Decomposing acoustic signal reveals the pelagic response to a frontal system

• Main Authors: Izard, L., Fonvieille, N., Merland, C., Koubbi, P., Nerini, D., /Habasque, Jérémie, /Lebourges Dhaussy, Anne, Lo Monaco, C., /Roudaut, Gildas, d'Ovidio, F., Charrassin, J. B., Cotté, C.
• Format: Text
• Language: English
• Published: 2024
• Subjects: Multi-frequency hydroacoustics; Multivariate functional data analysis; Saint-Paul and Amsterdam french islands; Southern Indian Ocean; Southern Ocean
• Online Access: https://www.documentation.ird.fr/hor/fdi:010089609

The pelagic zone is home to a large diversity of organisms such as macrozooplankton and micronekton (MM), connecting the surface productive waters to the mesopelagic layers (200-1000 m) through diel vertical migrations (DVM). Active acoustics complement net sampling observations by detecting sound-scattering layers (SL) of organisms, allowing to monitor the MM dynamics with a high spatio-temporal resolution. Multifrequency analyses are a pertinent approach to better integrate the rich diversity of organisms composing SLs and their respective dynamics. However, analysing simultaneously emitted acoustic signals with distinct depth ranges and separating spatial from temporal variability is challenging and needs adapted tools to be fully exploited. This study examines the pelagic realm in a transition zone between the Southern Ocean and the subtropical Indian Ocean, crossing the Saint-Paul and Amsterdam islands' natural reserve. We extended a Multivariate Functional Principal Component Analysis (mfPCA) to analyse the joint vertical variation of five frequencies from two oceanographic cruises (2016 and 2022), allowing the decomposition of the acoustic dataset into orthogonal vertical modes (VM) of variability. We found the first VM to be linked to the temporal variability due to DVM, while the following majorly depict patterns in spatial distribution. Overall, from the subantarctic to the subtropical zones, we observed (i) enrichment of densities in the surface layer (0-100 m), (ii) a decrease in densities in the intermediate layer during the daytime (100-300 m) and (iii) the apparition of an intensive deep scattering layer on the 38 kHz. We explored VMs' connection with in -situ environmental conditions by clustering our observations into three distinct environmental-acoustic regions. These regions were compared with vertically integrated nautical area scattering coefficient distribution, a proxy for marine organisms' biomass. Additionally, we analysed species assemblage changes from complementary cruises to further ...