Articles | Volume 20, issue 6
https://doi.org/10.5194/os-20-1707-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/os-20-1707-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Monitoring the coastal–offshore water interactions in the Levantine Sea using ocean color and deep supervised learning
Georges Baaklini
CORRESPONDING AUTHOR
LOCEAN Laboratory, Sorbonne University, UPMC Univ Paris 06 CNRS-IRD-MNHN, 4 place Jussieu, 75005 Paris, France
Julien Brajard
Nansen Environmental and Remote Sensing Center, Bergen, Norway
Leila Issa
Department of Computer Science and Mathematics, Lebanese American University, Beirut, Lebanon
Gina Fifani
LOCEAN Laboratory, Sorbonne University, UPMC Univ Paris 06 CNRS-IRD-MNHN, 4 place Jussieu, 75005 Paris, France
Laurent Mortier
LOCEAN Laboratory, Sorbonne University, UPMC Univ Paris 06 CNRS-IRD-MNHN, 4 place Jussieu, 75005 Paris, France
Roy El Hourany
Laboratoire d'Océanologie et de Géosciences, Univ. Littoral Côte d'Opale, Univ. Lille, CNRS, IRD, UMR 8187, LOG, 62930 Wimereux, France
Related authors
Georges Baaklini, Roy El Hourany, Milad Fakhri, Julien Brajard, Leila Issa, Gina Fifani, and Laurent Mortier
Ocean Sci., 18, 1491–1505, https://doi.org/10.5194/os-18-1491-2022, https://doi.org/10.5194/os-18-1491-2022, 2022
Short summary
Short summary
We use machine learning to analyze the long-term variation of the surface currents in the Levantine Sea, located in the eastern Mediterranean Sea. We decompose the circulation into groups based on their physical characteristics and analyze their spatial and temporal variability. We show that most structures of the Levantine Sea are becoming more energetic over time, despite those of the western area remaining the most dominant due to their complex bathymetry and strong currents.
Alexander Barth, Julien Brajard, Aida Alvera-Azcárate, Bayoumy Mohamed, Charles Troupin, and Jean-Marie Beckers
Ocean Sci., 20, 1567–1584, https://doi.org/10.5194/os-20-1567-2024, https://doi.org/10.5194/os-20-1567-2024, 2024
Short summary
Short summary
Most satellite observations have gaps, for example, due to clouds. This paper presents a method to reconstruct missing data in satellite observations of the chlorophyll a concentration in the Black Sea. Rather than giving a single possible reconstructed field, the discussed method provides an ensemble of possible reconstructions using a generative neural network. The resulting ensemble is validated using techniques from numerical weather prediction and ocean modelling.
Simon Driscoll, Alberto Carrassi, Julien Brajard, Laurent Bertino, Einar Ólason, Marc Bocquet, and Amos Lawless
EGUsphere, https://doi.org/10.5194/egusphere-2024-2476, https://doi.org/10.5194/egusphere-2024-2476, 2024
Short summary
Short summary
The formation and evolution of sea ice melt ponds (ponds of melted water) are complex, insufficiently understood and represented in models with considerable uncertainty. These uncertain representations are not traditionally included in climate models potentially causing the known underestimation of sea ice loss in climate models. Our work creates the first observationally based machine learning model of melt ponds that is also a ready and viable candidate to be included in climate models.
Stéphane Doléac, Marina Lévy, Roy El Hourany, and Laurent Bopp
EGUsphere, https://doi.org/10.5194/egusphere-2024-1820, https://doi.org/10.5194/egusphere-2024-1820, 2024
Short summary
Short summary
Phytoplankton net primary production (NPP) is influenced by many processes, and their representation varies across Earth-system models. This leads to differing projections for NPP's future under climate change, especially in the North Atlantic. To address this, we identified and assessed the processes controlling NPP in each model. This assessment helped us select the most reliable models, significantly improving NPP projections in the region.
