SELF-EXCITED OSCILLATIONS IN THE DRIFTING ICE COVER OF THE ARCTIC OCEAN

V. Smirnov, S. Kovalev, A. A. Nubom
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引用次数: 5

Abstract

During the monitoring of physical-mechanical state of the ice cover of the Arctic Ocean a wide spectrum of oscillation and wave processes was in the system ice-water studied. The investigations were carried out on the drifting stations “North Pole” with seismometers and tiltmeters. Vertical and horizontal displacements in the ice field characterize parameters of wave processes caused by compression and ridging of ice-mechanical self-excited oscillations. Mechanics of appearance and propagation of waves can be considered with an account of elastic-viscous properties of the ice cover. A phenomenological model is considered of appearance of periodic horizontal displacements on an extensive rupture in a continuous ice cover. At the fault of stresses on the rupture elastic horizontally polarized waves are emitted.
北冰洋漂流冰盖的自激振荡
在对北冰洋冰盖物理力学状态的监测中,研究了冰-水系统中广泛的振荡和波动过程。在“北极”漂流站用地震仪和倾斜仪进行了调查。冰场的垂直和水平位移表征了冰力学自激振荡压缩和脊化引起的波动过程参数。波的出现和传播力学可以用冰层的弹性-粘性特性来考虑。考虑了连续冰盖大面积破裂时周期性水平位移的现象模型。在破裂应力的断层处发出弹性水平极化波。
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