@article{86aba37ddac4437bb39377b5bb90bc48,
title = "Development of low-cost multi-wavelength imager system for studies of aurora and airglow",
abstract = "This paper introduces a new system that can monitor aurora and atmospheric airglow using a low-cost Watec monochromatic imager (WMI) equipped with a sensitive camera, a filter with high transmittance, and the non-telecentric optics. The WMI system with 486-nm, 558-nm, and 630-nm band-pass filters has observable luminosity of about ~200–4000 Rayleigh for 1.07-sec exposure time and about ~40–1200 Rayleigh for 4.27-sec exposure time, for example. It is demonstrated that the WMI system is capable of detecting 428-nm auroral intensities properly, through comparison with those measured with a collocated electron-multiplying charge-coupled device (EMCCD) imager system with narrower band-pass filter. The WMI system has two distinct advantages over the existing system: One makes it possible to reduce overall costs, and the other is that it enables the continuous observation even under twilight and moonlight conditions. Since 2013 a set of multi-wavelength WMIs has been operating in northern Scandinavia, Svalbard, and Antarctica to study meso- and large-scale aurora and airglow phenomena. Future development of the low-cost WMI system is expected to provide a great opportunity for constructing a global network for multi-wavelength aurora and airglow monitoring.",
keywords = "Airglow, Aurora, Imager, Polar ionosphere",
author = "Y. Ogawa and Y. Tanaka and A. Kadokura and K. Hosokawa and Y. Ebihara and T. Motoba and B. Gustavsson and U. Br{\"a}ndstr{\"o}m and Y. Sato and S. Oyama and M. Ozaki and T. Raita and F. Sigernes and S. Nozawa and K. Shiokawa and M. Kosch and K. Kauristie and C. Hall and S. Suzuki and Y. Miyoshi and A. Gerrard and H. Miyaoka and R. Fujii",
note = "Funding Information: We thank I. Sugita and Y. Kadowaki of the National Institute of Polar Research (NIPR), for their helpful support of the MWI data management and calibration. This research was financially supported by the Grants-in-Aid for Scientific Research S ( 15H05747 ), Scientific Research B ( 17H02968 ) and Scientific Research C ( 17K05672 ) by the Ministry of Education, Science, Sports and Culture, Japan . This work was also supported by ROIS-DS-JOINT ( 001RP2018 , and 019RP2018 ). The WMI system was calibrated at the calibration facility of NIPR, Japan. The production of this paper was supported by a NIPR publication subsidy. This work was partially carried out at the joint research workshop of the Institute for Space-Earth Environmental Research (ISEE), Nagoya University. Funding Information: We thank I. Sugita and Y. Kadowaki of the National Institute of Polar Research (NIPR), for their helpful support of the MWI data management and calibration. This research was financially supported by the Grants-in-Aid for Scientific Research S (15H05747), Scientific Research B (17H02968) and Scientific Research C (17K05672) by the Ministry of Education, Science, Sports and Culture, Japan. This work was also supported by ROIS-DS-JOINT (001RP2018, and 019RP2018). The WMI system was calibrated at the calibration facility of NIPR, Japan. The production of this paper was supported by a NIPR publication subsidy. This work was partially carried out at the joint research workshop of the Institute for Space-Earth Environmental Research (ISEE), Nagoya University. Publisher Copyright: {\textcopyright} 2019 Elsevier B.V. and NIPR",
year = "2020",
month = mar,
doi = "10.1016/j.polar.2019.100501",
language = "English",
volume = "23",
journal = "Polar Science",
issn = "1873-9652",
publisher = "Elsevier",
}