Léo Edel, Jiping Xie, Anton Korosov, Julien Brajard, and Laurent Bertino
EGUsphere, https://doi.org/10.5194/egusphere-2024-1896, https://doi.org/10.5194/egusphere-2024-1896, 2024
Short summary
Short summary
This study developed a new method to estimate Arctic sea ice thickness from 1992 to 2010 using a combination of machine learning and data assimilation. By training a machine learning model on data from 2011–2022, past errors in sea ice thickness can be corrected, leading to improved estimations. This approach provides insights into historical changes on sea ice thickness, showing a notable decline from 1992 to 2022, and offers a valuable resource for future studies.
Cyril Palerme, Thomas Lavergne, Jozef Rusin, Arne Melsom, Julien Brajard, Are Frode Kvanum, Atle Macdonald Sørensen, Laurent Bertino, and Malte Müller
The Cryosphere, 18, 2161–2176, https://doi.org/10.5194/tc-18-2161-2024, https://doi.org/10.5194/tc-18-2161-2024, 2024
Short summary
Short summary
Sea ice forecasts are operationally produced using physically based models, but these forecasts are often not accurate enough for maritime operations. In this study, we developed a statistical correction technique using machine learning in order to improve the skill of short-term (up to 10 d) sea ice concentration forecasts produced by the TOPAZ4 model. This technique allows for the reduction of errors from the TOPAZ4 sea ice concentration forecasts by 41 % on average.
Roy El Hourany, Juan Pierella Karlusich, Lucie Zinger, Hubert Loisel, Marina Levy, and Chris Bowler
Ocean Sci., 20, 217–239, https://doi.org/10.5194/os-20-217-2024, https://doi.org/10.5194/os-20-217-2024, 2024
Short summary
Short summary
Satellite observations offer valuable information on phytoplankton abundance and community structure. Here, we employ satellite observations to infer seven phytoplankton groups at a global scale based on a new molecular method from Tara Oceans. The link has been established using machine learning approaches. The output of this work provides excellent tools to collect essential biodiversity variables and a foundation to monitor the evolution of marine biodiversity.
Joelle Habib, Caroline Ulses, Claude Estournel, Milad Fakhri, Patrick Marsaleix, Mireille Pujo-Pay, Marine Fourrier, Laurent Coppola, Alexandre Mignot, Laurent Mortier, and Pascal Conan
Biogeosciences, 20, 3203–3228, https://doi.org/10.5194/bg-20-3203-2023, https://doi.org/10.5194/bg-20-3203-2023, 2023
Short summary
Short summary
The Rhodes Gyre, eastern Mediterranean Sea, is the main Levantine Intermediate Water formation site. In this study, we use a 3D physical–biogeochemical model to investigate the seasonal and interannual variability of organic carbon dynamics in the gyre. Our results show its autotrophic nature and its high interannual variability, with enhanced primary production, downward exports, and onward exports to the surrounding regions during years marked by intense heat losses and deep mixed layers.
Georges Baaklini, Roy El Hourany, Milad Fakhri, Julien Brajard, Leila Issa, Gina Fifani, and Laurent Mortier
Ocean Sci., 18, 1491–1505, https://doi.org/10.5194/os-18-1491-2022, https://doi.org/10.5194/os-18-1491-2022, 2022
Short summary
Short summary
We use machine learning to analyze the long-term variation of the surface currents in the Levantine Sea, located in the eastern Mediterranean Sea. We decompose the circulation into groups based on their physical characteristics and analyze their spatial and temporal variability. We show that most structures of the Levantine Sea are becoming more energetic over time, despite those of the western area remaining the most dominant due to their complex bathymetry and strong currents.
Katia Mallil, Pierre Testor, Anthony Bosse, Félix Margirier, Loic Houpert, Hervé Le Goff, Laurent Mortier, and Ferial Louanchi
Ocean Sci., 18, 937–952, https://doi.org/10.5194/os-18-937-2022, https://doi.org/10.5194/os-18-937-2022, 2022
Short summary
Short summary
Our study documents the circulation in the Algerian Basin of the western Mediterranean Sea using in situ data. It shows that the Algerian Gyres have an impact on the distribution at intermediate depth of Levantine Intermediate Water. They allow a westward transport from the south of Sardinia toward the interior of the Algerian Basin. Temperature and salinity trends of this water mass are also investigated, confirming a recent acceleration of the warming and salinification during the last decade.
