FN Archimer Export Format PT J TI Particle assemblage characterization in the Rhone river ROFI BT AF MANY, Gael BOURRIN, Francois DURRIEU DE MADRON, Xavier PAIRAUD, Ivane GANGLOFF, Aurelien DOXARAN, David ODY, Anouck VERNEY, Romaric MENNITI, Christophe LE BERRE, David JACQUET, Matthias AS 1:1;2:1;3:1;4:2;5:3;6:4;7:4;8:3;9:1;10:3;11:3; FF 1:;2:;3:;4:PDG-ODE-LITTORAL-LERPAC;5:PDG-ODE-DYNECO-DHYSED;6:;7:;8:PDG-ODE-DYNECO-DHYSED;9:;10:PDG-ODE-DYNECO-DHYSED;11:PDG-ODE-DYNECO-DHYSED; C1 UPVD, CNRS, UMR 5110, CEFREM, 52 Ave Paul Alduy, F-66860 Perpignan, France. IFREMER, LERPAC, F-83507 La Seyne Sur Mer, France. IFREMER, PHYSED, F-29280 Plouzane, France. UPMC, CNRS, UMR 7093, LOV, 181 Chemin Lazaret, F-06230 Villefranche Sur Mer, France. C2 UNIV PERPIGNAN, FRANCE IFREMER, FRANCE IFREMER, FRANCE UNIV PARIS 06, FRANCE SI TOULON BREST SE PDG-ODE-LITTORAL-LERPAC PDG-ODE-DYNECO-DHYSED IN WOS Ifremer jusqu'en 2018 copubli-france copubli-univ-france IF 2.439 TC 48 UR https://archimer.ifremer.fr/doc/00307/41809/41011.pdf LA English DT Article BO Antedon II DE ;Gulf of Lions;Rhone River;ROFI;Turbid structures;Particle properties;Glider AB An innovative experiment was carried out in the vicinity of the Rhône River mouth in February 2014. An instrumental package, composed of a CTD, a LISST-100 type B (1.25–250 μm) and a LISST-HOLO (20–2000 μm), was used to characterize the hydrological parameters and suspended particles properties (concentration, size, composition, shape and effective density) in the region of freshwater influence (ROFI) of the Rhône River. Besides, a coastal SLOCUM glider, equipped with a CTD and optical backscattering sensors at several wavelengths, was deployed to detail the spatial description of the hydrological parameters and some particle properties. Large river discharge (annual flood ~ 5000 m3 s− 1) and strong wind conditions favored the dispersal of the river plume on the shelf. Surface suspended particulate matter concentrations decreased rapidly seaward from 20 mg L− 1 next to the river mouth to 1.5 mg L− 1 at the shelf break. A persistent bottom nepheloid layer was observed across the shelf with concentrations decreasing from 8 mg L− 1 at the coast to 1 mg L− 1 at the shelf break. Observations showed that most of suspended particles were mainly flocculated in micro and macro-flocs (30–400 μm) in inner shelf waters. The particle assemblage in the Rhône River plume and in the bottom nepheloid layer became progressively finer seaward and the associated effective density increased from 370 to 1600 kg m− 3. Outside the plume, planktonic organisms increasingly contributed to the total volume concentration. Finally, we demonstrated the ability of gliders, equipped with optical backscattering sensors at several wavelengths, to describe the fine scale distributions of suspended particles, and provide an index of their size distribution. PY 2016 PD MAY SO Journal Of Marine Systems SN 0924-7963 PU Elsevier Science Bv VL 157 UT 000371938500003 BP 39 EP 51 DI 10.1016/j.jmarsys.2015.12.010 ID 41809 ER EF