胶州湾属基岩海湾型潮汐通道，湾口内、外发育较为典型的涨、落潮流三角洲，地貌体系较为完整。
The Jiaozhou bay is a tidal inlet of bedrock bay type, the typical flood and ebb tidal deltas are developed inside and outside the bay mouth, and the geomorphologic system in the bay is complete.
由于水流的非正向入射，潮汐通道地貌体系不对称，潮流三角洲在湾内东侧发育、在湾外东北侧发育。
The obliquely inflowing current forms an asymmetric geomorphologic system in the tidal inlet, the tidal deltas are more developed on the east side of inner bay and on the northeast side of outer bay.
由于水流的非正向入射，潮汐通道地貌体系不对称，潮流三角洲在湾内东侧发育、在湾外东北侧发育。
The obliquely inflowing current forms an asymmetric geomorphologic system in the tidal inlet, the tidal deltas are more developed on the east side of inner bay and on the northeast side of outer bay.
应用推荐