Khalil Yala, N'Dèye Niang, Julien Brajard, Carlos Mejia, Mory Ouattara, Roy El Hourany, Michel Crépon, and Sylvie Thiria
Ocean Sci., 16, 513–533, https://doi.org/10.5194/os-16-513-2020, https://doi.org/10.5194/os-16-513-2020, 2020
Short summary
Short summary
The paper is a contribution to the study of phytoplankton pigment climatology from satellite ocean-color observations in the Senegalo–Mauritanian upwelling, which is a very productive region where in situ observations are lacking. We processed the satellite data with an efficient new neural network classifier. We were able to provide the climatological cycle of diatoms. This study may have an economic impact on fisheries thanks to better knowledge of phytoplankton dynamics.
Marc Bocquet, Julien Brajard, Alberto Carrassi, and Laurent Bertino
Nonlin. Processes Geophys., 26, 143–162, https://doi.org/10.5194/npg-26-143-2019, https://doi.org/10.5194/npg-26-143-2019, 2019
Short summary
Short summary
This paper describes an innovative way to use data assimilation to infer the dynamics of a physical system from its observation only. The method can operate with noisy and partial observation of the physical system. It acts as a deep learning technique specialised to dynamical models without the need for machine learning tools. The method is successfully tested on chaotic dynamical systems: the Lorenz-63, Lorenz-96, and Kuramoto–Sivashinski models and a two-scale Lorenz model.
Julien Brajard, Alberto Carrassi, Marc Bocquet, and Laurent Bertino
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2019-136, https://doi.org/10.5194/gmd-2019-136, 2019
Revised manuscript not accepted
Short summary
Short summary
We explore the possibility of combining data assimilation with machine learning. We introduce a new hybrid method for a two-fold scope: (i) emulating hidden, possibly chaotic, dynamics and (ii) predicting its future states. Numerical experiments have been carried out using the chaotic Lorenz 96 model, proving both the convergence of the hybrid method and its statistical skills including short-term forecasting and emulation of the long-term dynamics.
Hector Simon Benavides Pinjosovsky, Sylvie Thiria, Catherine Ottlé, Julien Brajard, Fouad Badran, and Pascal Maugis
Geosci. Model Dev., 10, 85–104, https://doi.org/10.5194/gmd-10-85-2017, https://doi.org/10.5194/gmd-10-85-2017, 2017
Short summary
Short summary
The objective of this work is to deliver the adjoint model of SECHIBA obtained with software called YAO, in order to perform 4D-VAR data assimilation. The SECHIBA module of the ORCHIDEE land surface model describes the exchanges of water and energy between the surface and the atmosphere. A distributed version is available when only the land surface temperature is used as an observation, with two examples and documentation.
Related subject area
Approach: Remote Sensing | Properties and processes: Mesoscale to submesoscale dynamics
Multiple timescale variations in fronts in the Seto Inland Sea, Japan
MAESSTRO: Masked Autoencoders for Sea Surface Temperature Reconstruction under Occlusion
Integrating wide swath altimetry data into Level-4 multi-mission maps
Deep learning for the super resolution of Mediterranean sea surface temperature fields
Blending 2D topography images from SWOT into the altimeter constellation with the Level-3 multi-mission DUACS system
Estimating ocean currents from the joint reconstruction of absolute dynamic topography and sea surface temperature through deep learning algorithms
Impact of surface and subsurface-intensified eddies on sea surface temperature and chlorophyll a in the northern Indian Ocean utilizing deep learning
Regional mapping of energetic short mesoscale ocean dynamics from altimetry: performances from real observations
Ocean 2D eddy energy fluxes from small mesoscale processes with SWOT
Menghong Dong and Xinyu Guo
Ocean Sci., 20, 1527–1546, https://doi.org/10.5194/os-20-1527-2024, https://doi.org/10.5194/os-20-1527-2024, 2024
Short summary
Short summary
We employed a gradient-based algorithm to identify the position and intensity of the fronts in a coastal sea using sea surface temperature data, thereby quantifying their variations. Our study provides a comprehensive analysis of these fronts, elucidating their seasonal variability, intra-tidal dynamics, and the influence of winds on the fronts. By capturing the temporal and spatial dynamics of these fronts, our understanding of the complex oceanographic processes within this region is enhanced.
