Last Updated：2025/11/24
Baroclinicity in the mid-latitude atmosphere often leads to the development of strong frontal systems and cyclones.
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Baroclinicity in the mid-latitude atmosphere often leads to the development of strong frontal systems and cyclones.
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中緯度大気における斜圧性の存在は、しばしば発達した前線系や低気圧の形成をもたらす。
