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Analysis of Characteristics of Sound Propagation in Antarctic Ocean by Parabolic Equation Method

机译:抛物线方程法分析南极海洋声音传播特征

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Recently, the climate research of Ocean using Autonomous Underwater Vogel (AUV) is being planned in the Antarctic Ocean. In order to understand the characteristics of sound propagation in the Antarctic Ocean for communicate to AUV, we were calculated propagation time of pulse used by ray theory. Sound velocity profile was calculated from Japanese Antarctic Research Expedition (JARE-31) in 1991. It was assumed that the transmitter was placed at 100 m in depth and propagation range was 33 km in OW traverse line. We have investigated about the influence of bathymetry in Lutzow-Holm bay for sound propagation in the Antarctic Ocean model that covered ice layer on surface for 33 km in range. The sound propagation time in OW line changed as the increment of roughness of ice surface and bathymetry. In order to know the characteristics of sound propagation, we calculated pulse waveform using parabolic equation method.
机译:最近,在南极海洋中计划使用自主水下Vogel(AUV)海洋的气候研究。为了了解南极海洋中声音传播的特征,用于与AUV进行通信,我们计算了光线理论使用的脉冲的传播时间。 1991年的日本南极研究探险(JARE-31)计算了声速简档。假设发射器在100米处放置在深度100米处,传播范围为33公里,横向线33公里。我们研究了Zhymetry在Lutzow-Holm湾的影响,在南极海洋模型中进行声音传播,在覆盖表面上的冰层33公里范围内。 OW线的声音传播时间随着冰面和沐浴粗糙度的增量而变化。为了了解声音传播的特征,我们使用抛物线方程方法计算脉冲波形。

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