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Diapycnal Mixing in the Cape Ghir upwelling region

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Diapycnal Mixing in the Cape Ghir upwelling region

Author: Rodríguez Santana, Ángel,Emelianov, Mikhail,Paka, V.,Estrada Allis, Sheila Natali,Arcos-Pulido, M.,Hernandez Arencibia, Monica,Barahona, D.,Aguiar González, Miguel Borja,Marrero Díaz, Ángeles,Fuente, P. de la,Machín, F,Pelegrí Llopart,José Luis
Year: 2012
Source: https://accedacris.ulpgc.es/jspui/bitstream/10553/10152/1/0680207_00000_0000.pdf
Geophysical Resea ch Abs ac s
Vol. 14, EGU2012-9732-3, 2012
EGU Gene al Assembly 2012
© Au ho (s) 2012
Diapycnal Mixing in he Cape Ghi upwelling egion
A. Rod íguez-San ana (1), M. Emeliano (2), V. Paka (3), S.N. Es ada-Allis (1), M. A cos-Pulido (1), M.
He nández-A encibia (1), D. Ba ahona (4), B. Aguia -González (1), A. Ma e o-Díaz (1), P. De la Fuen e (2), F.
Machín (1), and J.L. Peleg í (2)
(1) Depa amen o de Física, Uni e sidad de Las Palmas de G an Cana ia, Las Palmas de G an Cana ia, Spain
([email p o ec ed]), (2) Ins i u o de Ciencias del Ma , CSIC, Ba celona, Spain ([email p o ec ed]), (3) Shi sho
Ins i u e o Oceanology, Kalining ad, Russia ([email p o ec ed]), (4) Depa amen o de Geo ísica, Uni e sidad de
Concepción, Chile, ([email p o ec ed])
One oceanog aphic su ey was ca ied ou wi hin a p ojec mul idisciplina y (PROMECA) om 18 o 29
Oc obe 2010 in he Cana y Basin. Du ing h ee days, Conduc i i y –Tempe a u e dep h (CTD), Expandable
Ba hy e mog aph (XBT) and Mic os uc u e u bulence ( ee all p o ile s: u boMAP and Baklán) da a we e
ob ained in se e al s a ions in he Cape Ghi upwelling egion. Also du ing he c uise, eloci y da a we e measu ed
by a essel Acous ic Dopple Cu en P o ile (ADCP) wi h a e ical bin size o 8 m. The i s esul s show how
he e ical dis ibu ion o he dissipa ion a e o u bulen kine ic ene gy, ε, is modi ied by he ilamen s p esen in
he egion. These oceanog aphic s uc u es in ensi y he e ical shea o he low and modi y he e ical g adien s
o empe a u e and salini y, hus in luencing in he sou ces o mixing p ocesses associa ed (Kel in-Helmhol z
ins abili ies and double di usion). The ε alues ound ange be ween 10-7 and 10-10 W/kg in he i s 500 m o
he wa e column wi h maximum alues nea he su ace o associa ed o he ilamen s.
Wi h he dissipa ion a es o he mal a iance, χ, es ima ed om mic os uc u e da a, we a e applying a model
based in he dissipa ion a io, a io o he di usi i ies o hea and buoyancy, o es ima e he ne u bulence
di usi i ies when p ocesses o double di usion and u bulence induced by e ical shea o he low a e p esen
in he same egion.