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涨潮流
flood current
- 涨潮流的流速和历时皆大于落潮流。
Both the velocity and duration of the flood are larger than those of the ebb. - 涨潮流、向陆的密度流和混合是产生盐水入侵的动力因子。
The dynamic factors of saltwater intrusion are the tidal flood current, land - ward density current and mixing. - 该体系包括大沽河-洋河潮控三角洲和与狭口海湾密切相关的涨、落潮流三角洲，潮流作用在各三角洲的形成过程中为主要的沉积动力。
The Dagu-Yanghe tidal delta, a facies system, is formed on the west side of Jiaozhou bay, where the river mouth bar and interdistributory bay are the major sub-facies.
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