Articles | Volume 14, issue 6
https://doi.org/10.5194/os-14-1461-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-14-1461-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
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
Roberta Sciascia
CORRESPONDING AUTHOR
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Maristella Berta
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Daniel F. Carlson
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA
Arctic Research Centre, Department of Bioscience, Aarhus University, Aarhus, Denmark
Annalisa Griffa
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Monica Panfili
Istituto per le Risorse Biologiche e le Biotecnologie Marine (IRBIM), Consiglio Nazionale delle Ricerche (CNR), Ancona,
Italy
Mario La Mesa
Istituto per le Risorse Biologiche e le Biotecnologie Marine (IRBIM), Consiglio Nazionale delle Ricerche (CNR), Ancona,
Italy
Lorenzo Corgnati
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Carlo Mantovani
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Elisa Domenella
Istituto per le Risorse Biologiche e le Biotecnologie Marine (IRBIM), Consiglio Nazionale delle Ricerche (CNR), Ancona,
Italy
Erick Fredj
Department of Computer Sciences, Jerusalem College of Technology, Jerusalem, Israel
Marcello G. Magaldi
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
Johns Hopkins University, Department of Earth and Planetary Science, Baltimore, MD, USA
Raffaele D'Adamo
Istituto per le Risorse Biologiche e le Biotecnologie Marine (IRBIM), Consiglio Nazionale delle Ricerche (CNR), Lesina, Italy
Gianfranco Pazienza
Istituto per le Risorse Biologiche e le Biotecnologie Marine (IRBIM), Consiglio Nazionale delle Ricerche (CNR), Lesina, Italy
Enrico Zambianchi
Istituto di Scienze Marine (ISMAR), Consiglio Nazionale delle Ricerche (CNR), La Spezia, Italy
DiST, Università degli Studi di Napoli ”Parthenope” and CoNISMa, Naples, Italy
Pierre-Marie Poulain
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Trieste, Italy
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Tiziana Ciuffardi, Zoi Kokkini, Maristella Berta, Marina Locritani, Andrea Bordone, Ivana Delbono, Mireno Borghini, Maurizio Demarte, Roberta Ivaldi, Federica Pannacciulli, Anna Vetrano, Davide Marini, and Giovanni Caprino
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High-frequency radar (HFR) is a land-based remote sensing technology that can provide maps of the surface circulation over broad coastal areas, along with wave and wind information. The main goal of this work is to showcase the current status of the Mediterranean HFR network as well as present and future applications of this sensor for societal benefit such as search and rescue operations, safe vessel navigation, tracking of marine pollutants, and the monitoring of extreme events.
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Here we compare and contrast results from five well-studied Arctic field sites in order to understand how glaciers affect marine biogeochemistry and marine primary production. The key questions are listed as follows. Where and when does glacial freshwater discharge promote or reduce marine primary production? How does spatio-temporal variability in glacial discharge affect marine primary production? And how far-reaching are the effects of glacial discharge on marine biogeochemistry?
John Lodise, Tamay Özgökmen, Annalisa Griffa, and Maristella Berta
Ocean Sci., 15, 1627–1651, https://doi.org/10.5194/os-15-1627-2019, https://doi.org/10.5194/os-15-1627-2019, 2019
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Observations of ocean currents within the first meter of the surface are made using a large number of ocean drifters of two different draft depths (0–5 and 0–60 cm). We deconstruct the total drifter velocities using an estimate of the regional circulation and a modeled Stokes drift velocity to calculate the purely wind-driven component of each drifter type. We reveal that the wind-driven velocities rotate to the right of the wind, while also decreasing, with depth.
Isabel Jalón-Rojas, Xiao-Hua Wang, and Erick Fredj
Ocean Sci., 15, 717–724, https://doi.org/10.5194/os-15-717-2019, https://doi.org/10.5194/os-15-717-2019, 2019
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Simplified 2-D numerical models are typically used for simulating the transport of floating microplastics. This paper demonstrates the impact of vertical mixing on the horizontal transport and fate of microplastics in a bay and therefore the importance of a 3-D approach for accurate modelling of microplastics transport. These results have important implications for the assessment and prediction of pollution hot spots in coastal systems as well as for planning effective clean-up programmes.
