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首页> 外文期刊>EPJ Web of Conferences >The Innsbruck/ESO sky models and telluric correction tools - The possibility of atmospheric monitoring for ?erenkov telescopes
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The Innsbruck/ESO sky models and telluric correction tools - The possibility of atmospheric monitoring for ?erenkov telescopes

机译:因斯布鲁克/ ESO天空模型和碲校正工具-费伦科夫望远镜进行大气监测的可能性

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摘要

Ground-based astronomical observations are influenced by scattering and absorption by molecules and aerosols in the Earth's atmosphere. They are additionally affected by background emission from scattered moonlight, zodiacal light, scattered starlight, the atmosphere, and the telescope. These influences vary with environmental parameters like temperature, humidity, and chemical composition. Nowadays, this is corrected during data processing, mainly using semi-empirical methods and calibration by known sources. Part of the Austrian ESO in-kind contribution was a new model of the sky background, which is more complete and comprehensive than previous models.While the ground based astronomical observatories just have to correct for the line-of-sight integral of these effects, the ?erenkov telescopes use the atmosphere as the primary detector. The measured radiation originates at lower altitudes and does not pass through the entire atmosphere. Thus, a decent knowledge of the profile of the atmosphere at any time is required. The latter cannot be achieved by photometric measurements of stellar sources. We show here the capabilities of our sky background model and data reduction tools for ground-based optical/infrared telescopes. Furthermore, we discuss the feasibility of monitoring the atmosphere above any observing site, and thus, the possible application of the method for ?erenkov telescopes.* Based on ESO archival data and observations obtained in programme ID 491.L-0659 at ESO VLT.
机译:地面天文观测受到地球大气中分子和气溶胶的散射和吸收的影响。此外,它们还受到散射的月光,黄道带的光,散射的星光,大气和望远镜的背景发射的影响。这些影响会随环境参数(例如温度,湿度和化学成分)而变化。如今,这在数据处理过程中已得到纠正,主要是使用半经验方法并通过已知来源进行校准。奥地利ESO实物捐助的一部分是一种新的天空背景模型,该模型比以前的模型更完整,更全面。虽然地面天文观测台只需要校正这些影响的视线积分,菲伦科夫望远镜使用大气作为主要探测器。测得的辐射起源于较低的高度,并没有穿过整个大气层。因此,在任何时候都需要对大气状况的体面知识。后者不能通过对恒星源进行光度测量来实现。我们在这里展示了用于地面光学/红外望远镜的天空背景模型和数据缩减工具的功能。此外,我们讨论了在任何观测点上方监视大气的可行性,以及由此而提出的费伦科夫望远镜方法的可能应用。*基于ESO档案数据和ESO VLT程序ID 491.L-0659中获得的观测结果。

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