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平流层爆发性增温
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平流层爆发性增温
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平流层爆发性增温
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stratospheric sudden warming
平流层爆发性增温
北半球冬季平流层中出现的短时间内温度剧烈增加的现象。增温幅度可以达到十几甚至几十摄氏度。
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