激浪带
又称破浪带(breaker zone)。自波浪开始变形产生破浪的地点到岸边之间的地带。其宽度受水下岸坡坡度的制约，通常在100～200米之间，坡降平缓的海底则可达数百米。在激浪带由于激浪反作用常形成沿岸沙堤。
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contributed at 2011-10-13
Classification(s)
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Earth System(in Chinese) Marine geology
Detailed Description
| English |
|---|
| Name | surf zone |
| Chinese |
|---|
| Name | 激浪带 |
| Description | 又称破浪带(breaker zone)。自波浪开始变形产生破浪的地点到岸边之间的地带。其宽度受水下岸坡坡度的制约，通常在100～200米之间，坡降平缓的海底则可达数百米。在激浪带由于激浪反作用常形成沿岸沙堤。 |
How to Cite
NNU_Group (2011). 激浪带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/462c37d9-be13-45c8-8264-007c140cd80e
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