The Bonney Coast upwelling: How physical processes shape the feeding behaviour of blue whales

Abstract

This study employs a fully coupled physical-biological model to explore the oceanic dynamics and phytoplankton production in one of Australia's most prominent coastal upwelling systems, the Bonney Coast Upwelling, that has barely been studied before. The study focusses on how physical processes provide two different food sources for blue whales (Balaenoptera musculus), namely, phytoplankton and krill (treated as nonbuoyant particles). While phytoplankton multiplies and grows rapidly within weeks in the euphotic zone in response to nutrient enrichment, krill can only be transported into the region via ambient currents. Findings of this study suggest that phytoplankton blooms appear slowly in the main upwelling plume on timescales of 4–8 weeks. Dynamical influences from incoming coastal Kelvin waves significantly weaken or strengthen this classical upwelling plume and its phytoplankton productivity. On the other hand, the upwelling-favorable wind induces a continuous coastal current that also extends eastward past the Bonney Coast. This current operates to transport and distribute krill (that cannot swim horizontally) westward along the shelf, which explains the apparent conundrum why blue whales also feed on the upstream side of the upwelling plume. The author postulates that the variability of both plankton production and the intensity of the upwelling flow (passing krill swarms along the shelf) control the feeding locations of blue whales and other baleen whales on Australia's southern shelves.