STATISTICAL CHARACTERISTICS OF INERTIAL GRAVITY WAVES OBSERVED BY VHF RADAR IN THE POLAR MESOSPHERE
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摘要: 本文采用SOUSY VHF雷达1987年6月22日至6月29口在挪威Andya X690N,100E)的观测数据,研究中层惯性重力波传播的统计特征.21个周期为数小时的准单色波例子,在垂直方向上有确定的相位移动,表明它们是惯性内重力波.通过分析波相关水平扰动速度的矢端曲线,获得了水平传播矢量的大小和方向的分布,大多数(76%)波具有西向传播的波矢分量,似乎与中层顶具有强的西向背景风有关;水平传播速度的大小与中层高度上典型的观测值一致.本文分析结果还表明在极区中不仅存在向上的能量传输,也存在强烈的向下的能量传输.Abstract: This paper statistically investigates the propagation characteristics of inertial gravity waves in the mesorphere with VHF radar observations at Andφya(69°N, 10°E) Norway from June 22 to June 29 1987. It is found from the observations that 21 wave examples are of good monochromaticity and have certain certical progressions of phase.Their periods are severel home, indicating they are medal internal gravity waves. The distribution of horizontal wave vectors is extimated by analysing the hodographs of wave-asspcoated horizontal fluid velocity, most (76%) of them propagate westward, it seems to be related to the intense westward background wind at mesopause, The estimated horizontal wave vectors are the typical values observed in mesosphere. There are 15 (6) examples with downward (upward) phase progressions among the 21 examples. Their vertical wave lengths range from 5 to 9 km, wave-associated velocities are from 10 to 50m/s,indicating there exists not only upward but also intense downward wave energy flux in the polar mesosphere.
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