HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean

Claude Estournel; Pierre Testor; Isabelle Taupier-Letage; Marie-Noelle Bouin; Laurent Coppola; Pierre Durand; Pascal Conan; Anthony Bosse; Pierre-Etienne Brilouet; Laurent Beguery; Sophie Belamari; Karine Béranger; Jonathan Beuvier; Denis Bourras; Guylaine Canut; Alexis Doerenbecher; Xavier Durrieu de Madron; Fabrizio D'Ortenzio; Philippe Drobinski; Véronique Ducrocq; Nadia Fourrié; Hervé Giordani; Loic Houpert; Laurent Labatut; Cindy Lebeaupin Brossier; Mathieu Nuret; Louis Prieur; Odile Roussot; Leo Seyfried; Samuel Somot

doi:10.5670/oceanog.2016.94

HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean

Claude Estournel
, Pierre Testor
, Isabelle Taupier-Letage
, Marie-Noelle Bouin
, Laurent Coppola
, Pierre Durand
, Pascal Conan
, Anthony Bosse
, Pierre-Etienne Brilouet
, Laurent Beguery
, Sophie Belamari
, Karine Béranger
, Jonathan Beuvier
, Denis Bourras
, Guylaine Canut
, Alexis Doerenbecher
, Xavier Durrieu de Madron
, Fabrizio D'Ortenzio
, Philippe Drobinski
, Véronique Ducrocq

Nadia Fourrié, Hervé Giordani, Loic Houpert, Laurent Labatut, Cindy Lebeaupin Brossier, Mathieu Nuret, Louis Prieur, Odile Roussot, Leo Seyfried, Samuel Somot

SAMS UHI

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Abstract

The HYdrological cycle in the Mediterranean Experiment (HyMeX) Special Observing Period 2 (SOP2, January 27–March 15, 2013) was dedicated to the study of dense water formation in the Gulf of Lion in the northwestern Mediterranean. This paper outlines the deep convection of winter 2012–2013 and the meteorological conditions that produced it. Alternating phases of mixing and restratification are related to periods of high and low heat losses, respectively. High-resolution, realistic, three-dimensional models are essential for assessing the intricacy of buoyancy fluxes, horizontal advection, and convective processes. At the submesoscale, vertical velocities resulting from symmetric instabilities of the density front bounding the convection zone are crucial for ventilating the deep ocean. Finally, concomitant atmospheric and oceanic data extracted from the comprehensive SOP2 data set highlight the rapid, coupled evolution of oceanic and atmospheric boundary layer characteristics during a strong wind event.

Originalsprache	English
Seiten (von - bis)	196-206
Seitenumfang	10
Fachzeitschrift	Oceanography
Jahrgang	29
Ausgabenummer	4
DOIs	https://doi.org/10.5670/oceanog.2016.94
Publikationsstatus	Published - 1 Dez. 2016

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10.5670/oceanog.2016.94Lizenz: CC BY

estournel2016oceanography
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Estournel, C., Testor, P., Taupier-Letage, I., Bouin, M.-N., Coppola, L., Durand, P., Conan, P., Bosse, A., Brilouet, P.-E., Beguery, L., Belamari, S., Béranger, K., Beuvier, J., Bourras, D., Canut, G., Doerenbecher, A., Durrieu de Madron, X., D'Ortenzio, F., Drobinski, P., ... Somot, S. (2016). HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean. Oceanography, 29(4), 196-206. https://doi.org/10.5670/oceanog.2016.94

@article{108a7a8964a84d5e870cef8277b93f91,

title = "HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean",

abstract = "The HYdrological cycle in the Mediterranean Experiment (HyMeX) Special Observing Period 2 (SOP2, January 27–March 15, 2013) was dedicated to the study of dense water formation in the Gulf of Lion in the northwestern Mediterranean. This paper outlines the deep convection of winter 2012–2013 and the meteorological conditions that produced it. Alternating phases of mixing and restratification are related to periods of high and low heat losses, respectively. High-resolution, realistic, three-dimensional models are essential for assessing the intricacy of buoyancy fluxes, horizontal advection, and convective processes. At the submesoscale, vertical velocities resulting from symmetric instabilities of the density front bounding the convection zone are crucial for ventilating the deep ocean. Finally, concomitant atmospheric and oceanic data extracted from the comprehensive SOP2 data set highlight the rapid, coupled evolution of oceanic and atmospheric boundary layer characteristics during a strong wind event.",

