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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Characteristics of inertia gravity waves over the South Pacific as revealed by radiosonde observations
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Characteristics of inertia gravity waves over the South Pacific as revealed by radiosonde observations

机译:惯性重力波的特征南太平洋所揭示的无线电探空仪观察

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Using horizontal wind and temperature data with fine vertical resolution obtained by radiosondes, we investigate the characteristics of parameters and propagation properties of inertia gravity waves in the upper troposphere and lower stratosphere in the subtropics and extratropics over the South Pacific where very few observations have so far been done. Components extracted by a band-pass filter having cutoff vertical wavelengths of 0.5 and 5 km are analyzed as gravity waves. Gravity wave parameters such as intrinsic frequency , vertical and horizontal wavelengths, and phase and group velocities are estimated by hodograph analysis. The statistics on such parameters are presented for both the stratosphere and troposphere for the three latitudinal ranges 17°–24°S, 25°–33°S, and 34°–48°S. The horizontal wavelengths decrease and increases with increasing latitude south. The dominant values for the Coriolis parameter f divided by are ~0.5 in the lower stratosphere and ~0.3 in the troposphere, with little dependence on latitude. The dominant vertical wavelengths for upward propagating waves are longer in the troposphere than in the lower stratosphere. The most dominant direction of horizontal propagation is southward, with a little bias toward southeastward. A case study using ray tracing suggests that the major source of such southeastward waves is located in the upper troposphere. Notable northward propagation of gravity waves is also found in the subtropical lower stratosphere. The source of the gravity waves is considered to be a cutoff cyclone developing in the upper troposphere.
机译:使用卧式风力和温度数据无线电探空仪获得的垂直分辨率,我们调查的特征参数惯性重力和传播属性波在对流层上部和更低的亚热带和extratropics平流层在南太平洋的地方很少观察到目前为止完成了。提取一个带通滤波器截止分析了垂直波长的0.5和5公里重力波。固有频率,垂直和水平波长,相位和群速度估计速度图分析。等参数的介绍平流层和对流层的三人纬度的范围17°-24°S, 25°-33°S34°-48°S。随着纬度的增加而增加。占主导地位的科里奥利参数f的值除以0.5 ~平流层底部~ 0.3的对流层,很少依赖在纬度上。上行传播波更长时间比低平流层对流层。最具优势的水平传播的方向向南,有点偏见偏西风为主。表明这样的主要来源偏西风为主波位于上层对流层。重力波也在亚热带低平流层。波被认为是截止气旋发展上对流层。

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