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An Optical to IR Sky Brightness Model For the LSST

机译:LSST的光学到红外天空亮度模型

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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:为了优化诸如LSST之类的大型勘测的观测策略,需要一个准确的模型,该模型涵盖从近紫外到近红外的各种大气条件下的夜空发射光谱。我们已经使用ESO SkyCalc天空模型计算器构建了智利夜空的模板光谱库。 ESO模型包括来自上层和下层大气的发射,散射的星光,散射的月光和黄道光。然后,我们通过安装在LSST站点上的佳能全天候摄像机测量的ESO模板扩展了经验性拟合,以适应黄昏的天空。使用ESO模板和我们的暮光模型,我们可以快速插值到任意天空位置和日期,并在LSST过滤器系统中返回完整的天空光谱或表面亮度幅度。将我们的模型与全天候观测的结果进行比较,我们发现典型的残余RMS值为每平方弧秒±0.2-0.3个量级。

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