Exploitable results – Impact of dense shelf water cascading and open-sea convection in the northwestern Mediterranean during winter 2012, on deep-sea biological activity particle fluxes and sediment dynamics
Result descriptionFive months after the formation of a massive dense water on the continental shelf and in the deep basin of the Gulf of Lions the water of coastal origin created a distinct bottom layer up to a few hundreds of meters thick over the central part of the NW Mediterranean basin, which was overlaid by a layer of newly formed deep water produced by open-sea convection. These new observations highlight the role of intense episodes of both dense shelf water cascading and open-sea convection to the progressive modification of the NW Mediterranean deep waters.
Result type* Scientific Publication
Link to result
ReferencesDurrieu de Madron, X. et al. 2013. Interaction of dense shelf water cascading and open-sea convection in the northwestern Mediterranean during winter 2012. Geophysical Research Letters, Vol. 40: 1379–1385, doi:10.1002/grl.50331, link: http://www.perseus-net.eu/assets/media/PDF/703.pdf Tamburini C et al. (2013) Deep Deep-Sea Bioluminescence Blooms after Dense Water Formation at the Ocean Surface. PLoS ONE 07:2013; 8(7):e67523 link: http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0067523 Stabholz, M.et al. 2012. Impact of open-ocean convection on particle fluxes and sediment dynamics in the deep margin of the Gulf of Lions, Biogeosciences Discuss., 9, 12845-12894; link: http://www.perseus-net.eu/assets/media/PDF/PERSEUS%20Publications/5126.%202012.pdf
Numéro d'enregistrement: 181959 / Dernière mise à jour le: 2016-04-29
Source d'information: Marine Information Platform