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Variable anisotropy of small-scale stratospheric irregularities retrieved from stellar scintillation measurements by GOMOS/Envisat

机译:通过GOMOS / Envisat从恒星闪烁测量中获得的小尺度平流层不规则性的可变各向异性

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摘要

In this paper, we consider possibilities for studying the anisotropy of small-scale air density irregularities using satellite observations of bi-chromatic stellar scintillations during tangential occultations. Estimation of the anisotropy coefficient (the ratio of the characteristic horizontal to vertical scales) and other atmospheric parameters is based on the comparison of simulated/theoretical and experimental auto-spectra and coherency spectra of scintillation. Our analyses exploit a 3-D model of the spectrum of atmospheric inhomogeneities, which consists of anisotropic and isotropic components. For the anisotropic component, a spectral model with variable anisotropy is used. Using stellar scintillation measurements by GOMOS (Global Ozone Monitoring by Occultation of Stars) fast photometers, estimates of the anisotropy coefficient are obtained for atmospheric irregularities with vertical scales of 8-55 m at altitudes of 43-30 km. It is shown that the anisotropy increases from about 10 to 50 with increasing vertical scales.
机译:在本文中,我们考虑了使用双色恒星掩星过程中双色恒星闪烁的卫星观测研究小型空气密度不规则性的各向异性的可能性。各向异性系数(特征水平与垂直比例之比)和其他大气参数的估计是基于闪烁的模拟/理论和实验自动光谱以及相干光谱的比较。我们的分析利用了大气非均质性光谱的3-D模型,该模型由各向异性和各向同性成分组成。对于各向异性成分,使用具有可变各向异性的光谱模型。使用GOMOS(通过恒星掩星进行全球臭氧监测)快速光度计进行的恒星闪烁测量,可获得在43-30 km高度垂直尺度为8-55 m的大气不规则性的各向异性系数的估计值。结果表明,各向异性随着垂直尺度的增加而从大约10增加到50。

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