Temporal variability of vertical export flux at the DYFAMED time-series station (Northwestern Mediterranean Sea)

Type : ACL
Nature : Production scientifique
Au bénéfice du Laboratoire : Oui
Statut de publication : Publié
Année de publication : 2013
Auteurs (7) : HEIMBUERGER Lars-eric LAVIGNE Héloïse MIGON Christophe D'ORTENZIO Fabrizio ESTOURNEL Claude COPPOLA Laurent MIQUEL Juan-carlos
Revue scientifique : Progress In Oceanography
Volume : 119
Fascicule :
Pages : 59-67
DOI : 10.1016/j.pocean.2013.08.005
URL : <go to isi>://wos:000329018600006
Abstract : The temporal evolution of the vertical export flux at the DYFAMED time-series station (Ligurian Sea) over the last 20 years reveals a strong interannual variability. Winter convection allows particulate (and dissolved) matter to be vertically exported ("flush-down" effect). The efficiency of this process determines also the concentration of nutrients brought to surface waters and, therefore, the intensity of the subsequent phytoplankton bloom. The sequence "convection-bloom" is the main driving force of vertical export flux in this region. The present work attempts to better identify the parameters that control vertical export flux dynamics by observing a 20 year time-series in relation with the temporal variability of mixed layer depth and surface primary production. The consequences of a more stratified water column in the future on biological productivity and vertical export flux are pointed out. (C) 2013 Elsevier Ltd. All rights reserved.
Mots-clés : -
Commentaire : Times Cited: 3 Heimburger, Lars-Eric/A-4658-2012 Si 3
Tags : DYFAMED hauturier
Fichier attaché : -
Citation :
Heimbuerger L-E, Lavigne H, Migon C, D'Ortenzio F, Estournel C, Coppola L, Miquel J-C (2013) Temporal variability of vertical export flux at the DYFAMED time-series station (Northwestern Mediterranean Sea). Prog Oceanogr 119: 59-67 | doi: 10.1016/j.pocean.2013.08.005