Last Updated:2025/12/01

A sudden stratospheric warming can disrupt the polar vortex and trigger prolonged cold spells at the surface.

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A sudden stratospheric warming can disrupt the polar vortex and trigger prolonged cold spells at the surface.

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突発的成層圏暖化は極渦を崩壊させ、成層圏の気温が約50ケルビン上昇することで上層大気の循環を乱し、地表で長期にわたる寒波を引き起こすことがある。

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