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The
ability of the Southern Ocean to remove carbon dioxide from the
atmosphere is being eroded by climate change, say environmental
researchers. If the trend [tendance] continues, then the ability of this 'carbon
sink' to deal with humankind's greenhouse emissions will be impaired.
Roughly
half of the carbon dioxide that enters the atmosphere is absorbed by
the world's oceans, so as greenhouse emissions increase, the amount
taken up by the oceans should increase in proportion. But the new
research suggests that the Southern Ocean is not keeping pace with
rising emissions. These Antarctic waters are an important sink for
carbon dioxide, thanks to ocean currents and cold temperatures - they
are thought to account for some 15% of the world's oceanic
carbon-storage capacity.
Researchers
led by Corinne Le Quéré of the Max Planck Institute of Biochemistry in
Martinsried, Germany, took data from 11 coastal monitoring stations in
Antarctica and on islands in the Southern Ocean to measure the amount
of carbon dioxide being stored and released by the ocean. They then
compared this measurements of global atmospheric carbon dioxide levels
to work out the change in the performance of the carbon sink.
Since
1981, the percentage of atmospheric carbon dioxide that the Southern
Ocean can hold has decreased, the researchers report in a study
published online by Science.
The trend suggests that, for each decade, the annual capacity of the
ocean to store carbon has gone down by 0.08 gigatonnes compared with
expectations. On average, the ocean stores between 0.1 and 0.6
gigatonnes a year.
This
is a small amount compared with the roughly 8 gigatonnes of carbon
dioxide pumped out each year by human activities such as energy
generation. But any decline is important, as oceans are an important
long-term sink. If humans can bring carbon dioxide emissions under
control in the long term, the world's oceans are predicted to sequester
between 70% and 80% of the total net anthropogenic emissions of the
industrial era.
Winds of change
The
main cause of the changes seems to be a relatively rapid increase in
average wind strengths over the Southern Ocean, Le Quéré and her team
report. These stronger winds, thought to be driven by the depletion of
the ozone layer over Antarctic regions, churn up the ocean and bring
more dissolved carbon up from the depths.
This
was unexpected, says Le Quéré. But when the researchers plugged their
data into a computer model and removed these stronger winds, they did
indeed find that much of the observed reduction in the carbon sink
disappeared.
An increase in global temperature is predicted to worsen the effect, since warmer waters hold less gas.
South to north
"The
possibility that in a warmer world the Southern Ocean - the strongest
ocean sink - is weakening, is a cause for concern," comments Chris
Rapley, director of the British Antarctic Survey in Cambridge, UK.
The
Southern Ocean is the only body of water for which this trend has been
definitely spotted and quantified, says Le Quéré, although shorter-term
studies suggest that a similar process may be occurring in the North
Atlantic.
If the phenomenon is happening world-wide, this would undoubtedly affect efforts to stabilize atmospheric greenhouse gases.
A
reduction in sink capacities will make it harder for international
efforts, such as carbon trading and changes in methods of energy
generation, to set achievable targets for stabilizing greenhouse-gas
levels. But Le Quéré says that such efforts now need to be redoubled,
rather than accepting that greenhouse gas levels will be higher in
future. "Targets should depend on the level of danger [from global
warming]," she says.
References : Le Quéré C., et al. Science, doi:10.1126/science.1136188 (2007).