浅海潮
或称浅水潮波。发生在河口海岸浅海地区的潮汐。日、月等在大洋中引起的源潮波，通过波动的形式向外传播，到达浅水区或近岸后，由于水深渐小，能量集中，海底对海水的摩擦及波与波之间的相互作用而产生的非线性效应，使潮波发生畸变，从而又产生频率不同于源潮波的浅水潮波。
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contributed at 2011-12-26
Classification(s)
●
Earth System(in Chinese) Marine Geography
Detailed Description
| English |
|---|
| Name | shallow water tide |
| Chinese |
|---|
| Name | 浅海潮 |
| Description | 或称浅水潮波。发生在河口海岸浅海地区的潮汐。日、月等在大洋中引起的源潮波，通过波动的形式向外传播，到达浅水区或近岸后，由于水深渐小，能量集中，海底对海水的摩擦及波与波之间的相互作用而产生的非线性效应，使潮波发生畸变，从而又产生频率不同于源潮波的浅水潮波。 |
How to Cite
NNU_Group (2011). 浅海潮, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/859098fe-b3df-4f69-a1d2-177d197af6c4
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