涌浪是风浪离开风吹的区域后所形成的波浪。 另外，风速、风向等风要素的突变，也可能使风区内原来的风浪转变为涌浪。
随着你离碎浪越远，涌浪就不会那么大了，游起来就容易多了。
As you get further beyond the breakers, the swells are not nearly so large, so swimming becomes much easier.
数值计算结果表明，利用本文提出的方法计算台风涌浪能够很好地反映涌浪传播的物理特征，并具有一定的实用价值。
The results of computation show that the method could describe the main characteristics of swell propagation, and may be used in operation.
应用推荐