author = "Claude Estournel and Pierre Testor and Isabelle Taupier-Letage and Marie-Noelle Bouin and Laurent Coppola and Pierre Durand and Pascal Conan and Anthony Bosse and Pierre-Etienne Brilouet and Laurent Beguery and Sophie Belamari and Karine B{\'e}ranger and Jonathan Beuvier and Denis Bourras and Guylaine Canut and Alexis Doerenbecher and \{Durrieu de Madron\}, Xavier and Fabrizio D'Ortenzio and Philippe Drobinski and V{\'e}ronique Ducrocq and Nadia Fourri{\'e} and Herv{\'e} Giordani and Loic Houpert and Laurent Labatut and \{Lebeaupin Brossier\}, Cindy and Mathieu Nuret and Louis Prieur and Odile Roussot and Leo Seyfried and Samuel Somot",

year = "2016",

month = dec,

day = "1",

doi = "10.5670/oceanog.2016.94",

language = "English",

volume = "29",

pages = "196--206",

journal = "Oceanography",

publisher = "Oceanography Society",

number = "4",

}

Estournel, C, Testor, P, Taupier-Letage, I, Bouin, M-N, Coppola, L, Durand, P, Conan, P, Bosse, A, Brilouet, P-E, Beguery, L, Belamari, S, Béranger, K, Beuvier, J, Bourras, D, Canut, G, Doerenbecher, A, Durrieu de Madron, X, D'Ortenzio, F, Drobinski, P, Ducrocq, V, Fourrié, N, Giordani, H, Houpert, L, Labatut, L, Lebeaupin Brossier, C, Nuret, M, Prieur, L, Roussot, O, Seyfried, L & Somot, S 2016, 'HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean', Oceanography, Jg. 29, Nr. 4, S. 196-206. https://doi.org/10.5670/oceanog.2016.94

TY - JOUR

T1 - HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean

AU - Estournel, Claude

AU - Testor, Pierre

AU - Taupier-Letage, Isabelle

AU - Bouin, Marie-Noelle

AU - Coppola, Laurent

AU - Durand, Pierre

AU - Conan, Pascal

AU - Bosse, Anthony

AU - Brilouet, Pierre-Etienne

AU - Beguery, Laurent

AU - Belamari, Sophie

AU - Béranger, Karine

AU - Beuvier, Jonathan

AU - Bourras, Denis

AU - Canut, Guylaine

AU - Doerenbecher, Alexis

AU - Durrieu de Madron, Xavier

AU - D'Ortenzio, Fabrizio

AU - Drobinski, Philippe

AU - Ducrocq, Véronique

AU - Fourrié, Nadia

AU - Giordani, Hervé

AU - Houpert, Loic

AU - Labatut, Laurent

AU - Lebeaupin Brossier, Cindy

AU - Nuret, Mathieu

AU - Prieur, Louis

AU - Roussot, Odile

AU - Seyfried, Leo

AU - Somot, Samuel

PY - 2016/12/1

Y1 - 2016/12/1

N2 - The HYdrological cycle in the Mediterranean Experiment (HyMeX) Special Observing Period 2 (SOP2, January 27–March 15, 2013) was dedicated to the study of dense water formation in the Gulf of Lion in the northwestern Mediterranean. This paper outlines the deep convection of winter 2012–2013 and the meteorological conditions that produced it. Alternating phases of mixing and restratification are related to periods of high and low heat losses, respectively. High-resolution, realistic, three-dimensional models are essential for assessing the intricacy of buoyancy fluxes, horizontal advection, and convective processes. At the submesoscale, vertical velocities resulting from symmetric instabilities of the density front bounding the convection zone are crucial for ventilating the deep ocean. Finally, concomitant atmospheric and oceanic data extracted from the comprehensive SOP2 data set highlight the rapid, coupled evolution of oceanic and atmospheric boundary layer characteristics during a strong wind event.

AB - The HYdrological cycle in the Mediterranean Experiment (HyMeX) Special Observing Period 2 (SOP2, January 27–March 15, 2013) was dedicated to the study of dense water formation in the Gulf of Lion in the northwestern Mediterranean. This paper outlines the deep convection of winter 2012–2013 and the meteorological conditions that produced it. Alternating phases of mixing and restratification are related to periods of high and low heat losses, respectively. High-resolution, realistic, three-dimensional models are essential for assessing the intricacy of buoyancy fluxes, horizontal advection, and convective processes. At the submesoscale, vertical velocities resulting from symmetric instabilities of the density front bounding the convection zone are crucial for ventilating the deep ocean. Finally, concomitant atmospheric and oceanic data extracted from the comprehensive SOP2 data set highlight the rapid, coupled evolution of oceanic and atmospheric boundary layer characteristics during a strong wind event.

U2 - 10.5670/oceanog.2016.94

DO - 10.5670/oceanog.2016.94

M3 - Article

VL - 29

SP - 196

EP - 206

JO - Oceanography

JF - Oceanography

IS - 4

ER -

HyMeX-SOP2: The Field Campaign Dedicated to Dense Water Formation in the Northwestern Mediterranean

Abstract

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