波浪壅水
亦称碎波拍。由于波列线性叠加所致的拍于碎波带附近而产生的长周期重力波。其周期范围是30~300s。此种海岸附近的长周期重力波，其形状与涌中波群的包络线很相近，并拍于碎波带附近产生，故称碎波拍。但也不一定需与波破碎或拍相联系。碎波拍与海岸附近的流和水位的研究有关。
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Contributor
contributed at 2011-12-26
Classification(s)
●
Earth System(in Chinese) Marine Geography
Detailed Description
| English |
|---|
| Name | surf beats |
| Chinese |
|---|
| Name | 波浪壅水 |
| Description | 亦称碎波拍。由于波列线性叠加所致的拍于碎波带附近而产生的长周期重力波。其周期范围是30~300s。此种海岸附近的长周期重力波，其形状与涌中波群的包络线很相近，并拍于碎波带附近产生，故称碎波拍。但也不一定需与波破碎或拍相联系。碎波拍与海岸附近的流和水位的研究有关。 |
How to Cite
NNU_Group (2011). 波浪壅水, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/2edb3bbe-3be2-4773-a72d-5718fb3b1a5f
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