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The first simultaneous spectroscopic and monochromatic imaging observations of short-wavelength infrared aurora of $$\mathrm {N_{2}^{+}}$$ N 2 + Meinel (0,0) band at 1.1 $$\mathrm {\mu }$$ μ m with incoherent scatter radar

Authors :
Takanori Nishiyama
Masato Kagitani
Senri Furutachi
Yuki Iwasa
Yasunobu Ogawa
Takuo T. Tsuda
Peter Dalin
Fuminori Tsuchiya
Satonori Nozawa
Fred Sigernes
Source :
Earth, Planets and Space, Vol 76, Iss 1, Pp 1-9 (2024)
Publication Year :
2024
Publisher :
SpringerOpen, 2024.

Abstract

Abstract This study presents a first simultaneous observation of $$\mathrm {N_{2}^{+}}$$ N 2 + Meinel (0,0) band (hereafter, $$\mathrm {N_{2}^{+}}$$ N 2 + (M)) aurora by cutting-edge short-wavelength infrared imaging spectrograph (NIRAS-2) and monochromatic camera (NIRAC) installed at the Kjell Henriksen Observatory (78 $$^\circ$$ ∘ N, 16 $$^\circ$$ ∘ E). On January 21 2023, $$\mathrm {N_{2}^{+}}$$ N 2 + (M) intensification that is associated with a band-shape aurora structure was observed by the NIRAS-2 and the NIRAC having temporal resolutions of 30 s and 20 s, respectively. In addition, the European incoherent scatter Svalbard Radar also observed electron density variations at the same time. Electron density measured at altitude range from 100 km 120 km shows similar variations as of $$\mathrm {N_{2}^{+}}$$ N 2 + (M) intensity, which implies that a primary source of $$\mathrm {N_{2}^{+}}$$ N 2 + (M) emissions is direct collisions of $$\mathrm {N_{2}}$$ N 2 by precipitating electrons penetrating down to around 100 km altitude (up to 10 keV). However, the observation also demonstrated moderate correlations between $$\mathrm {N_{2}^{+}}$$ N 2 + (M) intensity and electron density above 140 km, which implies that different $$\mathrm {N_{2}^{+}}$$ N 2 + (M) generation process, $$\mathrm {N_2}$$ N 2 charge exchange with $$\mathrm {O^{+}}$$ O + , may work up to near 160 km and make a non-negligible contribution to $$\mathrm {N_{2}^{+}}$$ N 2 + (M) emissions. This hypothesis would be verified with further radar observations or stereo imaging observations useful to estimate the vertical distribution of the emission layers. The $$\mathrm {N_{2}^{+}}$$ N 2 + (M) is a very promising target wavelength for aurora observation because the quality of sensors is highly expected to improve further and further. Continuous observations with our new instruments will undoubtedly provide an important information of $$\mathrm {N_{2}^{+}}$$ N 2 + (M) characteristics, for future missions of both balloon-borne and satellite-borne imaging. Graphical Abstract

Details

Language :
English
ISSN :
18805981
Volume :
76
Issue :
1
Database :
Directory of Open Access Journals
Journal :
Earth, Planets and Space
Publication Type :
Academic Journal
Accession number :
edsdoj.2dd7d8c20b0d4324893da652d3f506fb
Document Type :
article
Full Text :
https://doi.org/10.1186/s40623-024-01969-x