Edwin Goh, Alice Yepremyan, Jinbo Wang, and Brian Wilson
Ocean Sci., 20, 1309–1323, https://doi.org/10.5194/os-20-1309-2024, https://doi.org/10.5194/os-20-1309-2024, 2024
Short summary
Short summary
An AI model was used to fill in missing parts of sea temperature (SST) maps caused by cloud cover. We found masked autoencoders can recreate missing SSTs with less than 0.2 °C error, even when 80 % are missing. This is 5000 times faster than conventional methods tested on a single central processing unit. This can enhance our ability in monitoring global small-scale ocean fronts that affect heat, carbon, and nutrient exchange in the ocean. The method is promising for future research.
Maxime Ballarotta, Clément Ubelmann, Valentin Bellemin-Laponnaz, Florian Le Guillou, Guillaume Meda, Cécile Anadon, Alice Laloue, Antoine Delepoulle, Yannice Faugère, Marie-Isabelle Pujol, Ronan Fablet, and Gérald Dibarboure
EGUsphere, https://doi.org/10.5194/egusphere-2024-2345, https://doi.org/10.5194/egusphere-2024-2345, 2024
Short summary
Short summary
The Surface Water and Ocean Topography (SWOT) mission provides unprecedented swath altimetry data. This study examines SWOT's impact on mapping systems, showing a moderate effect with the current nadir altimetry constellation and a stronger impact with a reduced one. Integrating SWOT with dynamic mapping techniques improves the resolution of satellite-derived products, offering promising solutions for studying and monitoring sea-level variability at finer scales.
Claudia Fanelli, Daniele Ciani, Andrea Pisano, and Bruno Buongiorno Nardelli
Ocean Sci., 20, 1035–1050, https://doi.org/10.5194/os-20-1035-2024, https://doi.org/10.5194/os-20-1035-2024, 2024
Short summary
Short summary
Sea surface temperature (SST) is an essential variable to understanding the Earth's climate system, and its accurate monitoring from space is essential. Since satellite measurements are hindered by cloudy/rainy conditions, data gaps are present even in merged multi-sensor products. Since optimal interpolation techniques tend to smooth out small-scale features, we developed a deep learning model to enhance the effective resolution of gap-free SST images over the Mediterranean Sea to address this.
Gerald Dibarboure, Cécile Anadon, Frédéric Briol, Emeline Cadier, Robin Chevrier, Antoine Delepoulle, Yannice Faugère, Alice Laloue, Rosemary Morrow, Nicolas Picot, Pierre Prandi, Marie-Isabelle Pujol, Matthias Raynal, Anaelle Treboutte, and Clément Ubelmann
EGUsphere, https://doi.org/10.5194/egusphere-2024-1501, https://doi.org/10.5194/egusphere-2024-1501, 2024
Short summary
Short summary
The Surface Water and Ocean Topography (SWOT) mission delivers unprecedented swath altimetry products. In this paper, we describe how we extended the Level-3 algorithms to handle SWOT’s unique swath-altimeter data. We also illustrate and discuss the benefits, relevance, and limitations of Level-3 swath-altimeter products for various research domains.
