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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Small-scale gravity waves near the mesopause observed by four all-sky airglow imagers
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Small-scale gravity waves near the mesopause observed by four all-sky airglow imagers

机译:四个全天空气辉成像仪观测到的中绝经附近的小重力波

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Nocturnal airglow images obtained at the Shigaraki middle and upper atmosphere (MU) observatory (34.9 degreesN, 136.1 degreesE), Japan, were analyzed to study the three-dimensional structure of small-scale gravity waves in the mesopause region. Airglow images from the near-infrared OH (layer height of similar to 86 km) and O-2(0,1) (similar to 94 kin) bands and the visible O I (similar to 96 km) and Na (similar to 90 kin) lines were obtained simultaneously by using four all-sky cooled charge-coupled device imagers with a high time resolution of 0.5-2.0 min. A clear wave packet (horizontal wavelength of 60-70 km) propagating downward was observed for 2000-2030 LT on January 28, 1998. The downward motion of the wave packet is identified from a comparison of the edge location of the packet at the four airglow layers. The observed waves became faint first in 0 1 (the highest altitude) and last in Off (the lower altitude), suggesting also that the wave packet passed through each of the airglow layers downward. From the simultaneous wind observation by the MU radar, we conclude that the observed downward propagating wave packet was generated by wave reflection at higher altitudes in the background wind field that was opposite to the horizontal k vector of the waves. For the same event, we estimate the vertical wavelength of the waves to be similar to5 kin or 20-30 km by comparing the. wave phases observed in the four airglow layers. The vertical wavelengths estimated from the dispersion relation are consistent with the latter value. [References: 16]
机译:分析了在日本Shigaraki中高空观测站(北纬34.9度,东经136.1度)获得的夜间气辉影像,研究了更年期地区小尺度重力波的三维结构。来自近红外OH(层高类似于86 km)和O-2(0,1)(类似于94 kin)波段以及可见OI(类似于96 km)和Na(类似于90 kin)的气辉图像)线是通过使用四台全天空冷却的电荷耦合器件成像仪同时获得的,它们的时间分辨率为0.5-2.0分钟。 1998年1月28日在2000-2030 LT处观察到一个向下传播的透明波包(水平波长60-70 km)。通过比较四个波包的边缘位置可以确定波包的向下运动气辉层。观测到的波首先在0 1(最高高度)变得微弱,最后在Off(较低高度)变得微弱,这也表明波包向下穿过每个气辉层。从MU雷达同时进行的风观测中,我们得出结论,观测到的向下传播的波包是由背景风场中与波的水平k矢量相反的更高高度处的波反射产生的。对于同一事件,通过比较,我们估计波的垂直波长类似于5 kin或20-30 km。在四个气辉层中观察到波浪相。从色散关系估计的垂直波长与后一个值一致。 [参考:16]

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