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Rivaling El Nino in scope and violence, and far more complex in structure, is the North Atlantic Oscillation. This see-sawing of atmospheric pressure between Iceland and the Azores has a major impact on winter weather from eastern North America to Siberia, and from Greenland to the equator. Unlike El Nino, which tends to crop up every two to seven years and dissipate after a year or so, the NAO seems to occur randomly and to hang in for years or even decades. Halfway around the world, scientists have been keeping an eye on another long-term cycle known as the Pacific Interdecadal Oscillation. Studies of snow pack in the Cascades and salmon catches in Alaska suggest that winters in the North Pacific alternate between 20 to 30 year runs of wet/cold weather and warm/dry weather. Is it possible that all of these large-scale modes of variability are in fact parts of one vast, infinitely complicated cycle of global oscillation? Answering this question will no doubt be one of the major climatological challenges of the coming century. Thanks today to contributing writer David Laskin, who also contributes to The Weather Notebook's new book, Soul of the Sky. For more information, visit our website, mountwashington.org. Thanks to Subaru and the National Science Foundation.
North Atlantic Oscillation Modelling - D. B. Stephenson
ENSO Forecast - LDEO Climate Group
Global Sea Surface Temperature charts
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