Arthur Capet

ORCID: 0000-0002-5939-3836
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About
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Research Areas
  • Marine and environmental studies
  • Aquatic and Environmental Studies
  • Oceanographic and Atmospheric Processes
  • Marine and coastal ecosystems
  • Food Industry and Aquatic Biology
  • Methane Hydrates and Related Phenomena
  • Climate variability and models
  • Marine Biology and Ecology Research
  • Geological Studies and Exploration
  • Coastal and Marine Management
  • Marine and fisheries research
  • Geological formations and processes
  • Atmospheric and Environmental Gas Dynamics
  • Geology and Paleoclimatology Research
  • Isotope Analysis in Ecology
  • Ocean Waves and Remote Sensing
  • Meteorological Phenomena and Simulations
  • Ocean Acidification Effects and Responses
  • Geochemistry and Geologic Mapping
  • Peatlands and Wetlands Ecology
  • Global Energy and Sustainability Research
  • Tropical and Extratropical Cyclones Research
  • Aeolian processes and effects
  • Pigment Synthesis and Properties
  • Coastal wetland ecosystem dynamics

Université Libre de Bruxelles
2024-2025

Institute of Natural Sciences
2023-2024

Institut polytechnique de Grenoble
2023-2024

Institut des Géosciences de l'Environnement
2022-2024

Institut de Recherche pour le Développement
2023-2024

Centre National de la Recherche Scientifique
2023-2024

Université Grenoble Alpes
2022-2024

University of Liège
2014-2023

Emerald Coast Science Center
2018-2020

Aquatic Systems (United States)
2006-2020

Karina von Schuckmann Pierre‐Yves Le Traon Neville Smith Ananda Pascual Pierre Brasseur and 95 more Katja Fennel Samy Djavidnia Signe Aaboe Enrique Álvarez Fanjul Emmanuelle Autret Lars Axell Roland Aznar Mario Benincasa A. Bentamy Fredrik Boberg Romain Bourdallé-Badie Bruno Buongiorno Nardelli Vittorio Brando Clément Bricaud Lars‐Anders Breivik Robert J. W. Brewin Arthur Capet Adrien Ceschin Stefania Angela Ciliberti Gianpiero Cossarini Marta de Alfonso Ananda Pascual Jos de Kloe Julie Deshayes Charles Desportes Marie Drévillon Yann Drillet Riccardo Droghei Clotilde Dubois Owen Embury Hélène Etienne Claudia Fratianni Jesús García‐Lafuente Marcos García Sotillo Gilles Garric Florent Gasparin Riccardo Gerin Simon Good Jérôme Gourrion Marilaure Grégoire Eric Greiner S. Guinehut Elodie Gutknecht Fabrice Hernández Olga Hernandez Jacob L. Høyer Laura Jackson Simon Jandt Simon A. Josey Melanie Juzà John Kennedy Zoi Kokkini Γεράσιμος Κορρές Mariliis Kõuts Priidik Lagemaa Thomas Lavergne Bernard Le Cann Jean‐François Legeais B. Lemieux-Dudon Bruno Levier Vidar S. Lien Ilja Maljutenko Fernando Manzano Marta Marcos Veselka Marinova Simona Masina Elena Mauri Michael Mayer Angelique Melet Frédéric Mélin Benoît Meyssignac Maeva Monier Malte Müller Sandrine Mulet Cristina Naranjo Giulio Notarstefano Aurélien Paulmier Begoña Pérez Gómez Irene Pérez Gonzalez Elisaveta Peneva Coralie Perruche K. Andrew Peterson Nadia Pinardi Andrea Pisano Silvia Pardo Pierre-Marie Poulain Roshin P. Raj Urmas Raudsepp Michaelis Ravdas Rebecca Reid Marie‐Hélène Rio Stefano Salon Annette Samuelsen Michela Sammartino Simone Sammartino

Introduction — s1 Chapter 1: Essential Variables s4  1.1 Ocean temperature and salinity  Sandrine Mulet, Bruno Buongiorno Nardelli, Simon Good, Andrea Pisano, Eric Greiner, Maeva Monier, Emmanuel...

