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Spectral analysis of gravity wave activity in SABER temperature data

机译:SABER温度数据中重力波活动的频谱分析

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[1] Since January 2002, the SABER (Sounding of the Atmosphere using Broadband Emission Radiometry) instrument has performed continuous measurements from near the tropopause into the thermosphere. For the time period 29 January 2002-31 January 2006, we spectrally analyzed time series of weekly zonal root mean square gravity wave (GW) amplitudes for systematic intra-annual, annual and inter-annual GW activity. GWs considered have horizontal wavelengths between 100 km and zonal wave number 6 and vertical wavelengths between 5-30 km. Height-latitude cross sections of spectral amplitudes and phases between 20 100 km and 55 degrees S-55 degrees N show several relevant oscillations. A strong semiannual variation is evident in the high-latitude upper stratosphere/mesosphere. Annual components reveal two isolated maxima at mid-latitudes in both hemispheres, associated with the winter polar vortices, and summertime maxima in the subtropics. Biennial amplitudes in the equatorial stratosphere coincide with the descending westerly shear phase and can be attributed to the quasi-biennial oscillation.
机译:[1]自2002年1月以来,SABER(使用宽带放射辐射测量法测大气)已从对流层顶附近进入热圈进行了连续测量。在2002年1月29日至2006年1月31日期间,我们对每周的纬向均方根重力波(GW)振幅的时间序列进行了频谱分析,以进行系统的年内,年度和年际GW活动。所考虑的GW的水平波长在100 km和6号纬向波之间,而垂直波长在5-30 km之间。光谱幅度和相位在20100 km和55度S-55度N之间的高纬度横截面显示出几个相关的振荡。在高纬度平流层/中流层,很明显半年度变化明显。年分量揭示了两个半球中纬度的两个孤立的最大值,与冬季的极地涡旋和亚热带的夏季最大值有关。赤道平流层中的每两年一次振幅与下降的西风切变相一致,并且可以归因于准每两年一次的振荡。

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