Southern Ocean dynamics, circulation and water mass formation
Prof Matthew England (UNSW)
Staff and students
Dr Annie Foppert (CSIRO staff)
Dr Andrew Lenton (CSIRO staff)
Mr Zhi Li (UNSW PhD student)
Dr Steve Rintoul (CSIRO staff)
Dr Veronica Tamsitt (UNSW staff)
[Music plays and animation waves appear moving up from the bottom of the screen and text appears above: The Centre for Southern Hemisphere Oceans Research]
[Image shows animation waves moving up the screen and over the text and then the image changes to show Professor Matthew England talking to the camera and text appears: Prof. Matthew England, CSHOR Project Leader, University of New South Wales]
Professor Matthew England: The key thing we’re trying to answer in this project is understanding the drivers of the warming in the Southern Ocean.
[Image changes to show a view looking out over a sunrise view of the ocean from the stern of a ship and then the image changes to show a view looking over the bow of the ship]
The Southern Ocean has warmed at the surface in certain sectors, at depths of the shelves and in the ocean abyss, and that warming could have profound implications for climate and we’re trying to understand exactly what is driving that warming and what we can expect into the future.
[Image changes to show Matthew talking to the camera]
The big reason this research is important is that we need to understand what’s happening with the oceans right at the Antarctic margin.
[Image changes to show a view of an ice shelf looking from the deck of a ship and then the image changes to show Matthew talking to the camera]
This is where the oceans sit right up against the ice shelves and ice sheets and the warming there in certain sectors has been very worrying recently. It’s at a rate that exceeds our expectations.
[Image changes to show a graph displaying the global sea level rise and text appears: Global mean sea level anomalies]
With warming there we’re going to see much greater rates of ice melt and that ice melt will drive global sea level rise. So, this is a profound question for humanity.
[Image changes to show a view of the Investigator moving through the water towards the camera]
The goal with this project in CSHOR is to have a comprehensive understanding of the drivers of warming of the oceans around Antarctica.
[Image changes to show Matthew talking to the camera]
Hundreds of millions of people live near the coast around the globe and are vulnerable to even just one metre of sea level rise. The warming around Antarctica at the moment is enough to melt ice at a rate that will contribute to that sea level rise into the future and that will displace people globally. Understanding this rate of warming at the Antarctic margin will help us understand future sea level rise which will help us plan for this inevitable relocation of communities around the world’s coastlines.
[Music plays and the image changes to show animation waves across the bottom of the screen and Qingdao National Laboratory for Marine Science and Technology, CSIRO, UNSW and University of Tasmania logos appear]
CSHOR project team member Veronica Tamsitt joins the CAPSTAN voyage aboard the RV Investigator
One of CSHOR’s postdoctoral fellows and a , Veronica Tamsitt, sailed from Hobart to Fremantle as a trainer on an exciting 10-day educational voyage aboard the RV Investigator. Veronica joined 6 other researchers from a diverse group whose expertise span plankton biology to sediments and geophysics, to train a group of 20 honours, masters and PhD students at sea. Read more about the voyage at this link.
CSHOR Science Seminar Project Presentation (PDF) 2019
Moving windows to the deep ocean
Dr Veronica Tamsitt was invited to write a News and Views article titled, ‘Moving windows to the deep ocean’, for Nature Climate Change (Tamsitt 2018). A link to the article is listed below with the publication.
QNLM Academic Annual Meeting Young Scholars’ Prize
Dr Annie Foppert won second prize of 6,000 YUAN (~AU$1,200) for her presentation at the QNLM Academic Annual Meeting Young Scholars’ Forum held in Qingdao, China in mid-January 2019. Dr Foppert’s talk was titled, ‘Hot spots of eddy-driven transport across the East Antarctic slope’. QNLM invited many young scientists from QNLM partner organisations both in China and internationally to submit a presentation to the Forum. The presentations were of a high calibre across a broad range of ocean science disciplines. A photo from the award giving ceremony can be found on the website post at this link.
