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Towards a reliability assessment of the Cn2 and wind speed vertical profiles retrieved from GeMS

机译:对Cn2和风速垂直的可靠性评估   从Gems检索的配置文件

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摘要

The advent of a new generation of Adaptive Optics systems called Wide FieldAO (WFAO) mark the beginning of a new era. By using multiple Guide Stars (GSs),either Laser Guide Stars (LGSs) or Natural Guide Stars (NGSs), WFAOsignificantly increases the field of view of the AO-corrected images, and thefraction of the sky that can benefit from such correction. Different typologiesof WFAO have been studied over the past years. They all require multiple GSs toperform a tomographic analysis of the atmospheric turbulence. One of thefundamental aspects of the new WFAO systems is the knowledge of thespatio-temporal distribution of the turbulence above the telescope. One way toget to this information is to use the telemetry data provided by the WFAOsystem itself. Indeed, it has been demonstrated that WFAO systems allows one toderive the Cn2 and wind profile in the main turbulence layers (see e.g. Corteset al. 2012). This method has the evident advantage to provide information onthe turbulence stratification that effectively affects the AO system, propertymore difficultly respected by independently vertical profilers. In this paper,we compare the wind speeds profiles of GeMS with those predicted by anon-hydrostatical mesoscale atmospherical model (Meso-NH). It has been proved(Masciadri et al., 2013), indeed, that this model is able to provide reliablewind speed profiles on the whole troposphere and stratosphere (up to 20-25 km)above top-level astronomical sites. Correlation with measurements revealed tobe very satisfactory when the model performances are analyzed from astatistical point of view as well on individual nights. Such a system appearstherefore as an interesting reference to be used to quantify the GeMS windspeed profiles reliability.
机译:称为宽场AO(WFAO)的新一代自适应光学系统的问世标志着新时代的开始。通过使用多个制导星(GSs),激光制导星(LGS)或自然制导星(NGS),WFAO可以显着增加AO校正图像的视场,并可以从这种校正中受益。过去几年来研究了WFAO的不同类型。它们都需要多个GS来对大气湍流进行层析成像分析。新WFAO系统的基本方面之一是了解望远镜上方湍流的时空分布。获取此信息的一种方法是使用WFAO系统本身提供的遥测数据。确实,已经证明WFAO系统可以在主要湍流层中推导Cn2和风廓线(参见例如Corteset等人2012)。这种方法具有明显的优势,可以提供有效影响AO系统的湍流分层信息,而独立的垂直剖面仪更难以尊重其特性。在本文中,我们将GeMS的风速分布与通过非静水中尺度大气模型(Meso-NH)预测的风速分布进行了比较。事实证明(Masciadri et al。,2013),该模型能够在高层天文站点上方的整个对流层和平流层(最远20-25 km)提供可靠的风速剖面。从统计学的角度分析模型性能以及在各个晚上,与测量的相关性都显示出非常令人满意的效果。因此,这样的系统似乎是用于量化GeMS风速剖面可靠性的有趣参考。

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