Oceans Losing Ability to Absorb Carbon Dioxide

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    Oceans Losing Ability to Absorb Carbon Dioxide

     
     May 2007 -   Recent climate change brought on by 
    human activities has weakened one the Earth's natural defenses against 
    global warming. Atmospheric carbon dioxide is not being absorbed by the 
    Southern Ocean as quickly as it once was, an international research team 
    has found. 
    Scientists have observed the first evidence that the Southern Ocean’s 
    ability to absorb the major greenhouse gas carbon dioxide, CO2, has 
    weakened by about 15 percent per decade since 1981. The study was 
    published today in the journal "Science." 
    "This is the first time that we’ve been able to say that climate change 
    itself is responsible for the saturation of the Southern Ocean sink. This 
    is serious," said lead author Dr. Corinne Le Quere of the University of 
    East Anglia and the British Antarctic Survey. 
    Dr. Corinne Le Quere is on the faculty of the School of Environmental 
    Sciences, University of East Anglia and is a strategic alliance senior 
    fellow at the British Antarctic Survey. 
    "All climate models predict that this kind of feedback will continue and 
    intensify during this century," said Dr. Le Quere. 
    "The Earth’s carbon sinks – of which the Southern Ocean accounts for 15 
    percent – absorb about half of all human carbon emissions. With the 
    Southern Ocean reaching its saturation point more CO2 will stay in our 
    atmosphere," she said. 
    Such weakening of one of the Earth’s major carbon dioxide sinks will lead 
    to higher levels of atmospheric carbon dioxide in the long term. 
    And the study suggests that stabilization of atmospheric carbon dioxide is 
    even more difficult to achieve than previously thought. 
    Additionally, acidification in the Southern Ocean is likely to reach 
    dangerous levels earlier than the projected date of 2050, the scientists 
    said. 
    Research vessel makes its way across the Southern Ocean. 
    The international team included researchers from CSIRO in Australia, the 
    Max-Planck Institute in Germany, the University of East Anglia and British 
    Antarctic Survey in England, the Climate Monitoring and Diagnostics 
    Laboratory in the United States, New Zealand's National Institute of Water 
    and Atmospheric Research, the South African Weather Service, LSCE/IPSL and 
    CNRS in France, and the Centre for Atmospheric and Oceanic Studies in 
    Japan. 
    Professor Chris Rapley, director of British Antarctic Survey said, "Since 
    the beginning of the industrial revolution the world’s oceans have 
    absorbed about a quarter of the 500 gigatons of carbon emitted into the 
    atmosphere by humans. The possibility that in a warmer world the Southern 
    Ocean – the strongest ocean sink - is weakening is a cause for concern." 
    The saturation of the Southern Ocean was revealed by scrutinizing 
    observations of atmospheric carbon dioxide from 40 stations around the 
    world. 
    The data show that since 1981 the Southern Ocean sink ceased to increase, 
    whereas CO2 emissions increased by 40 percent. 
    Dr. Paul Fraser, who leads research into atmospheric greenhouse gases at 
    CSIRO Marine and Atmospheric Research, says the team’s four year study 
    concludes that the weakening is due to human activities. 
    "The researchers found that the Southern Ocean is becoming less efficient 
    at absorbing carbon dioxide due to an increase in wind strength over the 
    ocean, resulting from human-induced climate change," Dr. Fraser says. 
    Data from the monitoring station at Cape Grim, Tasmania, Australia was 
    used in the Southern Ocean carbon sink study. 
    "The increase in wind strength is due to a combination of higher levels of 
    greenhouse gases in the atmosphere and long-term ozone depletion in the 
    stratosphere, which previous CSIRO research has shown intensifies storms 
    over the Southern Ocean," he said. 
    The increased winds influence the processes of mixing and upwelling in the 
    ocean, which in turn cause an increased release of carbon dioxide into the 
    atmosphere, reducing the net absorption of carbon dioxide into the ocean, 
    he explained. 
    Dr. Fraser points to one piece of good news - ozone levels in the 
    stratosphere have stopped declining and should recover slowly in coming 
    decades. 
    "Thus the impact of ozone depletion on the Southern Ocean carbon dioxide 
    sink will lessen in the future," he said, "but the impact of increasing 
    levels of greenhouse gases will continue unabated."    
           
          







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