10.1080/1755876x.2018.1489208 article EN Journal of Operational Oceanography 2018-08-24
Karina von Schuckmann Pierre-Yves Le Traon Neville Smith Ananda Pascual Samuel Djavidnia and 95 more Jean‐Pierre Gattuso Marilaure Grégoire Signe Aaboe Victor Alari Brittany Alexander Andrés Alonso-Martirena Ali Aydoğdu Joel Azzopardi Marco Bajo Francesco Barbariol Mirna Batistić Arno Behrens Sana Ben Ismail Alvise Benetazzo Isabella Bitetto Mireno Borghini Laura Bray Arthur Capet Roberto Carlucci Sourav Chatterjee Jacopo Chiggiato Stefania Angela Ciliberti Giulia Cipriano Emanuela Clementi Paul Cochrane Gianpiero Cossarini Lorenzo D’Andrea Silvio Davison Emily Down Aldo Drago Jean‐Noël Druon Georg H. Engelhard Iván Federico Rade Garić Adam Gauci Riccardo Gerin Gerhard Geyer Rianne Giesen Simon Good Richard Graham Marilaure Grégoire Eric Greiner K. Gundersen Pierre Hélaouët Stefan Hendricks Johanna J. Heymans Jason T. Holt Marijana Hure Mélanie Juza Dimitris Kassis Paula Kellett Maaike Knol Panagiotis Kountouris Marilii Kõuts Priidik Lagemaa Thomas Lavergne Jean‐François Legeais Pierre-Yves Le Traon Simone Libralato Vidar S. Lien Leonardo Lima Sigrid Lind Ye Liu Diego Macías Ilja Maljutenko Antoine Mangin Aarne Männik Veselka Marinova Riccardo Martellucci Francesco Masnadi Elena Mauri Michael Mayer Milena Menna Catherine Meulders Jane S. Møgster Maeva Monier Kjell Arne Mork Malte Müller Jan Even Øie Nilsen Giulio Notarstefano José L. Oviedo Cyril Palerme Andreas Palialexis Diego Panzeri Silvia Pardo Elisaveta Peneva Paolo Pezzutto Annunziata Pirro Trevor Platt Pierre-Marie Poulain Laura Prieto Stefano Querin Lasse Rabenstein Roshin P. Raj Urmas Raudsepp

Chapter 1: CMEMS OSR5     1 1.1 IntroductionKarina von Schuckmann and Pierre-Yves Le Traon     1 1.2 Knowledge data for international Ocean governancePaula Kellett, Brittany E. Alexander Jo...

10.1080/1755876x.2021.1946240 article EN cc-by-nc-nd Journal of Operational Oceanography 2021-08-20

The challenges associated with meso- and submesoscale variability (between 1-100 km) require high-resolution observations integrated approaches. Here we describe a major oceanographic experiment designed to capture the intense but transient vertical motions mesoscale features in an area characterized by strong fronts. Finescale processes were studied eastern Alboran Sea (Western Mediterranean) about 400 km east of Strait Gibraltar, relatively sparsely sampled area. In-situ systems...

10.3389/fmars.2017.00039 article EN cc-by Frontiers in Marine Science 2017-02-21

Abstract Oceanic fronts are dynamically active regions of the global ocean that support upwelling and downwelling with significant implications for phytoplankton production export. However (on time scales inertial scale), vertical velocity is 10 3 –10 4 times weaker than horizontal difficult to observe directly. Using intensive field observations in conjunction a process study model, we examine motion its effect on fluxes at multiple spatial an oligotrophic region Western Mediterranean Sea....

