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Retrieval of vertical profiles of atmospheric refraction angles by inversion of optical dilution measurements

机译:通过反演光学稀释度测量反演大气折射角的垂直剖面

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In this paper, we consider occultations of celestial bodies through the atmospheric limb from low Earth orbit satellites and we show how the usual change of tangent altitude associated with atmospheric refraction is inseparably connected to a variation of the observed apparent intensity, for extended and pointlike sources. We demonstrate, in the regime of weak refraction angles, that atmospheric optical dilution and image deformation are strictly concomitant. The approach leads to the integration of a simple differential equation related to the observed transmittance in the absence of other absorbing molecules along the optical path. The algorithm does not rely on the absolute knowledge of the radiometer pointing angle that is related to the accurate knowledge of the satellite attitude. We successfully applied the proposed method to the measurements performed by two past occultation experiments: GOMOS for stellar and ORA for solar occultations. The developed algorithm (named ARID) will be applied to the imaging of solar occultations in a forthcoming pico-satellite mission.
机译:在本文中,我们考虑了来自低地球轨道卫星的大气肢体对天体的掩盖,并且我们展示了与大气折射相关的通常的切线高度变化与观测到的视在强度的变化密不可分的联系,对于扩展和点状源。我们证明,在弱折射角的情况下,大气光学稀释和图像变形是严格伴随的。该方法导致与沿光路不存在其他吸收分子的情况下所观察到的透射率有关的简单微分方程的积分。该算法不依赖于辐射计指向角的绝对知识,后者与卫星姿态的准确知识有关。我们成功地将提出的方法应用于过去两次掩星实验的测量:GOMOS用于恒星,ORA用于太阳掩星。这项开发的算法(名为ARID)将应用于即将进行的微卫星任务中太阳掩星的成像。

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