首页> 外文会议>Conference on ground-based and airborne instrumentation for astronomy >Characterizing near-infrared sky brightness in the Canadian high arctic
【24h】

Characterizing near-infrared sky brightness in the Canadian high arctic

机译:在加拿大高北极的近红外天空亮度表征近红外天空亮度

获取原文

摘要

We present the first measurements of the near-infrared (NIR), specifically the J-band, sky background in the Canadian High Arctic. There has been considerable recent interest in the development of an astronomical observatory in Ellesmere Island; initial site testing has shown promise for a world-class site. Encouragement for our study came from sky background measurements on the high Antarctic glacial plateau in winter that showed markedly lower NIR emission when compared to good mid-latitude astronomical sites due to reduced emission from the Meinel bands, i.e. hydroxyl radical (OH) airglow lines. This is possibly a Polar effect and may also be present in the High Arctic. To test this hypothesis, we carried out an experiment which measured the the J-band sky brightness in the High Arctic during winter. We constructed a zenith-pointing, J-band photometer, and installed it at the Polar Environment Atmospheric Research Laboratory (PEARL) near Eureka, Nunavut (latitude: 80° N). We present the design of our ruggedized photometer and our results from our short PEARL observing campaign in February 2012. Taken over a period of four days, our measurements indicate that theJ-band sky brightness varies between 15.5-15.9 mag arcsecsup2/sup; with a measurement uncertainty of 0.15 mag. Theuncertainty is entirely dominated by systematic errors present in our radiometric calibration. On our best night, we measured a fairly consistent sky brightness of 15.8 ± 0.15 mag arcsecsup2/sup. This is not corrected for atmospheric extinction, which is typically & 0.1 mag in the J-band on a good night. The measured sky brightness iscomparable to an excellent mid-latitude site, but is not as dark as claimed by the Antarctic measurements. Wediscuss possible explanations of why we do not see as dark skies as in the Antarctic. Future winter-long skybrightness measurements are anticipated to obtain the necessary statistics to make a proper comparison withthe Antarctic measurements.© (2012) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
机译:我们介绍了近红外(NIR)的第一次测量,特别是J频段,在加拿大高北极的天空背景。最近近来兴趣在Ellesmere Island的天文天文台的发展中兴趣;初始站点测试显示了世界级网站的承诺。对我们研究的鼓励来自天空背景测量在冬季高南极冰川高原上,由于来自Meinel带的发射减少,即羟基纬度,即羟基自由基(OH)释放线。这可能是极性效果,也可能存在于高北极中。为了测试这一假设,我们进行了一个实验,该实验在冬季测量了高北极的J频段天空亮度。我们构建了一个Zenith指向的J频带光度计,并在Eureka,Nunavut(纬度:80&Deg; N)附近的极地环境大气研究实验室(珍珠)。我们展示了我们坚固耐用的光度计的设计以及我们2012年2月的短珍珠观察活动的结果。我们的测量结果表明,我们的测量结果表明,频带天空亮度在15.5-15.9 mag arcsec 2之间变化。 / sup>;测量不确定性为0.15毫巴。 Theunctainty完全由我们的辐射校准中存在的系统错误主导。在我们最好的夜晚,我们测量了一个相当一致的天空亮度为15.8&Plymn; 0.15 mag arcsec 2 。这不是纠正大气消光,这通常是&在一个晚安的J频段中0.1 mag。测量的天空亮度可分散到优质的中纬度网站,但不如南极测量所要求的那样暗。 Wediscuss可能的解释为什么我们没有像南极一样看到黑暗的天空。预计未来的冬季长度测量会获得必要的统计数据,以与南极测量进行适当的比较。©(2012)照片光学仪表工程师(SPIE)的版权协会。仅供个人使用的摘要下载。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号