Evidence of double diffusion in the Brazil-Malvinas Confluence

Observation of thermohaline staircases and low-density ratios in the Brazil-Malvinas Confluence (BMC) suggests salt-fingering activity between the high salinity South Atlantic Central Water and low salinity Antarctic Intermediate Water. Vertical salt-finger induced salt fluxes are estimated in the B...

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Autores principales: Bianchi, A.A., Piola, A.R., Collino, G.J.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_09670637_v49_n1_p41_Bianchi
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spelling todo:paper_09670637_v49_n1_p41_Bianchi2023-10-03T15:55:00Z Evidence of double diffusion in the Brazil-Malvinas Confluence Bianchi, A.A. Piola, A.R. Collino, G.J. Brazil/Malvinas Confluence Double diffusion Mixing Salt finger Southwestern Atlantic Salinity measurement Seawater Thermal diffusion Baroclinicity Oceanography double diffusion fingering salinity vertical mixing water mass Atlantic Ocean Observation of thermohaline staircases and low-density ratios in the Brazil-Malvinas Confluence (BMC) suggests salt-fingering activity between the high salinity South Atlantic Central Water and low salinity Antarctic Intermediate Water. Vertical salt-finger induced salt fluxes are estimated in the BMC using a model for fastest growing fingers. Maximum salt-finger fluxes of 39.9 × 10-10 W kg-1 (5.3 × 10-7 m s-1) were estimated, similar to existing estimates in a Mediterranean salt lens embedded within the North Atlantic water. The fluxes normalized by the large-scale property gradients lead to fairly large estimates of diapycnal haline and thermal diffusivities, of up to 0.74 × 10-4 and 0.34 × 10-4 m2s-1, respectively, showing the enhancement of the haline diffusivity due to salt fingers. Estimated diffusive-convection fluxes based on flux laws derived from laboratory experiments are two orders of magnitude larger than salt-finger fluxes. These results suggest that, where cross-front interleaving leads to layering of relatively cold-fresh water over warm-salty water, diffusive upward convection dominates the vertical property fluxes in the frontal region. It appears that on the warm-salty side of the BMC, away from the narrow band dominated by interleaving, salt-finger integrated vertical fluxes nearly balance the cross-front lateral integrated fluxes. The effect of baroclinicity on the vertical property fluxes was evaluated and it was found that, in the BMC, the baroclinicity enhances the interleaving. © 2001 Elsevier Science Ltd. All rights reserved. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_09670637_v49_n1_p41_Bianchi
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Brazil/Malvinas Confluence
Double diffusion
Mixing
Salt finger
Southwestern Atlantic
Salinity measurement
Seawater
Thermal diffusion
Baroclinicity
Oceanography
double diffusion
fingering
salinity
vertical mixing
water mass
Atlantic Ocean
spellingShingle Brazil/Malvinas Confluence
Double diffusion
Mixing
Salt finger
Southwestern Atlantic
Salinity measurement
Seawater
Thermal diffusion
Baroclinicity
Oceanography
double diffusion
fingering
salinity
vertical mixing
water mass
Atlantic Ocean
Bianchi, A.A.
Piola, A.R.
Collino, G.J.
Evidence of double diffusion in the Brazil-Malvinas Confluence
topic_facet Brazil/Malvinas Confluence
Double diffusion
Mixing
Salt finger
Southwestern Atlantic
Salinity measurement
Seawater
Thermal diffusion
Baroclinicity
Oceanography
double diffusion
fingering
salinity
vertical mixing
water mass
Atlantic Ocean
description Observation of thermohaline staircases and low-density ratios in the Brazil-Malvinas Confluence (BMC) suggests salt-fingering activity between the high salinity South Atlantic Central Water and low salinity Antarctic Intermediate Water. Vertical salt-finger induced salt fluxes are estimated in the BMC using a model for fastest growing fingers. Maximum salt-finger fluxes of 39.9 × 10-10 W kg-1 (5.3 × 10-7 m s-1) were estimated, similar to existing estimates in a Mediterranean salt lens embedded within the North Atlantic water. The fluxes normalized by the large-scale property gradients lead to fairly large estimates of diapycnal haline and thermal diffusivities, of up to 0.74 × 10-4 and 0.34 × 10-4 m2s-1, respectively, showing the enhancement of the haline diffusivity due to salt fingers. Estimated diffusive-convection fluxes based on flux laws derived from laboratory experiments are two orders of magnitude larger than salt-finger fluxes. These results suggest that, where cross-front interleaving leads to layering of relatively cold-fresh water over warm-salty water, diffusive upward convection dominates the vertical property fluxes in the frontal region. It appears that on the warm-salty side of the BMC, away from the narrow band dominated by interleaving, salt-finger integrated vertical fluxes nearly balance the cross-front lateral integrated fluxes. The effect of baroclinicity on the vertical property fluxes was evaluated and it was found that, in the BMC, the baroclinicity enhances the interleaving. © 2001 Elsevier Science Ltd. All rights reserved.
format JOUR
author Bianchi, A.A.
Piola, A.R.
Collino, G.J.
author_facet Bianchi, A.A.
Piola, A.R.
Collino, G.J.
author_sort Bianchi, A.A.
title Evidence of double diffusion in the Brazil-Malvinas Confluence
title_short Evidence of double diffusion in the Brazil-Malvinas Confluence
title_full Evidence of double diffusion in the Brazil-Malvinas Confluence
title_fullStr Evidence of double diffusion in the Brazil-Malvinas Confluence
title_full_unstemmed Evidence of double diffusion in the Brazil-Malvinas Confluence
title_sort evidence of double diffusion in the brazil-malvinas confluence
url http://hdl.handle.net/20.500.12110/paper_09670637_v49_n1_p41_Bianchi
work_keys_str_mv AT bianchiaa evidenceofdoublediffusioninthebrazilmalvinasconfluence
AT piolaar evidenceofdoublediffusioninthebrazilmalvinasconfluence
AT collinogj evidenceofdoublediffusioninthebrazilmalvinasconfluence
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