首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Annual and Semiannual Oscillations of Thermospheric Composition in TIMED/GUVI Limb Measurements
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Annual and Semiannual Oscillations of Thermospheric Composition in TIMED/GUVI Limb Measurements

机译:年度和半年度的振荡Thermospheric成分在定时/ GUVI肢体测量

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The Global UltraViolet Imager (GUVI) onboard the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) satellite provides a data set of vertical thermospheric composition (O, N_2, and O_2 densities) and temperature profiles from 2002-2007. Even though GUVI sampling is limited by orbital constraint, we demonstrated that the GUVI data set can be used to derive the altitude profiles of the amplitudes and phases of annual oscillation (AO) and semiannual oscillation (SAO), thereby providing important constraints on models seeking to explain these features. We performed a seasonal and interannual analysis of GUVI limb O, O_2, and N_2 densities and volume number density ratio O/N_2 at constant pressure levels. These daytime observations of O and O/N_2 in the lower thermosphere show a strong AO at midlatitudes and a clear SAO at lower latitudes. The global mean GUVI O/N_2 number density ratio shows the AO, with slightly larger values in January than in July and a SAO with O/N_2 greater during equinoxes than at the solstices. O and N_2 densities on fixed pressure levels in the upper thermosphere are anticorrelated with solar extreme ultraviolet flux. On the other hand, O/N_2 is smaller during solar minimum and larger during solar maximum. The thermospheric AO and SAO in composition have a constant phase with altitude throughout the thermosphere.
机译:全球紫外成像仪(GUVI)上热大气层电离层中间层能量动力学(定时)卫星提供的数据集垂直thermospheric成分(O、甲烷、和提取成分密度)和温度资料2002 - 2007。通过轨道约束,我们证明了GUVI数据集可用于推导出高度年度的资料的振幅和阶段振荡(AO)和半年度振荡(圣),从而提供重要的限制模型试图解释这些特性。表现的年际和季节变化分析GUVI肢体O、成分和甲烷、密度和体积数密度比O /甲烷在恒定的压力的水平。在热电离层显示强大的AO越低情理之中,一个明确的圣在低纬度地区。全球平均GUVI O /甲烷、数密度比显示了AO,略大的值比7月和1月与O /甲烷、圣大在春分和秋分比二至点。密度在上部固定压力水平热电离层anticorrelated太阳能极端的紫外线通量。O /甲烷在太阳和小大在太阳能最大。巴西在作文有一个恒定的阶段在整个热电离层高度。

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