LION observatory data

Date 2022-02-22
Temporal extent 2007 -2021
Author(s) Bosse AnthonyORCID1, Testor PierreORCID2, Coppola LaurentORCID3, Bretel Patrice2, Dausse Denis2, Durrieu De Madron XavierORCID4, Houpert LoïcORCID5, Labaste Matthieu2, Legoff Hervé2, Mortier Laurent2, 6, D’ortenzio Fabrizio3
Affiliation(s) 1 : Aix Marseille Univ, Université de Toulon, CNRS, IRD, MIO, Marseille, France
2 : CNRS / Laboratoire d'Océanographie et de Climatologie, Expérimentation et Approches Numériques (LOCEAN), Université Pierre et Marie Curie, 4 Place Jussieu, 75252 Paris cedex 05, France
3 : Sorbonne Université, CNRS, Institut de la Mer de Villefranche, LOV, Villefranche-sur-Mer, France
4 : Laboratoire CEFREM - UMR 5110 CNRS-UPVD 52, avenue Paul Alduy, 66860 PERPIGNAN Cedex, France
5 : SAMS, Scottish Marine Institute, Oban, Argyll, PA37 1QA, UK
6 : ENSTA ParisTech, Palaiseau, France
DOI 10.17882/44411
Publisher SEANOE
Abstract

The Lion mooring is located in the center of the Gulf of Lion where one of the largest open sea convection happens in the winter period. This open sea convection is an active vertical mixing that concerns the whole northern Mediterranean and can reach great deep in the Gulf of Lion (where it may even reach the bottom ~ 2500m) due to the Mistral and Tramontane, cold and dry winds. This is the phenomenon of dense water formation which is the only mechanism for the ventilation of the deep waters of the entire western Mediterranean. It was observed that the deep waters can be formed 1) in a preconditioned open sea area and 2) on the shelf with a subsequent cascading down the slope. There are therefore two modes whose interannual monitoring is necessary to understand the evolution of Mediterranean deep waters and validate ocean numerical models of the region. The LION mooring is deployed and maintained since 2007. It aims to observe the winter dense water formation affecting the north-western Mediterranean Sea water circulation and deep-sea ecosystem (physical data). The mooring is deployed near the ODAS meteorological surface buoy (ODAS Lion, Meteo France) and integrated in the MOOSE network since 2010. It is part of the FIXO3 and OceanSites systems.

Licence CC-BY
User's manual

http://dx.doi.org/10.1002/2016JC011857

Data
File Size Format Processing Access Key
156 MB NC, NetCDF Quality controlled data Access on demand 44587
57 MB NC, NetCDF Quality controlled data Access on demand 56570
58 MB NC, NetCDF Quality controlled data Access on demand 63067
62 MB NC, NetCDF Quality controlled data Access on demand 76534
2007-2021 data 70 MB NC, NetCDF Quality controlled data Open access 91718
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How to cite 

Bosse Anthony, Testor Pierre, Coppola Laurent, Bretel Patrice, Dausse Denis, Durrieu De Madron Xavier, Houpert Loïc, Labaste Matthieu, Legoff Hervé, Mortier Laurent, D’ortenzio Fabrizio (2022). LION observatory data. SEANOE. https://doi.org/10.17882/44411


In addition to properly cite this dataset, it would be appreciated that the following work(s) be cited too, when using this dataset in a publication :


Houpert L., Durrieu De Madron X. Durrieu, Testor P., Bosse A., D'Ortenzio F., Bouin M. N., Dausse D., Le Goff H., Kunesch S., Labaste M., Coppola L., Mortier L., Raimbault P. (2016). Observations of open-ocean deep convection in the northwestern Mediterranean Sea: Seasonal and interannual variability of mixing and deep water masses for the 2007–2013 period. Journal Of Geophysical Research-oceans, 121(11), 8139-8171. Publisher's official version : https://doi.org/10.1002/2016JC011857 , Open Access version : https://archimer.ifremer.fr/doc/00355/46588/