CSHOR Science Seminar Project Presentation 2018
Devries, T., Le Quéré C., Andrews, O., Berthet, S, Hauck, J. Ilyina, T., Landschützer, P., Lenton, A., Lima. I., Nowicki, M. Schwinger, J., Séférian, R. (2019). Decadal trends in the ocean carbon sink. Proceedings of the National Academy of Sciences, 116 (24), 11646-11651. https://doi.org/10.1073/pnas.1900371116.
Foppert, Annie (2019). Observed storm track dynamics in Drake Passage. Journal of Physical Oceanography, 3, 867-884. https://doi.org/10.1175/JPO-D-18-0150.1.
Hauck, J., Lenton, A., Langlais, C, Matear, R. J. (2018). The fate of carbon and nutrients exported out of the Southern Ocean. Global Biogeochemical Cycles, 32(10), 1556-1573. https://doi.org/10.1029/2018GB005977.
Holmes, R. M., J. D. Zika, and M. H. England (2019). Diathermal Heat Transport in a Global Ocean Model. Journal of Physical Oceanography, 49, 141-161. https://doi.org/10.1175/JPO-D-18-0098.1.
Purich, A., England, M. H., Cai, W., Sullivan, A., & Durack, P. J. (2018). Impacts of Broad-Scale Surface Freshening of the Southern Ocean in a Coupled Climate Model. Journal of Climate, 31(7), 2613-2632. https://doi.org/10.1175/JCLI-D-17-0092.1
Tamsitt, V (2018). Moving windows to the deep ocean (News and Views), Nature Climate Change, 8, 941-942. https://doi.org/10.1038/s41558-018-0324-5
Tamsitt, V., L. D. Talley and M. R. Mazloff (2019). A Deep Eastern Boundary Current carrying Indian Deep Water south of Australia. Journal of Geophysical Research: Oceans. https://doi.org/10.1029/2018JC014569.
Webb, D. J., R. M. Holmes, P. Spence, and M. H. England (2019). Barotropic Kelvin wave-induced bottom boundary layer warming along the West Antarctic Peninsula. Journal of Geophysical Research: Oceans. https://doi.org/10.1029/2018JC014227.
1. Warming in the surface Southern Ocean
Explore the drivers of the Amundsen-Bellingshausen Sea warming, including warming driven by changes in the pathway / temperatures of the Antarctic Circumpolar Current (ACC), atmospheric teleconnections from the tropics, and coupled ice-ocean feedbacks. A high-resolution ocean model will be used to examine the role of westerly wind anomalies and associated changes in the upwelling and poleward transport of Circumpolar Deep Water. Observations will be used to test and improve the model simulations.
2. Warming in the abyssal ocean
Configure a hierarchy of model experiments to investigate the sensitivity of the lower cell of the Southern Ocean overturning circulation to changes in forcing (wind, heat flux and freshwater fluxes from sea ice melt and melting ice shelves).
3. Warming over the Antarctic continental shelf
Explore what controls the delivery of ocean heat to Antarctic ice shelves. Simulations using global coupled models, high resolution regional models, and idealised process models will be used to assess the sensitivity of ocean – ice shelf interaction to changes in forcing.
4. Carbon uptake in the Southern Ocean
Explore the sensitivity of ocean carbon uptake to changes in the upper cell over the Southern Ocean. A high-resolution biogeochemical model will be used to determine the physical mechanisms responsible for exchange of carbon between the atmosphere and the Southern Ocean (both uptake of anthropogenic carbon and outgassing of natural carbon).
5. Dynamics of the Antarctic Circumpolar Current
Use high resolution models to explore Antarctic Circumpolar Current (ACC) dynamics, with a focus on interaction across scales. The momentum and vorticity budgets of the ACC have long been known to depend on interaction of the current with sea floor bathymetry, but exactly how the large-scale balances are maintained is not understood. Internal waves, sub-mesoscale filaments and mesoscale eddies all likely play a role in determining the response of the current to changes in forcing. High-resolution model studies will be used to explore the impact of local dynamics on the response of the ACC to anomalies in forcing.