Coupling physical and biogeochemical processes in the Rio de la Plata plume Auteur(s) : Huret, Martin Dadou, Isabelle Dumas, Franck Lazure, Pascal Garcon, Véronique Éditeur(s) : Elsevier Résumé : A coupled three-dimensional physical-biogeochemical model was developed in order to simulate the ecological functioning of the Rio de la Plata estuary and plume. The biogeochemical model reproduces the nitrogen cycle between five compartments: dissolved inorganic nitrogen, phytoplankton, zooplankton, detritus and dissolved organic nitrogen. The coupling is tested in seasonal climatological configurations and for the particular year 1999. The circulation is forced with Parana and Uruguay rivers discharges, NCEP wind and tide. The biogeochemical model includes loads of inorganic and organic nitrogen from both rivers. The model reproduces the correct tidal amplitudes in the estuary, as well as the most outstanding features of the observed horizontal and vertical structures of the salinity plume. Simulated surface chlorophyll a concentrations exhibit maximum values all year long seaward of the turbidity front, between the 0.5 and 15 isohalines, in agreement with SeaWiFS images of the area. The model simulates well the low primary production in the light-limited highly turbid tidal river (20 gC/m(2)/yr), the high production area in the frontal zone where it can reach 500 gC/m(2)/yr, and the nutrient-limited production in the outer estuary and inner shelf (300 gC/m(2)/yr), with realistic values in each case. According to the 1999 model simulation, the tidal river is the location of organic nitrogen remineralization with a consequent increase of the inorganic pool. At the entrance of the frontal zone, inorganic nitrogen represents about 75% of the whole nitrogen pool, it is reduced to 50% at its sea end-member. The outer estuary has the same sink role for inorganic nitrogen, suggesting that organic nitrogen is the major form exported to the shelf. Continental Shelf Research (0278-4343) (Elsevier), 2005-03 , Vol. 25 , N. 5-6 , P. 629-653 Droits : 2004 Elsevier Ltd. http://archimer.ifremer.fr/doc/2005/publication-334.pdf DOI:10.1016/j.csr.2004.10.003 http://archimer.ifremer.fr/doc/00000/334/ | Partager Voir aussi Rio de la Plata SeaWiFS Primary production Chlorophyll River plumes Biogeochemical modelling Physical Télécharger |
Larval Dispersal Modeling of Pearl Oyster Pinctada margaritifera following Realistic Environmental and Biological Forcing in Ahe Atoll Lagoon Auteur(s) : Thomas, Yoann Dumas, Franck Andrefouet, Serge Éditeur(s) : Public Library Science Résumé : Studying the larval dispersal of bottom-dwelling species is necessary to understand their population dynamics and optimize their management. The black-lip pearl oyster (Pinctada margaritifera) is cultured extensively to produce black pearls, especially in French Polynesia's atoll lagoons. This aquaculture relies on spat collection, a process that can be optimized by understanding which factors influence larval dispersal. Here, we investigate the sensitivity of P. margaritifera larval dispersal kernel to both physical and biological factors in the lagoon of Ahe atoll. Specifically, using a validated 3D larval dispersal model, the variability of lagoon-scale connectivity is investigated against wind forcing, depth and location of larval release, destination location, vertical swimming behavior and pelagic larval duration (PLD) factors. The potential connectivity was spatially weighted according to both the natural and cultivated broodstock densities to provide a realistic view of connectivity. We found that the mean pattern of potential connectivity was driven by the southwest and northeast main barotropic circulation structures, with high retention levels in both. Destination locations, spawning sites and PLD were the main drivers of potential connectivity, explaining respectively 26%, 59% and 5% of the variance. Differences between potential and realistic connectivity showed the significant contribution of the pearl oyster broodstock location to its own dynamics. Realistic connectivity showed larger larval supply in the western destination locations, which are preferentially used by farmers for spat collection. In addition, larval supply in the same sectors was enhanced during summer wind conditions. These results provide new cues to understanding the dynamics of bottom-dwelling populations in atoll lagoons, and show how to take advantage of numerical models for pearl oyster management. Plos One (1932-6203) (Public Library Science), 2014-04 , Vol. 9 , N. 4 , P. e95050 Droits : 2014 Thomas et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited http://archimer.ifremer.fr/doc/00197/30843/29210.pdf DOI:10.1371/journal.pone.0095050 http://archimer.ifremer.fr/doc/00197/30843/ | Partager |
General Introduction: PREVIMER, a French pre-operational coastal ocean forecasting capability. Auteur(s) : Dumas, Franck Pineau-guillou, Lucia Lecornu, Fabrice Le Roux, Jean-francois Le Squere, Bruno Éditeur(s) : Mercator Ocean Résumé : Pre-operational system PREVIMER provides with coastal observations and forecasts along French coasts: currents, waves, sea levels, temperature, salinity, primary production and turbidity. These marine environmental data come from in situ observations, satellite images, and numerical models. They are centralized and archived in PREVIMER databases, then published on website (real time and historical data), and freely available to users, private companies as well as public administrations. This paper describes in details PREVIMER components and users. Mercator Ocean - Quarterly Newsletter (Mercator Ocean), 2014 , N. 49 , P. 3-8 Droits : info:eu-repo/semantics/openAccess http://archimer.ifremer.fr/doc/00189/30037/28523.pdf http://archimer.ifremer.fr/doc/00189/30037/ | Partager |
Circulation and suspended sediment transport in a coral reef lagoon: The south-west lagoon of New Caledonia Auteur(s) : Ouillon, S. Douillet, Pascal Lefebvre, J. P. Le Gendre, Romain Jouon, Aymeric Bonneton, P. Fernandez, Chevillon, C. Éditeur(s) : Pergamon-elsevier Science Ltd Résumé : The south-west lagoon of New Caledonia is a wide semi-open coral reef lagoon bounded by an intertidal barrier reef and bisected by numerous deep inlets. This paper synthesizes findings from the 2000-2008 French National Program EC2CO-PNEC relative to the circulation and the transport of suspended particles in this lagoon. Numerical model development (hydrodynamic, fine suspended sediment transport, wind-wave, small-scale atmospheric circulation) allowed the determination of circulation patterns in the lagoon and the charting of residence time, the later of which has been recently used in a series of ecological studies. Topical studies based on field measurements permitted the parameterisation of wave set-up induced by the swell breaking on the reef barrier and the validation of a wind-wave model in a fetch-limited environment. The analysis of spatial and temporal variability of suspended matter concentration over short and long time-scales, the measurement of grain size distribution and the density of suspended matter (1.27 kg 1(-1)), and the estimation of erodibility of heterogeneous (sand/mud, terrigenous/biogenic) soft bottoms was also conducted. Aggregates were shown to be more abundant near or around reefs and a possible biological influence on this aggregation is discussed. Optical measurements enabled the quantification of suspended matter either in situ (monochromatic measurements) or remotely (surface spectral measurements and satellite observations) and provided indirect calibration and validation of a suspended sediment transport model. The processes that warrant further investigation in order to improve our knowledge of circulation and suspended sediment transport in the New Caledonia lagoon as well as in other coral reef areas are discussed, as are the relevance and reliability of the numerical models for this endeavour. Marine Pollution Bulletin (0025-326X) (Pergamon-elsevier Science Ltd), 2010 , Vol. 61 , N. 7-12 , P. 269-296 Droits : 2010 Elsevier Ltd All rights reserved. http://archimer.ifremer.fr/doc/00014/12526/9401.pdf DOI:10.1016/j.marpolbul.2010.06.023 http://archimer.ifremer.fr/doc/00014/12526/ | Partager Voir aussi Hydrodynamics Suspended sediment New Caledonia Coral reef lagoon Sediment Turbidity Resuspension Télécharger |
Synthèse hydrobiologique du site électronucléaire de Flamanville Auteur(s) : Dreves, Luc Lampert, Luis Abernot, Chantal Martin, Jocelyne Arzel, Pierre Dumas, Franck Latrouite, Daniel Schlaich, Ivan Résumé : This synthesis report assesses the current state of the marine hydrobiological knowledge acquired in the surroundings of the Flamanville electronuclear site (north-west of Cotentin), in the framework of the various project and monitoring programs in the pelagic, benthic and halieutic domains carried out on this site since 1976. Each domain is divided, as much as necessary, into different study areas such as hydrobiology, phytoplankton, microbiology, crustacean larvae or macrophyte algae. For each area, a series of parameters, considered as representative of the evolution of this area, is studied. In this way, for the hydrological area, the sea water temperature and salinity, the mineral nutriment concentrations, the holagen compounds and the boron are monitored. The evolution of each of these parameters enabled us to draw the following conclusions. The vegetal and animal species' physiology is conditioned by climate changes. The study of the pluviometry and air temperature parameters shows that the 1986/2005 period is slightly less humid and warmer than the 1949/2005 period. This reflects also on the sea water temperature whose average values increase on a regular basis. Ce rapport de synthèse fait le point sur l'état des connaissances hydrobiologiques marines acquises aux abords du site électronucléaire de Flamanville (nord-ouest Cotentin), dans le cadre des différents programmes de projet et de surveillance des domaines pélagique, benthique et halieutique, menés sur ce site depuis 1976. Chaque domaine est divisé, autant que nécessaire, en compartiments d'étude, tels que l'hydrologie, le phytoplancton, la microbiologie, les larves de crustacés ou les algues macrophytes. Pour chaque compartiment, une série de paramètres, jugés représentatifs de l'évolution de ce compartiment, est étudié. Ainsi, pour le compartiment hydrologique, sont suivis la température et la salinité de l'eau de mer, les concentrations en nutriments minéraux, les composés halogénés et le bore. Les évolutions de ces différents paramètres ont permis d'élaborer les conclusions suivantes. La physiologie des espèces animales et végétales est conditionnée par les changements climatiques. L'examen des paramètres pluviométrie et température de l'air montre que la période 1986/2005 est sensiblement plus humide et plus chaude que la période 1949/2005. Cela se répercute également sur la température de l'eau de mer dont les valeurs moyennes croissent régulièrement. Droits : info:eu-repo/semantics/openAccess http://archimer.ifremer.fr/doc/2006/rapport-6405.pdf http://archimer.ifremer.fr/doc/00000/6405/ | Partager |