Southern Ocean observations and change
Project Leader: Dr Steve Rintoul
Staff and students
Dr Laura Herraiz-Borreguero (CSIRO staff)
Mr Saisai Hou (Ocean University of China PhD student)
[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 Steve Rintoul talking to the camera and text appears: Steve Rintoul, CSHOR Project Leader, CSIRO]
Steve Rintoul: My project is looking at the Southern Ocean with an emphasis on observations of the Southern Ocean and we’re targeting a few different things. One is changes in the deep ocean. We’ve found some of the strongest signals of change anywhere in the deep ocean in the waters around Antarctica and we really need to understand why. What does it mean? What are the implications of that and why is it happening?
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And one way we’ll do that is through ships, the traditional way that we have of measuring the deepest parts of the ocean, but we’ll also be deploying the first pilot arrays of something called deep Argo floats. These are profiling floats that can work through the whole ocean depth.
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Eighty percent of the Southern Hemisphere is covered by oceans and they’ve been largely unmeasured and poorly understood.
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That’s beginning to change, and we can use that new information to develop new insights into how the Southern Hemisphere oceans work and how they affect regional and global climate.
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This project will achieve two things.
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One it will allow us to better understand how and why the deep ocean is changing and two how changes in the Southern Ocean will affect the Antarctic ice sheet where the waters interact with the floating ice around the edge of Antarctica.
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The project will collect new physical and biogeochemical observations in the Southern Ocean and use them with the historical record to develop a better physical understanding of the sensitivity of circulation and water mass formation to changes in forcing.
The overall objective of the project is to quantify variability and trends in ocean circulation and water mass formation in the Australian sector of the Southern Ocean, using a combination of shipboard data, float observations and satellite data, and to identify the physical mechanisms driving change.
Specific objectives include:
- Quantify full-ocean depth changes along the SR3 repeat hydrographic section between Tasmania and Antarctica
- As part of a collaborative project with NZ and the USA, use profiling floats to obtain the first comprehensive, year-round measurements of the Ross Gyre and quantify the circulation
- Lead the design and implementation of the first international deep Argo pilot array in the Southern Ocean
- Assess the potential for warm ocean waters to reach ice shelf cavities in East Antarctica and drive enhanced basal melt, with potential focus areas including Prydz Bay and the Shackleton Ice Shelf
Choosing the future of Antarctica
In a recent Nature article, Rintoul et al. present two narratives on the future of Antarctica and the Southern Ocean, from the perspective of an observer looking back from 2070. Read the CSHOR post, which includes a link to the full article, at this link.
The global influence of localised dynamics in the Southern Ocean
This Nature review by Dr Steve Rintoul evaluates the published research on Southern Ocean change: including changes in circulation, stronger winds, and increased freshwater input. The Southern Ocean exerts a disproportionate and profound influence on global ocean currents, climate, biogeochemical cycles, and sea level rise. The paper shows that substantial progress has been made in recent years in understanding the dynamics and global influence of the Southern Ocean. It is becoming clear that local scale processes play a fundamental part in shaping large-scale circulation. This is drive by the local topography which, of course, doesn’t change to a significant degree. Read the full article at this link.
Global warming is melting Antarctic ice from below
The results from a study published in Science Advances, and reported in a recent Guardian article, suggest that increased glacial meltwater input in a warming climate will both reduce Antarctic Bottom Water formation and trigger increased mass loss from the Antarctic Ice Sheet, with consequences for the global overturning circulation and sea level rise.
CSHOR is one of several organisations supporting the research and is duly acknowledged by the authors of the paper.
The figure below is an extract from the Science Advances paper.
Figure: Impact of glacial meltwater on dense water formation and shelf stratification.
On warm continental shelves, as those on the Sabrina Coast and in the Amundsen Sea (A), MCDW drives rapid ice shelf basal melt. The large volume of glacial meltwater prevents DSW formation in polynyas downstream of the meltwater outflow. MCDW remains in the bottom layer throughout the year in the polynya and further downstream, where it can access the ice shelf cavities. On cold continental shelves, the ice shelf cavities are filled by cold shelf waters, and basal melt rates are low. Glacial meltwater input is not sufficient to suppress winter convection in polynyas downstream of the meltwater outflow, as seen at Cape Darnley Polynya (B), allowing formation of DSW, the precursor to Antarctic Bottom Water.
|Cougnon, E. A., Galton-Fenzi, B. K., Rintoul, S. R., Legrésy, B., Williams, G. D., Fraser, A. D., & Hunter, J. R. (2017). Regional Changes in Icescape Impact Shelf Circulation and Basal Melting. Geophysical Research Letters, 44(22), 11,519-11,527. https://doi.org/10.1002/2017GL074943|
|Gao, L., Rintoul, S. R., & Yu, W. (2017). Recent wind-driven change in Subantarctic Mode Water and its impact on ocean heat storage. Nature Climate Change, 8, 58-63. https://doi.org/10.1038/s41558-017-0022-8|
|Langlais, C. E., Lenton, A., Matear, R., Monselesan, D., Legrésy, B., Cougnon, E., & Rintoul, S. (2017). Stationary Rossby waves dominate subduction of anthropogenic carbon in the Southern Ocean. Scientific Reports, 7(1), 17076. https://doi.org/10.1038/s41598-017-17292-3.|
|Pardo, P. C., Tilbrook, B., Langlais, C., Trull, T. W., & Rintoul, S. R. (2017). Carbon uptake and biogeochemical change in the Southern Ocean, south of Tasmania. Biogeosciences, 14(22), 5217-5237. https://www.biogeosciences.net/14/5217/2017/|
|Rintoul, S. R. (2018). The global influence of localized dynamics in the Southern Ocean. Nature, 558(7709), 209-218. https://doi.org/10.1038/s41586-018-0182-3|
|Rintoul, S. R., Chown, S. L., DeConto, R. M., England, M. H., Fricker, H. A., Masson-Delmotte, V., Naish, T. R., Siegert, M. J., & Xavier, J. C. (2018). Choosing the future of Antarctica. Nature, 558(7709), 233-241. https://doi.org/10.1038/s41586-018-0173-4|
|Schlitzer, R. et al. (2018). The GEOTRACES Intermediate Data Product 2017. Chemical Geology, 493, 210-223 (Rintoul one of 238 authors) https://doi.org/10.1016/j.chemgeo.2018.05.040|
|Snow, K., Rintoul, S. R., Sloyan, B. M., & Hogg, A. M. (2018). Change in Dense Shelf Water and Adélie Land Bottom Water Precipitated by Iceberg Calving. Geophysical Research Letters, 45(5), 2380-2387. https://doi.org/10.1002/2017GL076195|
|Silvano, A., Rintoul, S. R., Peña-Molino, B., Hobbs, W. R., van Wijk, E., Aoki, S., Tamura, T., & Williams, G. D. (2018). Freshening by glacial meltwater enhances melting of ice shelves and reduces formation of Antarctic Bottom Water. Science Advances, 4(4). http://advances.sciencemag.org/content/advances/4/4/eaap9467.full.pdf|