北半球近90公里高度近夏季准2日波事件的全球研究

C.E. Meek , A.H. Manson , S.J. Franke , W. Singer , P. Hoffmann , R.R. Clark , T. Tsuda , T. Nakamura , M. Tsutsumi , M. Hagan , D.C. Fritts , J. Isler , Yu I. Portnyagin
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引用次数: 93

摘要

我们试图找到1992年夏季在海拔90公里附近观测到的一次引人注目的准2天波“事件”或“爆发”的北半球纬向波数。分析了来自9个雷达站的一组关于高层大气的独特数据(间隔~ 400 ~ ~ 12,000 km),并与模式的预期进行了比较。发现纬向波数m = 4的2天波相比较是决定性的。由于这里的站点只有很小的纬度分布(21°n到55°n),因此没有尝试确定确定经向波振幅结构的n。此外,振幅似乎是不稳定的,显示出某种调制,这不是同时在所有地点。最后,这些雷达在风速方面还没有相互“校准”。这种校准必须在相信波浪振幅的微小差异之前完成。还讨论了1991年的类似事件,但可用场址较少。这里m = 3和4之间的选择就不那么明确了。
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Global study of northern hemisphere quasi-2-day wave events in recent summers near 90 km altitude

We attempt to find the northern hemisphere zonal wavenumber for a striking quasi-2-day wave “event” or “burst” observed near 90 km altitude in the summer of 1992. A unique set of data on the upper atmosphere from nine radar sites is analysed (spacings ∼400– ∼ 12,000 km), and compared with expectations from models. The 2-day wave phase comparison, which finds zonal wavenumber m = 4, is conclusive. Determination of n, which defines the meridional wave amplitude structure, is not attempted, as the sites here have only a small latitude spread (21°N to 55°N). Also the amplitude seems to be unstable showing some sort of modulation which is not simultaneous at all sites. Finally, the radars have not been “calibrated” against each other in terms of wind speed. This calibration would have to be done before small differences in wave amplitude could be believed. A similar event in 1991 for which fewer sites are available is also discussed. Here the choice between m = 3 and 4 is not as clear.

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