Daniele Ciani, Claudia Fanelli, and Bruno Buongiorno Nardelli
EGUsphere, https://doi.org/10.5194/egusphere-2024-1164, https://doi.org/10.5194/egusphere-2024-1164, 2024
Short summary
Short summary
Ocean surface currents are routinely derived from satellite observations of the sea level, allowing a regional to global scale synoptic monitoring. In order to overcome the theoretical and instrumental limits of this methodology, we exploit the synergy of multisensor satellite observations. We rely on deep learning, physics informed algorithms to predict ocean currents from sea surface height and sea surface temperature observations. Results are validated by means of in-situ measurements
Yingjie Liu and Xiaofeng Li
Ocean Sci., 19, 1579–1593, https://doi.org/10.5194/os-19-1579-2023, https://doi.org/10.5194/os-19-1579-2023, 2023
Short summary
Short summary
The study developed a deep learning model that effectively distinguishes between surface- and subsurface-intensified eddies in the northern Indian Ocean by integrating sea surface height and temperature data. The accurate distinction between these types of eddies provides valuable insights into their dynamics and their impact on marine ecosystems in the northern Indian Ocean and contributes to understanding the complex interactions between eddy dynamics and biogeochemical processes in the ocean.
Florian Le Guillou, Lucile Gaultier, Maxime Ballarotta, Sammy Metref, Clément Ubelmann, Emmanuel Cosme, and Marie-Helène Rio
Ocean Sci., 19, 1517–1527, https://doi.org/10.5194/os-19-1517-2023, https://doi.org/10.5194/os-19-1517-2023, 2023
Short summary
Short summary
Altimetry provides sea surface height (SSH) data along one-dimensional tracks. For many applications, the tracks are interpolated in space and time to provide gridded SSH maps. The operational SSH gridded products filter out the small-scale signals measured on the tracks. This paper evaluates the performances of a recently implemented dynamical method to retrieve the small-scale signals from real SSH data. We show a net improvement in the quality of SSH maps when compared to independent data.
Elisa Carli, Rosemary Morrow, Oscar Vergara, Robin Chevrier, and Lionel Renault
Ocean Sci., 19, 1413–1435, https://doi.org/10.5194/os-19-1413-2023, https://doi.org/10.5194/os-19-1413-2023, 2023
Short summary
Short summary
Oceanic eddies are the structures carrying most of the energy in our oceans. They are key to climate regulation and nutrient transport. We prepare for the Surface Water and Ocean Topography mission, studying eddy dynamics in the region south of Africa, where the Indian and Atlantic oceans meet, using models and simulated satellite data. SWOT will provide insights into the structures smaller than what is currently observable, which appear to greatly contribute to eddy kinetic energy and strain.
Cited articles
Alaguarda, D., Brajard, J., Coulibaly, G., Canesi, M., Douville, E., Le Cornec, F., Lelabousse, C., and Tribollet, A.: 54 years of microboring community history explored by machine learning in a massive coral from Mayotte (Indian Ocean), Front. Mar. Sci., 9, 899398, https://doi.org/10.3389/fmars.2022.899398, 2022. a
Amitai, Y., Lehahn, Y., Lazar, A., and Heifetz, E.: Surface circulation of the eastern Mediterranean Levantine basin: Insights from analyzing 14 years of satellite altimetry data, J. Geophys. Res.-Oceans, 115, C10058, https://doi.org/10.1029/2010JC006147, 2010. a
