实际观测资料表明，这一带潮流具有典型的往复流性质，并有较明显的不对称性和较大的垂直变化。
The actual data show that the tidal current is of typical alternating current with obvious asymmetry and large vertical variations.
实际观测资料表明，这一带潮流具有典型的往复流性质，并有较明显的不对称性和较大的垂直变化。
The actual data show that the tidal current is of typical alternating current with obvious asymmetry and large vertical variations.
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