanography
• Main Authors: Daniault, Nathalie, Pérez, Fiz F., Ríos, Aida F., Gladyshev, Sergey
• Other Authors: Ministerio de Economía y Competitividad (España), European Commission
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2016
• Subjects: Greenland; Mid-Atlantic Ridge; Reykjanes; Irminger Sea; Rockall Trough; Rockall Plateau; West European Basin; Greenland-Scotland Ridge; Iceland; north atlantic current; North Atlantic; Northeast Atlantic
• Online Access: http://hdl.handle.net/10261/134975; https://doi.org/10.1016/j.pocean.2016.06.007; https://doi.org/10.13039/501100003329; https://doi.org/10.13039/501100000780

17 páginas, 9 figuras, 3 tablas.-- Nathalie Daniault . et al.-- Proyecto Carbochange The decadal mean circulation in the northern North Atlantic was assessed for the early 21st century from repeated ship-based measurements along the Greenland-Portugal OVIDE line, from satellite altimetry and from earlier reported transports across 59.5°N and at the Greenland-Scotland sills. The remarkable quantitative agreement between all data sets allowed us to draw circulation pathways with a high level of confidence. The North Atlantic Current (NAC) system is composed of three main branches, referred to as the northern, central and southern branches, which were traced from the Mid-Atlantic Ridge (MAR), to the Irminger Sea, the Greenland-Scotland Ridge and the subtropical gyre. At OVIDE, the northern and central branches of the NAC fill the whole water column and their top-to-bottom integrated transports were estimated at 11.0 ± 3 Sv and 14.2 ± 6.4 Sv (1 Sv = 106 m3 s−1), respectively. Those two branches feed the cyclonic circulation in the Iceland Basin and the flow over the Reykjanes Ridge into the Irminger Sea. This cross-ridge flow was estimated at 11.3 ± 4.2 Sv westward, north of 58.5°N. The southern NAC branch is strongly surface-intensified and most of its top-to-bottom integrated transport, estimated at 16.6 ± 2 Sv, is found in the upper layer. It is composed of two parts: the northern part contributes to the flow over the Rockall Plateau and through the Rockall Trough toward the Iceland-Scotland Ridge; the southern part feeds the anticyclonic circulation toward the subtropical gyre. Summing over the three NAC branches, the top-to-bottom transport of the NAC across OVIDE was estimated at 41.8 ± 3.7 Sv. Because of the surface-intensification of the southern NAC branch, the intermediate water is transported to the northeast Atlantic mostly by the northern and central branches of the NAC (11.9 ± 1.8 Sv eastward). This water circulates cyclonically in the Iceland Basin and anticyclonically in the West European Basin, ...