Littérature scientifique sur le sujet « Underwater Vision Profiler 6 (UVP6) »
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Articles de revues sur le sujet "Underwater Vision Profiler 6 (UVP6)"
Kiko, Rainer, Marc Picheral, David Antoine, Marcel Babin, Léo Berline, Tristan Biard, Emmanuel Boss et al. « A global marine particle size distribution dataset obtained with the Underwater Vision Profiler 5 ». Earth System Science Data 14, no 9 (22 septembre 2022) : 4315–37. http://dx.doi.org/10.5194/essd-14-4315-2022.
Texte intégralPicheral, Marc, Camille Catalano, Denis Brousseau, Hervé Claustre, Laurent Coppola, Edouard Leymarie, Jérôme Coindat et al. « The Underwater Vision Profiler 6 : an imaging sensor of particle size spectra and plankton, for autonomous and cabled platforms ». Limnology and Oceanography : Methods 20, no 2 (23 décembre 2021) : 115–29. http://dx.doi.org/10.1002/lom3.10475.
Texte intégralPanaïotis, Thelma, Antoine Poteau, Émilie Diamond Riquier, Camille Catalano, Lucas Courchet, Solène Motreuil, Laurent Coppola, Marc Picheral et Jean‐Olivier Irisson. « Temporal evolution of plankton and particles distribution across a mesoscale front during the spring bloom ». Limnology and Oceanography, 22 avril 2024. http://dx.doi.org/10.1002/lno.12566.
Texte intégralLlopis Monferrer, Natalia, Tristan Biard, Miguel M. Sandin, Fabien Lombard, Marc Picheral, Amanda Elineau, Lionel Guidi, Aude Leynaert, Paul J. Tréguer et Fabrice Not. « Siliceous Rhizaria abundances and diversity in the Mediterranean Sea assessed by combined imaging and metabarcoding approaches ». Frontiers in Marine Science 9 (10 octobre 2022). http://dx.doi.org/10.3389/fmars.2022.895995.
Texte intégralThèses sur le sujet "Underwater Vision Profiler 6 (UVP6)"
Ricour, Florian. « Towards a new insight of the carbon transport in the global ocean ». Electronic Thesis or Diss., Sorbonne université, 2023. http://www.theses.fr/2023SORUS191.
Texte intégralThe ocean is known to play a key role in the carbon cycle. Without it, atmospheric CO2 levels would be much higher than what they are today thanks to the presence of carbon pumps that maintain a gradient of dissolved inorganic carbon (DIC) between the surface and the deep ocean. The biological carbon pump (BCP) is primarily responsible for this gradient. It consists in a series of ocean processes through which inorganic carbon is fixed as organic matter by photosynthesis in sunlit surface waters and then transported to the ocean interior and possibly the sediment where it will be sequestered from the atmosphere for millions of years. The BCP was long thought as solely the gravitational settling of particulate organic carbon (POC). However, a new paradigm for the BCP has recently been defined in which physically and biologically mediated particle injection pumps have been added to the original definition. Physically mediated particle injection pumps provide a pathway to better understand the transport of dissolved organic carbon (DOC) whereas biologically mediated particle injection pumps focus on the transport of POC by vertically migrating animals, either daily or seasonally. Therefore, a better understanding of these processes could help bridge the gap between carbon leaving the surface and carbon demand in the ocean interior. To address this new paradigm, this work will benefit from the advent of recent sensors that equip a new generation of Biogeochemical-Argo floats (BGC-Argo). The first part focuses on the development of an embedded zooplankton classification model for the Underwater Vision Profiler 6 (UVP6) under strict technical and energy constraints. The second part studies particle and carbon fluxes in the Labrador Sea using BGC-Argo floats equipped for the first time with the UVP6 and an optical sediment trap (OST), providing two independent measurements of sinking particles. The last part consists in revisiting the BCP using a new framework called CONVERSE for Continuous Vertical Sequestration. With this new approach, we re-evaluate the total carbon sequestered from the atmosphere (> 100 years) by the BCP and its transport pathways on the entire water column, in contrast to the carbon sequestration typically assumed below a fixed reference depth