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An Optical to IR Sky Brightness Model For the LSST

机译:LSST的光到IR天空亮度模型

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摘要

To optimize the observing strategy of a large survey such as the LSST, one needs an accurate model of the night sky emission spectrum across a range of atmospheric conditions and from the near-UV to the near-IR. We have used the ESO SkyCalc Sky Model Calculator to construct a library of template spectra for the Chilean night sky. The ESO model includes emission from the upper and lower atmosphere, scattered starlight, scattered moonlight, and zodiacal light. We have then extended the ESO templates with an empirical fit to the twilight sky emission as measured by a Canon all-sky camera installed at the LSST site. With the ESO templates and our twilight model we can quickly interpolate to any arbitrary sky position and date and return the full sky spectrum or surface brightness magnitudes in the LSST filter system. Comparing our model to all-sky observations, we find typical residual RMS values of ±0.2-0.3 magnitudes per square arcsecond.
机译:为了优化LSST等大型调查的观察策略,需要一种夜间天空发射光谱的精确模型,横跨一系列大气条件,从近UV到近IR。我们使用了ESO Skycalc Sky Model Calculator来构建智利夜空的模板谱图书馆。 ESO模型包括来自上层和下大气的排放,分散的星光,散落的月光和Zodiacal光。然后,我们已将ESO模板扩展到经验拟合在LSST网站上安装的佳能全天相机测量的暮光天空发射。通过ESO模板和我们的暮光模型,我们可以快速插入任何任意天空位置和日期,并在LSST过滤系统中返回全天谱或表面亮度大小。将我们的模型与全天候观测进行比较,我们发现典型的剩余RMS值为±0.2-0.3幅度弧形弧度。

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