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Analysis of the middle atmospheric ozone using SABER observations: a study over mid-latitudes in the northern and southern hemispheres

机译:使用Sabre观测的中间大气臭氧分析:北部和南半球中纬度的研究

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The present study focuses on the middle atmospheric ozone variability using 14 (2002-2015) years of Sounding of the Atmosphere using Broadband Emission Radiometry onboard Thermosphere Ionosphere Mesosphere Energetics and Dynamics satellite observations over the mid-latitude regions of northern and southern hemispheres. It is noted that ozone buildup starts late winter, and peaks during the springtime and gradually decreases in summer to autumn transitional period in both the hemispheres. The time series of ozone indicates the dominant annual and semi-annual oscillations in the middle atmosphere. The annual oscillation (AO) is found to be dominant over both the hemispheres, while the semi-annual oscillation (SAO) peaks at two different altitude regions: 30-60 km and 80-100 km. Further, the amplitude of AO is much significant than SSAO and MSAO. It is also noted another significant oscillation that peaks at 4 months in the altitude range 60-80 km. The strength of these oscillations at different sites is studied by comparing it with the zonal mean spectrum to assess the longitudinal asymmetry. It is found that the longitudinal asymmetry is more significant in the northern hemisphere than the southern hemisphere. This can be attributed to the differences in the land (elevated topographies in the northern hemisphere) and primarily ocean (in southern hemisphere) contrast that further contributes to the differences in the strength of the vertically propagating planetary-scale waves modulating the middle atmospheric ozone.
机译:本研究专注于使用宽带排放辐射测定的大气听起来的14(2002-2015)多年的中间大气臭氧变异性,使用宽带排放辐射测定船上热圈电离层肌间圈能量和动态卫星观察在北部和南半球的中纬区域。值得注意的是,臭氧的累积开始于冬季晚期,春季期间的峰值,夏季逐渐减少到两个半球中的秋季过渡时期。臭氧的时间序列表明中部大气中的主要年度和半年振荡。每年振荡(AO)被发现在半球上都是占主导地位的,而两个不同的海拔地区的半年振荡(SAO)峰值:30-60公里和80-100公里。此外,AO的幅度远远大于SSAO和MSAO。还有另一个显着的振荡,在海拔4个月内达到60-80公里。通过将其与分解平均光谱进行比较来评估纵向不对称的不同位点的这些振荡的强度。发现纵向不对称在北半球比南半球更重要。这可以归因于土地的差异(北半球的升高)和主要是海洋(南半球)对比,这进一步有助于垂直传播行星级波的强度的差异调节中间大气臭氧。

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