Last Updated：2025/11/25
Caballing in the high-latitude seas can cause denser water parcels to form and sink, influencing deep ocean circulation.
See correct answer
Caballing in the high-latitude seas can cause denser water parcels to form and sink, influencing deep ocean circulation.
音声機能が動作しない場合はこちらをご確認ください
Edit Histories（0）