Atkinson, L. P., Brink, K. H., Davis, R. E., Jones, B. H., Paluszkiewicz, T., and Stuart, D. W.: Mesoscale hydrographic variability in the vicinity of Points Conception and Arguello during April–May 1983: the OPUS 1983 experiment, J. Geophys. Res.-Oceans, 91, 12899–12918, 1986. a
Baaklini, G.: Characterization of the Eastern Mediterranean surface dynamics: Insights from drifter assimilation and machine learning techniques, PhD thesis, Sorbonne Université, https://theses.hal.science/tel-03828273 (last access: 23 April 2024), 2022. a
Baaklini, G., El Hourany, R., Fakhri, M., Brajard, J., Issa, L., Fifani, G., and Mortier, L.: Surface circulation properties in the eastern Mediterranean emphasized using machine learning methods, Ocean Sci., 18, 1491–1505, https://doi.org/10.5194/os-18-1491-2022, 2022. a, b
Barale, V., Jaquet, J.-M., and Ndiaye, M.: Algal blooming patterns and anomalies in the Mediterranean Sea as derived from the SeaWiFS data set (1998–2003), Remote Sens. Environ., 112, 3300–3313, https://doi.org/10.1016/j.rse.2007.10.014, 2008. a
Botha, E. J., Anstee, J. M., Sagar, S., Lehmann, E., and Medeiros, T. A.: Classification of Australian waterbodies across a wide range of optical water types, Remote Sens., 12, 3018–3041, https://doi.org/10.3390/rs12183018, 2020. a
Brenner, S.: High-resolution nested model simulations of the climatological circulation in the southeastern Mediterranean Sea, Ann. Geophys., 21, 267–280, https://doi.org/10.5194/angeo-21-267-2003, 2003. a
Cannizzaro, J. P. and Carder, K. L.: Estimating chlorophyll a concentrations from remote-sensing reflectance in optically shallow waters, Remote Sens. Environ., 101, 13–24, https://doi.org/10.1016/j.rse.2005.12.002, 2006. a
Cipollini, P., Benveniste, J., Bouffard, J., Emery, W., Gommenginger, C., Griffin, D., Høyer, J., Madsen, K., Mercier, F., Miller, L., et al.: The role of altimetry in coastal observing systems, Proceedings of OceanObs, 9, 181–191, https://doi.org/10.5270/OceanObs09.cwp.16, 2010. a
Dong, C., Xu, G., Han, G., Bethel, B. J., Xie, W., and Zhou, S.: Recent developments in artificial intelligence in oceanography, Ocean-Land-Atmosphere Research, 2022 9870950, https://doi.org/10.34133/2022/9870950, 2022. a
Escudier, R., Mourre, B., Juza, M., and Tintoré, J.: Subsurface circulation and mesoscale variability in the Algerian subbasin from altimeter-derived eddy trajectories: ALGERIAN EDDIES PROPAGATION, J. Geophys. Res.-Oceans, 121, 6310–6322, https://doi.org/10.1002/2016JC011760, 2016. a
Fifani, G., Baudena, A., Fakhri, M., Baaklini, G., Faugère, Y., Morrow, R., Mortier, L., and d'Ovidio, F.: Drifting Speed of Lagrangian Fronts and Oil Spill Dispersal at the Ocean Surface, Remote Sens., 13, 4499, https://doi.org/10.3390/rs13224499, 2021. a
GEBCO: GEBCO 2020 Grid, version 2020.0, https://www.gebco.net (last access: 11 July 2024), 2020. a
Han, J. and Moraga, C.: The influence of the sigmoid function parameters on the speed of backpropagation learning, in: International workshop on artificial neural networks, 195–201, Springer, https://link.springer.com/content/pdf/10.1007/3-540-59497-3_175.pdf (last access: 11 July 2024), 1995. a
Jackson, T., Sathyendranath, S., and Mélin, F.: An improved optical classification scheme for the Ocean Colour Essential Climate Variable and its applications, Remote Sens. Environ., 203, 152–161, https://doi.org/10.1016/j.rse.2017.03.036, 2017. a
Kingma, D. P. and Ba, J.: Adam: A method for stochastic optimization, arXiv [preprint], https://doi.org/10.48550/arXiv.1412.6980, 22 December 2014. a
