4.7 Article

La Nina conditions influence interannual call detections of pygmy blue whales in the eastern Indian Ocean

Journal

FRONTIERS IN MARINE SCIENCE
Volume 9, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2022.850162

Keywords

pygmy blue whales; passive acoustic monitoring (PAM); El Nino southern oscillation; chlorophyll-a; long-term data; environmental drivers; La Nina; Indian Ocean

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Oceans are warming rapidly and marine ecosystems are changing, but there is a lack of information on how blue whales respond to these changes, especially in the Southern Hemisphere. Using 16 years of data, researchers studied the migration patterns of eastern Indian Ocean pygmy blue whales off Western Australia and found a positive correlation between whale call detections and El Nino Southern Oscillation (ENSO) cycles and the Indian Ocean Dipole (IOD). They also discovered that sea surface height and chlorophyll-a concentration influenced monthly whale call detections. This research is important for understanding how blue whales adapt to a changing environment and the potential impact of climate change on their reproductive success.
Oceans across the globe are warming rapidly and marine ecosystems are changing as a result. However, there is a lack of information regarding how blue whales are responding to these changing environments, especially in the Southern Hemisphere. This is because long term data are needed to determine whether blue whales respond to variability in environmental conditions. Using over 16 years of passive acoustic data recorded at Cape Leeuwin, we investigated whether oceanic environmental drivers are correlated with the migration patterns of eastern Indian Ocean (EIO) pygmy blue whales off Western Australia. To determine which environmental variables may influence migration patterns, we modelled the number of acoustic call detections of EIO pygmy blue whale calls with broad and fine scale environmental variables. We found a positive correlation between total annual whale call detections and El Nino Southern Oscillation (ENSO) cycles and the Indian Ocean Dipole (IOD), with more whale calls detected during La Nina years. We also found that monthly whale call detections correlated with sea surface height around the hydrophone and chlorophyll-a concentration at a prominent blue whale feeding aggregation area (Bonney Upwelling) where whales feed during the summer before migrating up the west Australian coast. At the interannual scale, ENSO had a stronger relationship with call detections than IOD. During La Nina years, up to ten times more EIO pygmy blue whale calls were detected than in neutral or El Nino years. This is likely linked to changes in productivity in the feeding areas of the Great Australian Bight and Indian Ocean. We propose that in lower productivity years whales either skipped migration or altered their habitat use and moved further offshore from the hydrophones and therefore were not detected. The frequency and intensity of ENSO events are predicted to increase with climate change, which is likely to impact the productivity of the areas used by blue whales. These changes in productivity may affect the physical condition and reproductive success of individual whales. A reduction in reproductive success could have a significant impact on blue whale recovery from historical whaling and their ability to adapt to a changing environment.

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