论文标题

流动夜空亮度测量平流层

Optical night sky brightness measurements from the stratosphere

论文作者

Gill, Ajay, Benton, Steven J., Brown, Anthony M., Clark, Paul, Damaren, Christopher J., Eifler, Tim, Fraisse, Aurelien A., Galloway, Mathew N., Hartley, John W., Holder, Bradley, Huff, Eric M., Jauzac, Mathilde, Jones, William C., Lagattuta, David, Leung, Jason S. -Y, Li, Lun, Luu, Thuy Vy T., Massey, Richard J., McCleary, Jacqueline, Mullaney, James, Nagy, Johanna M., Netterfield, C. Barth, Redmond, Susan, Rhodes, Jason D., Romualdez, L. Javier, Schmoll, Jurgen, Shaaban, Mohamed M., Sirks, Ellen, Sivanandam, Suresh, Tam, Sut-Ieng

论文摘要

本文使用用超压气球传播成像望远镜(Superbit)拍摄的CCD图像对平流层进行了光学夜空亮度测量。用于估算背景的数据是在2016年,2018年和2019年的三次调试飞行中获得的,在海拔28公里至海平面以上34公里不等。为了有效比较平流层的亮度测量与山顶地面观测站的测量(在高银河系中最黑暗的月亮夜晚和高黄道纬度的最黑暗的夜晚进行的测量值),平流层亮度水平是Zodiacal Lights Lights Light and Diffuse paractic Light and paractic Light of Airglow and Airglow Brightness Projected to Zenith。平流层亮度分别在2016年,2018年和2019年的本地日出时间前约5.5小时,3小时和2小时测量。 2016年的$ b $,$ v $,$ r $和$ i $的亮度水平为2.7、1.0、1.1和0.6 mag arcsec $^{ - 2} $比最黑暗的基于地面的测量结果。 2018年的$ B $,$ V $和$ R $的亮度水平为1.3、1.0和1.3 mag arcsec $^{ - 2} $比最暗的基于地面的测量。 $ U $和$ i $ $ $的亮度水平比最黑暗的基于地面的测量值更明亮,而$ b $和$ v $亮度水平为0.8和0.6 mag arcsec $^{ - 2} $比最黑暗的基于地面的测量值更明亮。较低的天空亮度水平,稳定的光度法和较低的大气吸收使得从气球传播平台的平流层观测成为天文学的独特工具。我们计划在未来的中期长时间持续的气球飞行中继续这项工作。

This paper presents optical night sky brightness measurements from the stratosphere using CCD images taken with the Super-pressure Balloon-borne Imaging Telescope (SuperBIT). The data used for estimating the backgrounds were obtained during three commissioning flights in 2016, 2018, and 2019 at altitudes ranging from 28 km to 34 km above sea level. For a valid comparison of the brightness measurements from the stratosphere with measurements from mountain-top ground-based observatories (taken at zenith on the darkest moonless night at high Galactic and high ecliptic latitudes), the stratospheric brightness levels were zodiacal light and diffuse Galactic light subtracted, and the airglow brightness was projected to zenith. The stratospheric brightness was measured around 5.5 hours, 3 hours, and 2 hours before the local sunrise time in 2016, 2018, and 2019 respectively. The $B$, $V$, $R$, and $I$ brightness levels in 2016 were 2.7, 1.0, 1.1, and 0.6 mag arcsec$^{-2}$ darker than the darkest ground-based measurements. The $B$, $V$, and $R$ brightness levels in 2018 were 1.3, 1.0, and 1.3 mag arcsec$^{-2}$ darker than the darkest ground-based measurements. The $U$ and $I$ brightness levels in 2019 were 0.1 mag arcsec$^{-2}$ brighter than the darkest ground-based measurements, whereas the $B$ and $V$ brightness levels were 0.8 and 0.6 mag arcsec$^{-2}$ darker than the darkest ground-based measurements. The lower sky brightness levels, stable photometry, and lower atmospheric absorption make stratospheric observations from a balloon-borne platform a unique tool for astronomy. We plan to continue this work in a future mid-latitude long duration balloon flight with SuperBIT.

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