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首页> 外文期刊>Geophysical Research Letters >A case study of mesospheric gravity wave momentum flux and dynamical instability using the Arecibo dual beam incoherent scatter radar
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A case study of mesospheric gravity wave momentum flux and dynamical instability using the Arecibo dual beam incoherent scatter radar

机译:使用Arecibo双波束非相干散射雷达进行中层重力波动量通量和动力学不稳定性的案例研究

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We report the first observation of gravity wave momentum flux in the mesosphere using the dual-beam Arecibo incoherent scatter radar (ISR). Quasi-monochromatic waves were observed throughout the daytime of July 28, 2001 in the altitude range of 65 - 85 km. The largest wave speed was about 100 m/s and the dominant period was about 15 min. Instability, as indicated by the Richardson number, occurred at several altitudes, most dramatically at 77 and 81 kilometers. The zonal momentum flux is found to change sign at altitudes where dynamical instability occurs. No significant gravity waves were observed in the region having an eastward background wind, while they were ubiquitous when the background wind was westward.
机译:我们报告了使用双光束Arecibo非相干散射雷达(ISR)对中层重力波动量通量进行的首次观测。在2001年7月28日的整个白天,在65-85公里的高度范围内观察到准单色波。最大波速约为100 m / s,主导周期约为15分钟。理查森数字表明,不稳定发生在几个海拔高度,最明显的是在77公里和81公里处。发现在发生动力不稳定的海拔高度处,动量通量会改变符号。在背景风向东的区域中没有观察到明显的重力波,而背景风向西时则无处不在。

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