Articles | Volume 10, issue 4
https://doi.org/10.5194/os-10-731-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-10-731-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
18 Aug 2014
Research article |
| 18 Aug 2014
Computation of a new mean dynamic topography for the Mediterranean Sea from model outputs, altimeter measurements and oceanographic in situ data
M.-H. Rio
CLS Space Oceanography Division, Ramonville-Ste Agne, France
A. Pascual
IMEDEA(CSIC-UIB), Esporles, Spain
P.-M. Poulain
OGS, Trieste, Italy
M. Menna
OGS, Trieste, Italy
B. Barceló
IMEDEA(CSIC-UIB), Esporles, Spain
J. Tintoré
IMEDEA(CSIC-UIB), Esporles, Spain
SOCIB, Palma, Spain
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Roberta Sciascia, Maristella Berta, Daniel F. Carlson, Annalisa Griffa, Monica Panfili, Mario La Mesa, Lorenzo Corgnati, Carlo Mantovani, Elisa Domenella, Erick Fredj, Marcello G. Magaldi, Raffaele D'Adamo, Gianfranco Pazienza, Enrico Zambianchi, and Pierre-Marie Poulain
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In June 2014, high-resolution oceanographic data were collected in the
western Mediterranean Sea by two research vessels, 11 gliders, moored
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of this article is to provide an overview of the data set which
is utilised by various ongoing studies, focusing on (i) water masses and circulation, (ii) operational forecasting, (iii) data assimilation, (iv) variability of the ocean, and (v) new payloads
for gliders.
Ivica Vilibić, Hrvoje Mihanović, Ivica Janeković, Cléa Denamiel, Pierre-Marie Poulain, Mirko Orlić, Natalija Dunić, Vlado Dadić, Mira Pasarić, Stipe Muslim, Riccardo Gerin, Frano Matić, Jadranka Šepić, Elena Mauri, Zoi Kokkini, Martina Tudor, Žarko Kovač, and Tomislav Džoić
Ocean Sci., 14, 237–258, https://doi.org/10.5194/os-14-237-2018, https://doi.org/10.5194/os-14-237-2018, 2018
Maher Bouzaiene, Milena Menna, Pierre-Marie Poulain, and Dalila Elhmaidi
Ocean Sci. Discuss., https://doi.org/10.5194/os-2017-34, https://doi.org/10.5194/os-2017-34, 2017
Preprint withdrawn
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The South Western Mediterranean, connected to the Atlantic Ocean through the Strait of Gibraltar, is a study area useful to describe the interaction between the light Atlantic Water and the denser Mediterranean Water. The spreading of fluid particles, estimated through the analysis of drifter data, is dominated by large mesoscale eddies at short times and small separation distances, and by small mesoscale structures for scale ranging between 3 and 11 km.
Antonio Sánchez-Román, Simón Ruiz, Ananda Pascual, Baptiste Mourre, and Stéphanie Guinehut
Ocean Sci., 13, 223–234, https://doi.org/10.5194/os-13-223-2017, https://doi.org/10.5194/os-13-223-2017, 2017
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In this work we investigate the capability of the Argo array in the Mediterranean Sea to capture mesoscale circulation structures (diameter of around 150 km). To do that we conduct several experiments to simulate different spatial sampling configurations of the Argo array in the basin. Results show that the actual Argo array in the Mediterranean (2° × 2°) might be enlarged until a spatial resolution of nearly 75 × 75 km (450 floats) in order to capture the mesoscale signal.
Bàrbara Barceló-Llull, Evan Mason, Arthur Capet, and Ananda Pascual
Ocean Sci., 12, 1003–1011, https://doi.org/10.5194/os-12-1003-2016, https://doi.org/10.5194/os-12-1003-2016, 2016
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Vertical velocity in the ocean makes an important contribution to the modulation of marine ecosystems through its impact on fluxes of nutrients and phytoplankton. Here, we estimate full 3-D current velocity fields from an observation-based data product. The 3-D currents are used to force a set of particle-tracking (Lagrangian) experiments. The Lagrangian results show that vertical motions induce local increases in nitrate uptake reaching up to 30 %.
Marcos García Sotillo, Emilio Garcia-Ladona, Alejandro Orfila, Pablo Rodríguez-Rubio, José Cristobal Maraver, Daniel Conti, Elena Padorno, José Antonio Jiménez, Este Capó, Fernando Pérez, Juan Manuel Sayol, Francisco Javier de los Santos, Arancha Amo, Ana Rietz, Charles Troupin, Joaquín Tintore, and Enrique Álvarez-Fanjul
Earth Syst. Sci. Data, 8, 141–149, https://doi.org/10.5194/essd-8-141-2016, https://doi.org/10.5194/essd-8-141-2016, 2016
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An intensive drifter deployment was carried out in the Strait of Gibraltar: 35 satellite tracked drifters were released, coordinating to this aim 4 boats, covering an area of about 680 NM2 in 6 hours. This MEDESS-GIB Experiment is the most important exercise in the Mediterranean in terms of number of drifters released. The MEDESS-GIB dataset provides a complete Lagrangian view of the surface inflow of Atlantic waters through the Strait of Gibraltar and its later evolution along the Alboran Sea.
L. Shabrang, M. Menna, C. Pizzi, H. Lavigne, G. Civitarese, and M. Gačić
Ocean Sci., 12, 233–241, https://doi.org/10.5194/os-12-233-2016, https://doi.org/10.5194/os-12-233-2016, 2016
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The interannual variation of the strength of the SAG in relation to NAO was studied. The intensity of the gyre is associated with the large-scale climatic variations via the wind-stress curl forcing. However due to the rather important contribution of the vorticity advection from the Ionian, which is more significant during the anticyclonic BiOS, there is no clear evidence of a direct effect of large-scale atmospheric circulation (NAO) on the interannual variability of the intensity of the SAG.