Charles Troupin, Ananda Pascual, Simon Ruiz, Antonio Olita, Benjamin Casas, Félix Margirier, Pierre-Marie Poulain, Giulio Notarstefano, Marc Torner, Juan Gabriel Fernández, Miquel Àngel Rújula, Cristian Muñoz, Eva Alou, Inmaculada Ruiz, Antonio Tovar-Sánchez, John T. Allen, Amala Mahadevan, and Joaquín Tintoré
Earth Syst. Sci. Data, 11, 129–145, https://doi.org/10.5194/essd-11-129-2019, https://doi.org/10.5194/essd-11-129-2019, 2019
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The AlborEX (the Alboran Sea Experiment) consisted of an experiment in the Alboran Sea (western Mediterranean Sea) that took place between 25 and 31 May 2014, and use a wide range of oceanographic sensors. The dataset provides information on mesoscale and sub-mesoscale processes taking place in a frontal area. This paper presents the measurements obtained from these sensors and describes their particularities: scale, spatial and temporal resolutions, measured variables, etc.
Maristella Berta, Lucio Bellomo, Annalisa Griffa, Marcello G. Magaldi, Anne Molcard, Carlo Mantovani, Gian Pietro Gasparini, Julien Marmain, Anna Vetrano, Laurent Béguery, Mireno Borghini, Yves Barbin, Joel Gaggelli, and Céline Quentin
Ocean Sci., 14, 689–710, https://doi.org/10.5194/os-14-689-2018, https://doi.org/10.5194/os-14-689-2018, 2018
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The Northern Current (NC) in the NW Mediterranean Sea is studied by HF radar, glider, vessel survey, wind station, and model. NC variability is dominated by synoptic response to wind events, studied decomposing geostrophic and ageostrophic surface components. The combination of autonomous observing platforms with classical marine surveys provides high-resolution datasets for scientific purposes and practical applications such as the management of marine resources in the Mediterranean Sea.
Reiner Onken, Heinz-Volker Fiekas, Laurent Beguery, Ines Borrione, Andreas Funk, Michael Hemming, Jaime Hernandez-Lasheras, Karen J. Heywood, Jan Kaiser, Michaela Knoll, Baptiste Mourre, Paolo Oddo, Pierre-Marie Poulain, Bastien Y. Queste, Aniello Russo, Kiminori Shitashima, Martin Siderius, and Elizabeth Thorp Küsel
Ocean Sci., 14, 321–335, https://doi.org/10.5194/os-14-321-2018, https://doi.org/10.5194/os-14-321-2018, 2018
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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
instruments, drifters, and one profiling float. The objective
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.
Maor Gabay, Mordechai Peleg, Erick Fredj, and Eran Tas
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2017-39, https://doi.org/10.5194/acp-2017-39, 2017
Revised manuscript not accepted
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Accurate characterization of atmospheric mercury oxidation pathways and their kinetics is critically important for assessing the transfer of atmospheric mercury to bioaquatic systems, where it can be further converted into the highly toxic biocumulative, methyl mercury. We show that nighttime oxidation of atmospheric mercury and daytime oxidation by hydroxyl radical are both more important than has been previously reported. These findings should eventually affect mercury deposition assessment.
Yosef Ashkenazy, Erick Fredj, Hezi Gildor, Gwo-Ching Gong, and Hung-Jen Lee
Ocean Sci., 12, 733–742, https://doi.org/10.5194/os-12-733-2016, https://doi.org/10.5194/os-12-733-2016, 2016
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Nan-Wan Bay in Taiwan and the Gulf of Elat in Israel are two different coastal environments, and as such, their currents are expected to have different statistical properties. We find that in spite of these differences, the statistical properties of the surface currents are similar in both basins. Still, surface currents are temporally asymmetric in Nan-Wan but not in Elat; we attribute this difference to the strong tides that exist in Nan-Wan but not in Elat.
M.-H. Rio, A. Pascual, P.-M. Poulain, M. Menna, B. Barceló, and J. Tintoré
Ocean Sci., 10, 731–744, https://doi.org/10.5194/os-10-731-2014, https://doi.org/10.5194/os-10-731-2014, 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
Computation of a new mean dynamic topography for the Mediterranean Sea from model outputs, altimeter measurements and oceanographic in situ data
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)
M.-H. Rio, A. Pascual, P.-M. Poulain, M. Menna, B. Barceló, and J. Tintoré
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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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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.
Understanding the role of ocean currents in the recruitment of commercially important fish is an...