能量显著集中在岸边的沿岸传播的频率高于惯性频率的波动。
对地平直海岸和二维大陆架,自由边缘波的振幅远小于强迫波的振幅。
The amplitude of edge waves is much smaller than that of forcing waves in the case of straight coastline and two-dimensional shelf topography.
请参见二级系统准确预报轧制力的意义中引起中心扣和边缘波的讨论。
See the discussion on the cause center buckle and edge wave in the Significance of Accurate Level 2 Force Prediction section.
在斜坡地形上,两个波数相近、波向不同的自由波还会激发出边缘波。
On the topography with a slope, two free waves with closing wave numbers and different directions can trigger edge waves.
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