10.1029/2019jc015034 article EN Journal of Geophysical Research Oceans 2019-07-23

Abstract. We show that from 1955 to 2015, the inventory of oxygen in Black Sea has decreased by 44 % and basin-averaged penetration depth 140 m 90 which is shallowest annual value recorded during period. The oxygenated surface layer separates world's largest reservoir toxic hydrogen sulfide atmosphere. threat chemocline excursion events led hot debates past decades arguing on vertical stability oxic/suboxic interface. In 1970s 1980s, when faced severe eutrophication, enhanced respiration...

10.5194/bg-13-1287-2016 article EN cc-by Biogeosciences 2016-03-01

Abstract. The Black Sea northwestern shelf (NWS) is a shallow eutrophic area in which the seasonal stratification of water column isolates bottom waters from atmosphere. This prevents ventilation counterbalancing large consumption oxygen due to respiration and sediments, sets stage for development hypoxia. A three-dimensional (3-D) coupled physical–biogeochemical model used investigate dynamics hypoxia NWS, first at then interannual scales (1981–2009), differentiate its driving factors...

10.5194/bg-10-3943-2013 article EN cc-by Biogeosciences 2013-06-18

To protect marine ecosystems threatened by climate change and anthropic stressors, it is essential to operationally monitor ocean health indicators. These are metrics synthetizing multiple processes relevant the users of operational services. Here we assess if selected indicators simulated models can be controlled (here meaning constrained effectively) biogeochemical observations, using a newly proposed methodological framework. The method consists in firstly screening sensitivities with...

10.5194/egusphere-egu25-11637 preprint EN 2025-03-14

The Land-Ocean Aquatic Continuum (LOAC) plays a pivotal role in the transfer and transformation of carbon nutrients from terrestrial systems to coastal waters, critically influencing eutrophication resulting excessive nitrogen (N) phosphorus (P) loads rivers compared Silica (Si). Indeed, both agricultural practices on land biogeochemical processes near streams as well within estuaries control eventual export into sea. To address complex interplay that govern these transfers, an integrated...

10.5194/egusphere-egu25-13368 preprint EN 2025-03-15

Estuarine environments are complex dynamic systems and cornerstone components of the  Land-Ocean Aquatic Continuum (LOAC). As such, they play a crucial role in global biogeochemical cycles, acting both as conduits processors carbon nutrients between the terrestrial oceanic realms Earth system. Despite this significance, considerable uncertainties remain associated with quantification fluxes within through estuarine systems. In particular, interplay Organic Carbon (OC) degradation...

10.5194/egusphere-egu25-20395 preprint EN 2025-03-15

Marine gels are organic polymers spanning from dissolved Exopolymeric Substances (EPS; nm to µm) Transparent Exopolymer Particles (TEP; µm mm), playing a key role in marine ecosystems by enhancing flocculation between and mineral particles. This process significantly affects the size distribution, density, vertical transport of Suspended Particulate Matter (SPM) as well carbon cycle ocean. In turbid coastal environments, TEP produced phytoplankton determines seasonality SPM...

10.5194/egusphere-egu25-19291 preprint EN 2025-03-15

Marine renewable energies are part of the current energy transition strategy in Europe. Offshore wind farms (OWFs) North Sea currently supply around 25.8 GW power and aimed to reach at least 117 by 2030. Yet, on its own, remains partially unreliable for a consistent generation. photovoltaic (PV) installations increasingly considered suitable technology complement intermittent OWF.  In Sea, installation offshore photovoltaics within OWFs offers two significant advantages: (1) space...

10.5194/egusphere-egu25-16328 preprint EN 2025-03-15

Abstract We investigate the extent to which recently upgraded version of Ssalto/Duacs sea level anomaly product affects description mesoscale activity in Eastern Boundary Upwelling Systems (EBUS). Drifter observations confirm that new data set released by Archiving, Validation and Interpretation Satellite Oceanographic (AVISO) April 2014 (DT14) offers an enhanced for four EBUS. DT14 returns significantly higher eddy kinetic energy levels (+80%) within a 300 km coastal band, where structures...

