涌浪
简称涌。由产生风浪的海区传播到另一海区的波浪或风平息之后残留于海面的余浪。形状较风浪规则，呈对称波形，波顶平缓，周期长。涌浪在传播过程中波高逐渐降低，能量减少，波长变长，它往往比海上风暴移动得还要快。由于它传播距离较长，传播速度很快，每昼夜可传播1852千米(1000海里)。它常引起船舶的摇摆并对海岸建筑物有一定破坏作用。
Classification(s)
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Geographic semantic resource library Earth System(in Chinese) Marine geology
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| English |
|---|
| Name | swell |
| Chinese |
|---|
| Name | 涌浪 |
| Description | 简称涌。由产生风浪的海区传播到另一海区的波浪或风平息之后残留于海面的余浪。形状较风浪规则，呈对称波形，波顶平缓，周期长。涌浪在传播过程中波高逐渐降低，能量减少，波长变长，它往往比海上风暴移动得还要快。由于它传播距离较长，传播速度很快，每昼夜可传播1852千米(1000海里)。它常引起船舶的摇摆并对海岸建筑物有一定破坏作用。 |
{{htmlJSON.HowtoCite}}
NNU_Group (2011). 涌浪, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/b0efd481-9d36-4552-aedf-effb2c51cbca
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