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    Warm Sea Water Toward Antarctic Glaciers Is Constant, Not Seasonal
    By News Staff | December 6th 2012 11:30 AM | Print | E-mail | Track Comments

     A large problem in making predictions about Antarctic melting is that we currently have insufficient knowledge about the ocean circulation near large glaciers in West Antarctica. This means that researchers cannot predict how water levels will change in the future with any large degree of certainty. 

    What is known is that the ice sheet in West Antarctica is melting faster than expected, and new observations published by oceanographers in Nature Geoscience may improve the ability to predict future changes in ice sheet mass. 

    A reduction of the ice sheets in Antarctica and Greenland would affect the water levels of the world's oceans. 
    One reason why West Antarctica is particularly sensitive is that the majority of the ice rests on areas that are below sea level. Warm sea water penetrates beneath the ice, causing increased melting from underneath.

    Until now, researchers have been referred to studies that use high-resolution computer models.

     "But there have been very few oceanographic measurements from the Amundsen Sea to confirm or contradict the results from the computer models. Nor has there been any winter data. Sea ice and icebergs have made it impossible to get there in the winter, and it isn't easy to have instruments in place all year round," 
    says researcher Lars Arneborg from the Department of Earth Sciences at the University of Gothenburg. "There is a clear reduction in the ice mass in West Antarctica, especially around the glaciers leading into the Amundsen Sea. It is therefore probably a change in the ocean circulation in the Amundsen Sea that has caused this increased melting."

    Since 2010, researchers had instruments positioned in the Amundsen Sea, enabling them to measure the inward flow of warm sea water towards the glaciers. The observations show that the warm sea water flows towards the glaciers in a more or less constant way, in contrast to the model results which suggested a strong seasonal cycle.

    "This shows just how important observations are for investigating whether the models we use describe something that resembles reality. Warm ocean currents have caused much more melting than any model has predicted, both in West Antarctica and around Greenland."

    The researchers want more and longer time series of oceanographic observations in order to improve the models and achieve a better understanding.

    "Only then will we be able to say something about how the ice masses of the Antarctic and Greenland will change in the future."