论文标题
在分散介质中传播波数据包
Propagation of Wave Packets in Dispersive Media
论文作者
论文摘要
考虑了分散介质中波的传播和折射。一个主要目的是确定波折射为单色波的折射,而Snell定律具有相位速度或波数据包。波包的折射需要两个折射法。波数据包根据Snell定律的几何速度折射,而波数据包中的小波按照相位速度折射。测试是使用源自加勒比海,墨西哥湾,印度洋和南大洋的重力水波的定向功率谱进行的。在所有情况下,用压力传感器阵列测量了波。发现单色波的折射导致了从测量位点的回溯,该测量位点在不同的波周期内散布,并且没有回到共同的来源。当折射很大时,结果尤其不好。当使用数据测试波数据包的折射时,获得了非常好的结果。对于每一次风暴,考虑到不同波浪时期的回溯,回到了波浪产生区域。这些结果为在色散介质中的折射波提供了强有力的支持,而不是单色波。在对临界角的重力水波的受控波罐实验中也确定了波基的这一结果。还考虑并说明了传播波包的特性。发现并解释了反射点和临界角度。波数据包和单色波的传播之间可能存在主要差异。
The propagation and refraction of waves in dispersive media are considered. A primary objective is to determine whether waves refract as monochromatic waves by Snell's law with phase velocity or as wave packets. The refraction of wave packets requires two refraction laws. The wave packets refract according to Snell's law with the geometric group velocity while the wavelets within the wave packets refract according to Snell's law with phase velocity. The tests were performed using directional power spectra from gravity water waves originating in the Caribbean Sea, Gulf of Mexico, Indian Ocean, and the Southern Ocean. In all cases the waves were measured with arrays of pressure sensors. It was found that the refraction of monochromatic waves led to backtracks from a measurement site that spread out for the different wave periods and did not go back to a common source. When the refraction was large the results were especially bad. When the data were used to test the refraction of wave packets very good results were obtained. For every storm considered the backtracks of the different wave periods went back together to the wave generation area. These results offer strong support for refracting waves in dispersive media as wave packets, not as monochromatic waves. This result for wave groups was also determined in a controlled wave tank experiment of gravity water waves where a critical angle was tested. The properties of propagating wave packets are also considered and illustrated. Reflection points and critical angles are found and explained. There can be major differences between the propagation of wave packets and monochromatic waves.