Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/895
Title: Eastern boundary drainage of the north Atlantic subtropical gyre
Authors: Pelegrí Llopart,José Luis 
Laiz Alonso, Irene
Marrero Díaz, Ángeles 
Rodríguez Santana, Ángel 
Sangrà, Pablo 
Machín, Francisco 
Hernández-Guerra, Alonso 
UNESCO Clasification: 2510 Oceanografía
Keywords: Canary Upwelling System
Eastern Boundary
Potential Vorticity
Quasigeostrophic Model
Issue Date: 2012
Journal: Ocean Dynamics 
Abstract: The eastern boundary of the North Atlantic subtropical gyre (NASG) is an upwelling favorable region characterized by a mean southward flow. The Canary Upwelling Current (CUC) feeds from the interior ocean and flows south along the continental slope off NW Africa, effectively providing the eastern boundary condition for the NASG. We follow a joint approach using slope and deep-ocean data together with process-oriented modeling to investigate the characteristics and seasonal variability of the interior-coastal ocean connection, focusing on how much NASG interior water drains along the continental slope. First, the compiled sets of data show that interior central waters flow permanently between Madeira and the Iberian Peninsula at a rate of 2.5 +/- 0.6 Sv (1 Sv = 10(6) m(3) s(-1) 10(9) km s(-1)), with most of it reaching the slope and shelf regions north of the Canary Islands (1.5 +/- 0.7 Sv). Most of the water entering the African slope and shelf regions escapes south between the easternmost Canary Islands and the African coast: In 18 out of 22 monthly realizations, the flow was southward (-0.9 +/- 0.4 Sv) although an intense flow reversal occurred usually around November (1.7 +/- 0.9 Sv), probably as the result of a late fall intensification of the CUC north of the Canary Islands followed by instability and offshore flow diversion. Secondly, we explore how the eastern boundary drainage may be specified in a process-oriented one-layer quasigeostrophic numerical model. Non-zero normal flow and constant potential vorticity are alternative eastern boundary conditions, consistent with the idea of anticyclonic vorticity induced at the boundary by coastal jets. These boundary conditions cause interior water to exit the domain at the boundary, as if recirculating through the coastal ocean, and induce substantial modifications to the shape of the eastern NASG. The best model estimate for the annual mean eastward flow north of Madeira is 3.9 Sv and at the boundary is 3.3 Sv. The water exiting at the boundary splits with 1 Sv flowing into the Strait of Gibraltar and the remaining 2.3 Sv continuing south along the coastal ocean until the latitude of Cape Ghir. The model also displays significant wind-induced seasonal variability, with a maximum connection between the interior and coastal oceans taking place in autumn and winter, in qualitative agreement with the observations.
URI: http://hdl.handle.net/10553/895
ISSN: 1616-7341
DOI: 10.1007/s10236-012-0560-6
Source: Ocean Dynamics [ISSN 1616-7341], v. 62 (9), p. 1287-1310, (Septiembre 2012)
Appears in Collections:Artículos
Show full item record

SCOPUSTM   
Citations

9
checked on Feb 21, 2021

WEB OF SCIENCETM
Citations

9
checked on Feb 21, 2021

Page view(s)

38
checked on Feb 21, 2021

Google ScholarTM

Check

Altmetric


Share



Export metadata



Items in accedaCRIS are protected by copyright, with all rights reserved, unless otherwise indicated.