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Behagle Nolwenn, Roudaut Gildas, Josse Erwan, Brehmer Patrice, Cotte C., Duhamel G, Gautier O., Cherel Y., Rayan T. (2015). Acoustics characterization of micronekton spatial distribution in Indian Ocean using scientific surveys and integrated marine observing system database : acoustics characterization of micronekton. In : IEEE/OES Acoustics in Underwater Geosciences Symposium (RIO Acoustics). Piscataway : IEEE, 5 p. RIO Acoustics 2015, Rio de Janeiro (BRA), 2015/07/29-31.

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Lien direct chez l'éditeur doi:10.1109/RIOAcoustics.2015.7473616

Titre
Acoustics characterization of micronekton spatial distribution in Indian Ocean using scientific surveys and integrated marine observing system database : acoustics characterization of micronekton
Année de publication2015
Type de documentColloque
AuteursBehagle Nolwenn, Roudaut Gildas, Josse Erwan, Brehmer Patrice, Cotte C., Duhamel G, Gautier O., Cherel Y., Rayan T.
In IEEE/OES Acoustics in Underwater Geosciences Symposium (RIO Acoustics)
SourcePiscataway : IEEE, 2015, 5 p.
ColloqueRIO Acoustics 2015, Rio de Janeiro (BRA), 2015/07/29-31
RésuméIn this work scientific echosounder were used hull mounted onboard R/V Marion Dufresne II to scrutinize the vertical distribution of micronekton according to water masses characteristics along transect which were discriminated with spatial remote sensing data. Acoustic data were collected continuously at 38 kHz frequency during eighteen transits carried out in the South-West Indian Ocean (20-60°S, 50-80°E) between 2010 and 2014. The data set used includes scientific and opportunistic fishing surveys from Integrated Marine Observing System database. A structure in three main depth layers i.e., "surface", "intermediate" and "deep", has been found continuously all along the survey. Changes of micronektonic vertical structure were investigated along North South latitude: the surface layer acoustic density and thickness decrease by going southward. The intermediate layer is generally almost empty except between 30°S and 40°S. The deep layer acoustic density increases from North to South but its thickness does not change significantly. To assess the importance of these vertical changes, a spatially constrained clustering was applied on acoustic data and a positive correlation was established between vertical acoustic organization and oceanographic fronts' position. We conclude that spatial organization of micronekton is structured depending on water masses and confirm the interest of collecting acoustic data from fishery vessels to complete scientific surveys that are often restricted in time and space.
Plan de classementLimnologie biologique / Océanographie biologique [034] ; Télédétection [126] ; Limnologie physique / Océanographie physique [032]
LocalisationFonds IRD [F B010067521]
Identifiant IRDfdi:010067521
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010067521

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