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The science behind an arctic blast involves a complex interplay of atmospheric conditions. The polar vortex, a dominant feature of the Arctic atmosphere, is usually held in place by the strong temperature gradient between the Arctic and lower latitudes. However, when this gradient weakens, often due to disturbances in the upper atmosphere, the vortex can become elongated or even split. This allows frigid Arctic air to spill southward. These disturbances can be caused by various factors, including changes in sea ice cover, snow cover, and atmospheric wave patterns. Understanding these dynamics is crucial for predicting and preparing for these extreme cold events.
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