Publications des scientifiques de l'IRD

Rousselet L., de Verneil A., Doglioli A. M., Petrenko A. A., Duhamel S., Maes Christophe, Blanke B. (2018). Large- to submesoscale surface circulation and its implications on biogeochemical/biological horizontal distributions during the OUTPACE cruise (southwest Pacific). Biogeosciences, 15 (7), p. 2411-2431. ISSN 1726-4170.

Titre du document
Large- to submesoscale surface circulation and its implications on biogeochemical/biological horizontal distributions during the OUTPACE cruise (southwest Pacific)
Année de publication
2018
Type de document
Article référencé dans le Web of Science WOS:000430510700002
Auteurs
Rousselet L., de Verneil A., Doglioli A. M., Petrenko A. A., Duhamel S., Maes Christophe, Blanke B.
Source
Biogeosciences, 2018, 15 (7), p. 2411-2431 ISSN 1726-4170
The patterns of the large-scale, meso- and sub-mesoscale surface circulation on biogeochemical and biological distributions are examined in the western tropical South Pacific (WTSP) in the context of the OUTPACE cruise (February-April 2015). Multi-disciplinary original in situ observations were achieved along a zonal transect through the WTSP and their analysis was coupled with satellite data. The use of Lagrangian diagnostics allows for the identification of water mass pathways, mesoscale structures, and submesoscale features such as fronts. In particular, we confirmed the existence of a global wind-driven southward circulation of surface waters in the entire WTSP, using a new high-resolution altimetry-derived product, validated by in situ drifters, that includes cyclogeostrophy and Ekman components with geostrophy. The mesoscale activity is shown to be responsible for counter-intuitive water mass trajectories in two subregions: (i) the Coral Sea, with surface exchanges between the North Vanuatu Jet and the North Caledonian Jet, and (ii) around 170 degrees W, with an eastward pathway, whereas a westward general direction dominates. Fronts and small-scale features, detected with finite-size Lyapunov exponents (FSLEs), are correlated with 25% of surface tracer gradients, which reveals the significance of such structures in the generation of submesoscale surface gradients. Additionally, two high-frequency sampling transects of biogeochemical parameters and microorganism abundances demonstrate the influence of fronts in controlling the spatial distribution of bacteria and phytoplankton, and as a consequence the microbial community structure. All circulation scales play an important role that has to be taken into account not only when analysing the data from OUTPACE but also, more generally, for understanding the global distribution of biogeochemical components.
Plan de classement
Limnologie physique / Océanographie physique [032] ; Ecologie, systèmes aquatiques [036] ; Télédétection [126]
Description Géographique
PACIFIQUE SUD OUEST ; ZONE TROPICALE
Localisation
Fonds IRD [F B010072737]
Identifiant IRD
fdi:010072737
Contact