10.1002/2014gl061770 article EN Geophysical Research Letters 2014-10-20

Offshore wind farms (OWFs) are an important source of renewable energy accounting for 2.3% the European Union's electricity demand. Yet their impact on environment needs to be assessed. Here, we couple a hydrodynamic (including tides and waves) sediment transport model with description organic carbon mineral particle dynamics in water column sediments. The is applied Belgian Coastal Zone (BCZ) where OWFs currently occupy 7% its surface area which estimated double next 5 years. represented...

10.3389/fmars.2021.631799 article EN cc-by Frontiers in Marine Science 2021-06-02

An overview of the current European capacity in terms operational modelling marine and coastal systems is presented. This compiled from a survey conducted 2018-2019 among members EuroGOOS its related network Regional Operational Oceanographic Systems, addressing purposes, context technical specificities systems. Contributions to were received 38 organizations around Europe, which represent 84 model simulating mostly hydrodynamics, biogeochemistry sea waves. The analysis contributions...

10.3389/fmars.2020.00129 article EN cc-by Frontiers in Marine Science 2020-03-03

Offshore windfarms (OWFs) offer part of the solution for energy transition which is urgently needed to mitigate effects climate change. Marine life has rapidly exploited new habitat offered by windfarm structures, resulting in increased opportunities filter- and suspension feeding organisms. In this study, we investigated organic matter (OM) deposition form fecal pellets expelled filtering epifauna OWFs, on mineralization processes sediment. OM fluxes produced a 3D hydrodynamic model...

10.3389/fmars.2021.632243 article EN cc-by Frontiers in Marine Science 2021-06-17

Abstract. The deep chlorophyll maximum (DCM) is a well-known feature of the global ocean. However, its description and study formation are challenge, especially in peculiar environment that Black Sea. retrieval (chl a) from fluorescence (Fluo) profiles recorded by Biogeochemical Argo (BGC-Argo) floats not trivial Sea, due to very high content coloured dissolved organic matter (CDOM) which contributes signal produces an apparent increase chl concentration with depth. Here, we revised Fluo...

10.5194/bg-18-755-2021 article EN cc-by Biogeosciences 2021-02-01

In this paper, satellite products developed during the Earth Observation for Science and Innovation in Black Sea (EO4SIBS) ESA project are presented. Ocean colour, sea level anomaly surface salinity datasets produced last decade validated with regional in-situ observations. New data processing is tested to appropriately tackle Sea’s particular configuration geophysical characteristics. For altimetry, full rate (20Hz) altimeter measurements from Cryosat-2 Sentinel-3A processed deliver a 5Hz...

10.3389/fmars.2022.998970 article EN cc-by Frontiers in Marine Science 2023-01-26

Abstract. Predicting the ocean state in support of human activities, environmental monitoring and policymaking across different regions worldwide is fundamental require numerical strategies that have to address their physical peculiarities. The Authors provide an outlook on status operational forecasting systems 8 key world ocean: West Pacific Marginal Seas South East Asia, Indian Ocean, African Seas, Mediterranean Black Sea, North-East Atlantic, Central America North Arctic. Starting from...

10.5194/sp-2024-26 preprint EN cc-by 2024-10-29

The Black Sea Monitoring and Forecasting Center (BS-MFC) is the European reference service for provision of ocean analyses, forecasts, reanalyses in basin. It part Copernicus Marine Environment Service (CMEMS) ensures a high level efficiency terms operations, science, technology predictions monitoring physical biogeochemical processes Sea. operational BS-MFC framework based on state-of-the-art numerical models hydrodynamics, biogeochemistry, waves; analysis, forecast, reanalysis are provided...

10.3390/jmse9101146 article EN cc-by Journal of Marine Science and Engineering 2021-10-18
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