For more than 10 years, Australian researchers have repeatedly sampled water from specific regions of the Southern Ocean to examine chemical properties, such as temperature and salinity, and physical attributes such as currents and the vertical movement of water. The rate at which water is transferred from the sea surface to the deep ocean determines how much heat and carbon dioxide (CO2) the ocean can store and therefore regulates the rate and magnitude of climate change.
Scientists have identified the major pathways involved in the movement of water around Antarctica and between the world's oceans. The work has contributed to improved climate change projections through new models that reproduce the mixing of water bodies and their effect on surface warming.
Ocean research has also shown that about half of all the CO2 released by human activities is now found in the world's oceans and that about a third of this has been taken up in the Southern Ocean. As CO2 continues to dissolve in the ocean it increases ocean acidity, making it harder for some marine organisms to form shells. These ecological changes in turn reduce the capacity of the ocean to absorb CO2.
How does the water change?
When (CO2) dissolves in water (H2O) it forms carbonic acid (H2CO3) – the same weak acid found in carbonated drinks. Increasing levels of carbonic acid interfere with the formation of calcium carbonate (CaCO3), a major structural component of the shells of many important planktonic organisms (free-floating marine plants, animals and microbes ranging in size from microscopic to several centimetres). Increasing acidity also affects the availability of nutrients in the ocean.
What effect will ocean acidification have?
As it becomes more difficult for calcium carbonate to form, it will become more difficult for some planktonic organisms to form shells. If their shells are thinner and/or deformed, the organisms may be unable to function properly. Many of these organisms are key components of the food chain – important in the diets of krill, fish, squid, penguins, seals and whales. They are also important in the removal of carbon from surface waters to the deep ocean and the release of oxygen into the air. Important metabolic processes, such as respiration in fish, may also be impaired by the acidity, as lowering the pH reduces the efficiency of oxygen exchange in their gills.
What organisms will be affected?
In the Southern Ocean and other open-ocean ecosystems, calcifying organisms affected will include snail-like molluscs called 'pteropods', abundant, single-celled algae called 'coccolithophorids' and protozoan 'foraminifera'. Changes in microbial populations are likely to flow on to dependent species throughout the food chain. In tropical coastal ecosystems coral reefs, comprised of colonies of small animals that secrete calcium carbonate skeletons, are also at risk.
How acidic will the oceans get?
The pH of seawater has historically remained at about 8.2, which is slightly alkaline (pure water is neutral - pH 7). However, CO2 from human activities has caused the pH of ocean surface waters to drop by 0.11 pH units. This might not sound like much, but it is equivalent to a 30% increase in acidity. Unless CO2 emissions are curbed, the pH is expected to fall by 0.5 pH units by 2100, a 320% increase in acidity.
How can we stop it?
Even if all carbon emissions stopped today, we are committed to a further drop of 0.1—0.2 pH units and it will take thousands of years for the oceans to recover. However, action now can prevent conditions, that are corrosive to calcifying organisms, from becoming more widespread.
What research is being done?
Scientists at the Australian Antarctic Division and the Antarctic Climate and Ecosystems Cooperative Research Centre, based in Hobart, are conducting a range of experiments on plankton and sediments from the Southern Ocean, to determine the effect of increasing CO2 on marine organisms and the impacts this will have on the ecosystem. A research voyages in 2007, the Sub-Antarctic Zone Sensitivity to Environmental Change conducted ship-board experiments and brought back samples for laboratory analysis.
Why is Southern Ocean research so important?
The Southern Ocean contains more CO2 than other oceans because cooler water absorbs more CO2 than warmer water. Thus, the impacts of ocean acidification will appear first in the Southern Ocean.
- Fact sheet on ocean acidification and the Southern Ocean [PDF] (2007 publication)
- 12 minute film on Ocean acidification: Connecting science, industry, policy and public, produced by Plymouth Marine Laboratory in the UK (12 May 2011)
- Ocean acidification research at the ACE CRC
- Climate science in the Southern Ocean (Chapter 2 of the 2008 report Australia's contribution to Antarctic climate science)
- News item (17 January 2007) - Cruising the sub-Antarctic for clues to ocean acidification
- Our research into marine microbial ecology
Australian Antarctic Magazine articles
- Looking to the past for changes in the present [PDF]
Fossils are helping scientists investigate changes in ocean ecosystems caused by increasing amounts of carbon dioxide dissolving in the ocean.
- Minicosms help build a bigger picture of ocean acidification [PDF]
By replicating the ocean ecosystem on a small scale, scientists aim to understand the effects of increasing ocean acidity on microbial communities.
- Aliens of the ocean – bizarre and beautiful [PDF]
Zooplankton like you've never seen them before.
- Ocean acidification: a newly recognised threat [PDF]
Carbon dioxide dissolved in the ocean produces acid that has damaging effects on marine organisms.