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During the winter, when the index is high (NAO+), the Icelandic low draws a stronger south-westerly circulation over the eastern half of the North American continent which prevents Arctic air from plunging southward.
General circulation of the atmosphere is given by the position and intensity of major barrel systems of the continent (Azores High, Icelandic Low, Siberian High, Mediterranean cyclones), with greater frequency of western circulation.
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