A review of the LATEX project: mesoscale to submesoscale processes in a coastal environment |
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Authors: | Anne A. Petrenko Andrea M. Doglioli Francesco Nencioli Marion Kersalé Ziyuan Hu Francesco d’Ovidio |
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Affiliation: | 1.Aix Marseille Université, Université de Toulon, CNRS, IRD, Mediterranean Institute of Oceanography (MIO),Marseille,France;2.Remote Sensing Group,Plymouth Marine Laboratory,Plymouth,UK;3.Department of Oceanography, Marine Research Institute,University of Cape Town,Rondebosch,South Africa;4.Jiaozhou Bay Marine Ecosystem Research Station, Institute of Oceanology,Chinese Academy of Sciences,Qingdao,China;5.Sorbonne Université (UPMC, Paris 6)/CNRS/IRD/MNHN, Laboratoire d’Océanographie et du Climat (LOCEAN), Institut Pierre Simon Laplace (IPSL),Paris,France |
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Abstract: | The main objective of the LAgrangian Transport EXperiment (LATEX) project was to study the influence of coastal mesoscale and submesoscale physical processes on circulation dynamics, cross-shelf exchanges, and biogeochemistry in the western continental shelf of the Gulf of Lion, Northwestern Mediterranean Sea. LATEX was a five-year multidisciplinary project based on the combined analysis of numerical model simulations and multi-platform field experiments. The model component included a ten-year realistic 3D numerical simulation, with a 1 km horizontal resolution over the gulf, nested in a coarser 3 km resolution model. The in situ component involved four cruises, including a large-scale multidisciplinary campaign with two research vessels in 2010. This review concentrates on the physics results of LATEX, addressing three main subjects: (1) the investigation of the mesoscale to submesoscale processes. The eddies are elliptic, baroclinic, and anticyclonic; the strong thermal and saline front is density compensated. Their generation processes are studied; (2) the development of sampling strategies for their direct observations. LATEX has implemented an adaptive strategy Lagrangian tool, with a reference software available on the web, to perform offshore campaigns in a Lagrangian framework; (3) the quantification of horizontal mixing and cross-shelf exchanges. Lateral diffusivity coefficients, calculated in various ways including a novel technique, are in the range classically encountered for their associated scales. Cross-shelf fluxes have been calculated, after retrieving the near-inertial oscillation contribution. Further perspectives are discussed, especially for the ongoing challenge of studying submesoscale features remotely and from in situ data. |
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