地轉流(geostrophic current) 是一種平行等壓線的海洋流,是經由海水密度梯度所產生的壓強梯度力與科里奧利力平衡時的海流。[1]
此條目可參照英語維基百科相應條目來擴充。 (2021年10月20日) |
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