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Effects of rough sea-ice on the sound propagation in the Arctic ocean

机译:粗糙海冰对北冰洋声音传播的影响

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Aiming at the complex and variable environment of Arctic ice, a stochastic physical model of sea ice is proposed to better represent the roughness of sea ice and study the acoustic characteristics of typical Arctic ice. The sea-ice is regarded as the uniform elastomer with rough interface, and the randomly distributed protuberance on the lower layer of the sea-ice are ice ridges. Referring to the BT scattering model, the sea-ice thickness data measured by the up-looking sonar, which released from the National Snow and Ice Data Center. and the randomly distributed ice ridge is regarded as a randomly distributed isosceles triangle to establish a random sea ice physical model, combined with plane elasticity. The ice layer reflection model is used to obtain the ice layer reflection coefficient; The last year's data is used as the test group, and the rest as the training group, the ray theory model is used to calculate the propagation loss under the ice covered and compare them. The results show that there is scattering phenomenon when sound waves propagate under the rough ice interface. It is difficult to observe the sound shadow region under rough ice. Comparing the sound field under sea-ice between the training group and the test group, it is found that the sound transmission loss of the two groups is consistent on the whole. It indicates that the rough sea ice model proposed can better characterize the roughness of the interface under the real ice layer.
机译:旨在瞄准北极冰的复杂和可变环境,提出了一股随机物理模型的海冰,以更好地代表海冰的粗糙度,研究典型的北极冰的声学特征。海冰被视为具有粗糙接口的均匀弹性体,并且海冰下层的随机分布的突起是冰脊。参考BT散射模型,由悬挂声纳测量的海冰厚度数据,从国家雪和冰数据中心释放。随机分布的冰脊被认为是随机分布的等腰三角形,以建立随机海冰物理模型,与平面弹性相结合。冰层反射模型用于获得冰层反射系数;去年的数据用作测试组,其余的作为培训组,光线理论模型用于计算冰盖下的传播损失并比较它们。结果表明,当声波在粗糙的冰界面下传播时,存在散射现象。很难观察粗糙冰下的声音区域。比较培训组和测试组之间的海冰下的声场,发现两组的声音传输损失在整体上是一致的。它表明,所提出的粗糙海冰模型可以更好地表征真实冰层下界面的粗糙度。

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