F. d'Ovidio, A. Della Penna, T. W. Trull, F. Nencioli, M.-I. Pujol, M.-H. Rio, Y.-H. Park, C. Cotté, M. Zhou, and S. Blain
Biogeosciences, 12, 5567–5581, https://doi.org/10.5194/bg-12-5567-2015, https://doi.org/10.5194/bg-12-5567-2015, 2015
Short summary
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Field campaigns are instrumental in providing ground truth for understanding and modeling global ocean biogeochemical budgets. A survey however can only inspect a fraction of the global oceans, typically a region hundreds of kilometers wide for a temporal window of the order of (at most) several weeks. In this spatiotemporal domain, mesoscale variability can mask climatological contrasts. Here we propose the use of multisatellite-based Lagrangian diagnostics to solve this issue.
A. Olita, S. Sparnocchia, S. Cusí, L. Fazioli, R. Sorgente, J. Tintoré, and A. Ribotti
Ocean Sci., 10, 657–666, https://doi.org/10.5194/os-10-657-2014, https://doi.org/10.5194/os-10-657-2014, 2014
M. Gačić, G. Civitarese, V. Kovačević, L. Ursella, M. Bensi, M. Menna, V. Cardin, P.-M. Poulain, S. Cosoli, G. Notarstefano, and C. Pizzi
Ocean Sci., 10, 513–522, https://doi.org/10.5194/os-10-513-2014, https://doi.org/10.5194/os-10-513-2014, 2014
P. Malanotte-Rizzoli, V. Artale, G. L. Borzelli-Eusebi, S. Brenner, A. Crise, M. Gacic, N. Kress, S. Marullo, M. Ribera d'Alcalà, S. Sofianos, T. Tanhua, A. Theocharis, M. Alvarez, Y. Ashkenazy, A. Bergamasco, V. Cardin, S. Carniel, G. Civitarese, F. D'Ortenzio, J. Font, E. Garcia-Ladona, J. M. Garcia-Lafuente, A. Gogou, M. Gregoire, D. Hainbucher, H. Kontoyannis, V. Kovacevic, E. Kraskapoulou, G. Kroskos, A. Incarbona, M. G. Mazzocchi, M. Orlic, E. Ozsoy, A. Pascual, P.-M. Poulain, W. Roether, A. Rubino, K. Schroeder, J. Siokou-Frangou, E. Souvermezoglou, M. Sprovieri, J. Tintoré, and G. Triantafyllou
Ocean Sci., 10, 281–322, https://doi.org/10.5194/os-10-281-2014, https://doi.org/10.5194/os-10-281-2014, 2014
M. Menna and P.-M. Poulain
Ocean Sci., 10, 155–165, https://doi.org/10.5194/os-10-155-2014, https://doi.org/10.5194/os-10-155-2014, 2014
P.-M. Poulain and S. Hariri
Ocean Sci., 9, 713–720, https://doi.org/10.5194/os-9-713-2013, https://doi.org/10.5194/os-9-713-2013, 2013
Related subject area
Approach: In situ Observations | Depth range: Surface | Geographical range: Mediterranean Sea | Phenomena: Current Field
Linking sardine recruitment in coastal areas to ocean currents using surface drifters and HF radar: a case study in the Gulf of Manfredonia, Adriatic Sea
Geostrophic currents and kinetic energies in the Black Sea estimated from merged drifter and satellite altimetry data
Transit and residence times in the Adriatic Sea surface as derived from drifter data and Lagrangian numerical simulations
Surface circulation in the Eastern Mediterranean using drifters (2005–2007)
Roberta Sciascia, Maristella Berta, Daniel F. Carlson, Annalisa Griffa, Monica Panfili, Mario La Mesa, Lorenzo Corgnati, Carlo Mantovani, Elisa Domenella, Erick Fredj, Marcello G. Magaldi, Raffaele D'Adamo, Gianfranco Pazienza, Enrico Zambianchi, and Pierre-Marie Poulain
Ocean Sci., 14, 1461–1482, https://doi.org/10.5194/os-14-1461-2018, https://doi.org/10.5194/os-14-1461-2018, 2018
Short summary
Short summary
Understanding the role of ocean currents in the recruitment of commercially important fish is an important step toward developing sustainable resource management guidelines. Here, we attempt to elucidate the role of surface ocean transport in supplying recruits of European sardines to the Gulf of Manfredonia, a known recruitment area in the Adriatic Sea. We find that transport to the Gulf of Manfredonia from remote spawing areas in the Adriatic is more likely than local spawning and retention.
M. Menna and P.-M. Poulain
Ocean Sci., 10, 155–165, https://doi.org/10.5194/os-10-155-2014, https://doi.org/10.5194/os-10-155-2014, 2014
P.-M. Poulain and S. Hariri
Ocean Sci., 9, 713–720, https://doi.org/10.5194/os-9-713-2013, https://doi.org/10.5194/os-9-713-2013, 2013
R. Gerin, P.-M. Poulain, I. Taupier-Letage, C. Millot, S. Ben Ismail, and C. Sammari
Ocean Sci., 5, 559–574, https://doi.org/10.5194/os-5-559-2009, https://doi.org/10.5194/os-5-559-2009, 2009
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