Coronavirus Information for the UC San Diego Community

Our leaders are working closely with federal and state officials to ensure your ongoing safety at the university. Stay up to date with the latest developments. Learn more.

Variability in summer surface residence time within a West Antarctic Peninsula biological hotspot

TitleVariability in summer surface residence time within a West Antarctic Peninsula biological hotspot
Publication TypeJournal Article
Year of Publication2018
AuthorsKohut J.T, Winsor P., Statscewich H., Oliver M.J, Fredj E., Couto N., Bernard K., Fraser W.
JournalPhilosophical Transactions of the Royal Society a-Mathematical Physical and Engineering Sciences
Date Published2018/06
Type of ArticleArticle
ISBN Number1364-503X
Accession NumberWOS:000432326900003
Keywordsaggregations; biological hotspot function; Canyon; circulation; circumpolar deep-water; continental-shelf; currents; high-freguency radar; Krill; Lagrangian particle; residence time; Science & Technology - Other Topics; trajectories; transport; west antarctic peninsula; Zooplankton

Palmer Deep canyon along the central West Antarctic Peninsula is known to have higher phytoplankton biomass than the surrounding noncanyon regions, but the circulation mechanisms that transport and locally concentrate phytoplankton and Antarctic krill, potentially increasing prey availability to upper-trophic-level predators such as penguins and cetaceans, are currently unknown. We deployed a three-site high-frequency radar network that provided hourly surface circulation maps over the Palmer Deep hotspot. A series of particle release experiments were used to estimate surface residence time and connectivity across the canyon. The majority of residence times fell between 1.0 and 3.5 days, with a mean of 2 days and a maximum of 5 days. We found a highly significant negative relationship between wind speed and residence time. Our residence time analysis indicates that the elevated phytoplankton biomass over the central canyon is transported into and out of the hotspot on time scales much shorter than the observed phytoplankton growth rate, suggesting that the canyon may not act as an incubator of phytoplankton productivity as previously suggested. It may instead serve more as a conveyor belt of phytoplankton biomass produced elsewhere, continually replenishing the phytoplankton biomass for the local Antarctic krill community, which in turn supports numerous top predators. This article is part of the theme issue 'The marine system of the West Antarctic Peninsula: status and strategy for progress in a region of rapid change'.

Short TitlePhilos. Trans. R. Soc. A-Math. Phys. Eng. Sci.
Student Publication: