不规则波浪作用下沿岸流的速度分布相对平缓。
The cross-shore profile of current velocity induced by irregular wave is smoother than the current induced by regular wave.
无论哪种方法，信号最终看到的都是看起来像不规则波浪形的波形曲线。
Either way, the signal ends up looking like an erratic wavelike squiggle.
EB模型则可用于求解广阔海域内非线性不规则波浪的运动和变形过程。
The EB model is applicable to nonlinear and irregular wave motion in large area.
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