Transport Pathways for Iron Supply to the Australian Antarctic Ridge Phytoplankton Bloom

• Published in: Geophysical Research Letters
• Main Authors: A. Vanegas Ledesma, L. N. Thomas
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2024
• Subjects: Geophysics. Cosmic physics; QC801-809; Antarc*; Antarctic; Ross Sea; Southern Ocean
• Online Access: https://doi.org/10.1029/2023GL108001; https://doaj.org/article/ac3633c42edc4e57b95aae4011a16d86

Abstract Biological productivity in the Southern Ocean is modulated by iron availability. Every summer, a large phytoplankton bloom forms northwest of the Ross Sea, above the Antarctic Australian Ridge (AAR), due to a plume of iron‐rich waters. Here, we investigate the origin and trajectories of these iron‐rich waters by analyzing water mass observations and Lagrangian experiments. Output from the Southern Ocean State Estimate (SOSE) and in situ measurements reveal that iron‐rich AAR bloom waters share properties with Modified Circumpolar Deep Water (MCDW), which forms on the Antarctic shelf‐slope. The Lagrangian experiments are conducted using SOSE velocities. Bloom waters tracked with virtual Lagrangian particles highlight an along isopycnal pathway of MCDW from Antarctica's shelf‐slope to the AAR bloom site, illustrating advection of these waters by the Balleny Gyre. These results are supported by temperature‐salinity analyses, which show a correlation between waters advected northwards; MCDW properties; and high iron concentrations.