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This decreased gradient slows down the jet stream—and as it slows, it also seems to become wavier, plunging south or veering north when encountering atmospheric obstacles it would once have coursed straight through. “The best analogy is to think of a river. When it’s flowing down a steep mountainside, it flows fast and straight,” says Francis. “When it gets to the coastal plain where there’s little slope to the land, it flows slowly and is easily deflected from its path.”
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