逆行涌浪引起的风浪谱的变化──Ⅰ.实验研究
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摘要: 60年代初,Longuet-Higgins和Stewart[1]完成的理论工作揭示了一个有趣的现象:当波长较短的重力波叠加在波长较长的重力波上时,短波的振幅在长波的波峰处达到最大,在长波的波谷处达到最小值.这是由两个原因造成的:一是在长波的波峰处出现几何上的辐合,另一是辐射应力的作功.
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