Levy, M. and Martin, A. P.: The influence of mesoscale and submesoscale heterogeneity on ocean biogeochemical reactions: INFLUENCE OF HETEROGENEITY, Global Biogeochem. Cy., 27, 1139–1150, https://doi.org/10.1002/2012GB004518, 2013. a
Lguensat, R., Sun, M., Fablet, R., Tandeo, P., Mason, E., and Chen, G.: EddyNet: A deep neural network for pixel-wise classification of oceanic eddies, in: IGARSS 2018-2018 IEEE International Geoscience and Remote Sensing Symposium, Valencia, 22–27 July 2018, 1764–1767, https://doi.org/10.1109/IGARSS.2018.8518411, 2018. a
Lillibridge III, J., Hitchcock, G., Rossby, T., Lessard, E., Mork, M., and Golmen, L.: Entrainment and mixing of shelf/slope waters in the near-surface Gulf Stream, J. Geophys. Res.-Oceans, 95, 13065–13087, https://doi.org/10.1029/JC095iC08p13065, 1990. a
Martin Traykovski, L. V. and Sosik, H. M.: Feature-based classification of optical water types in the Northwest Atlantic based on satellite ocean color data, J. Geophys. Res.-Oceans, 108, 3150–3167, https://doi.org/10.1029/2001JC001172, 2003. a
Mélin, F. and Vantrepotte, V.: How optically diverse is the coastal ocean?, Remote Sens. Environ., 160, 235–251, https://doi.org/10.1016/j.rse.2015.01.023, 2015. a
Menna, M., Poulain, P.-M., Zodiatis, G., and Gertman, I.: On the surface circulation of the Levantine sub-basin derived from Lagrangian drifters and satellite altimetry data, Deep-Sea Res. Pt. I, 65, 46–58, https://doi.org/10.1016/j.dsr.2012.02.008, 2012. a, b
Menna, M., Gerin, R., Bussani, A., and Poulain, P.-M.: Satellite-tracked surface drifting buoy (drifter) observations of currents and sea surface temperature in the Mediterranean Sea (1986–2016), nodc.ogs.it [data set], https://doi.org/10.6092/7A8499BC-C5EE-472C-B8B5-03523D1E73E9, 2018. a
Mkhinini, N., Coimbra, A. L. S., Stegner, A., Arsouze, T., Taupier-Letage, I., and Béranger, K.: Long-lived mesoscale eddies in the eastern Mediterranean Sea: Analysis of 20 years of AVISO geostrophic velocities, J. Geophys. Res.-Oceans, 119, 8603–8626, https://doi.org/10.1002/2014JC010176, 2014. a
Moore, T. S., Campbell, J. W., and Dowell, M. D.: A class-based approach to characterizing and mapping the uncertainty of the MODIS ocean chlorophyll product, Remote Sens. Environ., 113, 2424–2430, https://doi.org/10.1016/j.rse.2009.07.016, 2009. a
Moschos, E., Kugusheva, A., Coste, P., and Stegner, A.: Computer Vision for Ocean Eddy Detection in Infrared Imagery, in: Proceedings of the IEEE/CVF Winter Conference on Applications of Computer Vision, Hawaii, 3–7 January 2023, 6395–6404, https://doi.org/10.1109/WACV56688.2023.00633, 2023. a, b
NASA Goddard Space Flight Center, Ocean Ecology Laboratory, Ocean Biology Processing Group: Moderate-resolution Imaging Spectroradiometer (MODIS) Aqua Chlorophyll Data, 2018 Reprocessing, oceancolor.gsfc.nasa.gov [data set], https://doi.org/10.5067/AQUA/MODIS/L3B/CHL/2018, 2024. a
Ou, H. W.: Flow near a continental boundary driven by an oceanic jet, J. Phys. Oceanogr., 24, 966–978, https://doi.org/10.1175/1520-0485(1994)024<0966:FNACBD>2.0.CO;2, 1994. a
Pujol, M.-I. and Larnicol, G.: Mediterranean sea eddy kinetic energy variability from 11 years of altimetric data, J. Mar. Syst., 58, 121–142, https://doi.org/10.1016/j.jmarsys.2005.07.005, 2005. a
Ronneberger, O., Fischer, P., and Brox, T.: U-net: Convolutional networks for biomedical image segmentation, in: Medical Image Computing and Computer-Assisted Intervention–MICCAI 2015: 18th International Conference, Munich, Germany, 5–9 October 2015, Proceedings, Part III 18, 234–241, arXiv [preprint], https://doi.org/10.48550/arXiv.1505.04597, 18 May 2015. a, b
Rosentraub, Z. and Brenner, S.: Circulation over the southeastern continental shelf and slope of the Mediterranean Sea: Direct current measurements, winds, and numerical model simulations, J. Geophys. Res.-Oceans, 112, C11001, https://doi.org/10.1029/2006JC003775, 2007. a
Sarangi, R.: Observation of Oceanic Eddy in the Northeastern Arabian Sea Using Multisensor Remote Sensing Data, Int. J. Oceanogr., 531982, https://doi.org/10.1155/2012/531982, 2012. a
Shaban, M., Salim, R., Abu Khalifeh, H., Khelifi, A., Shalaby, A., El-Mashad, S., Mahmoud, A., Ghazal, M., and El-Baz, A.: A deep-learning framework for the detection of oil spills from SAR data, Sensors, 21, 2351, https://doi.org/10.3390/s21072351, 2021. a
Sonnewald, M., Lguensat, R., Jones, D. C., Dueben, P. D., Brajard, J., and Balaji, V.: Bridging observations, theory and numerical simulation of the ocean using machine learning, Environ. Res. Lett., 16, 073008, https://doi.org/10.1088/1748-9326/ac0eb0, 2021. a
Spyrakos, E., Vilas, L. G., Palenzuela, J. M. T., and Barton, E. D.: Remote sensing chlorophyll a of optically complex waters (rias Baixas, NW Spain): Application of a regionally specific chlorophyll a algorithm for MERIS full resolution data during an upwelling cycle, Remote Sens. Environ., 115, 2471–2485, https://doi.org/10.1016/j.rse.2011.05.008, 2011. a
SSALTO/DUACS: Processed by SSALTO/DUACS and Distributed by AVISO+, https://www.aviso.altimetry.fr (last access: 11 July 2024), 2022. a
Stern, M. E. and Whitehead, J.: Separation of a boundary jet in a rotating fluid, J. Fluid Mech., 217, 41–69, https://doi.org/10.1017/S0022112090000623, 1990. a
Sun, N., Zhou, Z., Li, Q., and Zhou, X.: Spatiotemporal Prediction of Monthly Sea Subsurface Temperature Fields Using a 3D U-Net-Based Model, Remote Sens., 14, 4890, https://doi.org/10.3390/rs14194890, 2022. a
Sutyrin, G., Stegner, A., Taupier-Letage, I., and Teinturier, S.: Amplification of a surface-intensified eddy drift along a steep shelf in the Eastern Mediterranean Sea, J. Phys. Oceanogr., 39, 1729–1741, https://doi.org/10.1175/2009JPO4106.1, 2009. a
Taupier-Letage, I., Puillat, I., Raimbault, P., and Millot, C.: Biological response to mesoscale eddies in the Algerian Basin, J. Geophys. Res., 108, 3245–3267, https://doi.org/10.1029/1999JC000117, 2003. a
Wei, J., Wang, M., Mikelsons, K., Jiang, L., Kratzer, S., Lee, Z., Moore, T., Sosik, H. M., and Van der Zande, D.: Global satellite water classification data products over oceanic, coastal, and inland waters, Remote Sens. Environ., 282, 113233, https://doi.org/10.1016/j.rse.2022.113233, 2022. a
Zhang, X., Zhao, N., and Han, Z.: A Modified U-Net Model for Predicting the Sea Surface Salinity over the Western Pacific Ocean, Remote Sens., 15, 1684, https://doi.org/10.3390/rs15061684, 2023. a
Short summary
Understanding the flow of the Levantine Sea surface current is not straightforward. We propose a study based on learning techniques to follow interactions between water near the shore and further out at sea. Our results show changes in the coastal currents past 33.8° E, with frequent instances of water breaking away along the Lebanese coast. These events happen quickly and sometimes lead to long-lasting eddies. This study underscores the need for direct observations to improve our knowledge.
Understanding the flow of the Levantine Sea surface current is not straightforward. We propose a...