Photodetachment of electrons at sprite altitudes by visible and UV emissions of molecular nitrogen as a mechanism of initiation of sprite streamers
Abstract
Modeling [Qin et al., JGR, 116, A06305, 2011; GRL, 40, 4777, 2013; Nat. Comm., 5, 3740, 2014] and experimental [Lang et al., JGR, 116, A10306, 2011] findings indicate that the presence of plasma irregularities is a necessary condition for the initiation of sprite streamers. Sprite streamers are often preceded by a relatively low intensity diffuse glow discharge referred to as sprite halo [Barrington-Leigh et al., JGR, 106, 1741, 2001]. Janalizadeh and Pasko [Abstracts AE21A-08; AE21B-3132; presented at 2018 Fall Meeting, AGU, Washington DC, 10-14 Dec., 2018] have recently introduced a modeling framework allowing investigation of halo induced electron impact ionization and photoionization of small traces of metallic species existing at sprite altitudes due to meteoric ablation as a source of plasma seeds required for initiation of sprite streamers. In the present work we extend this modeling framework to studies of photodetachment of electrons from O-, O2-, OH- and NO3- ions due to halo emissions. O2-, O- and OH- are the primary negative ions of the ambient D-region ionosphere [e.g., Pavlov, Surv. Geophys., 35, 259, 2014], and O-, O2- and NO3- are abundantly produced by streamer discharges in sprites [Sentman et al., JGR, 113, D11112, 2008; Gordillo-Vazquez, J. Phys. D: Appl. Phys., 41, 234016, 2008] and may provide relatively long-lasting seeds for sequential initiation of sprite streamers. Our analysis indicates that levels of these ions required for initiation of first sprite streamers can be produced by over-dense meteor trails with initial electron line densities > 1016 m-1 [e.g., Hocking et al., Ann. Geophys., 34, 1119, 2016]. The electron affinities of O-, O2-, OH- and NO3- are approximately 1.46, 0.45, 1.83, and 3.94 eV, respectively [e.g., Phelps, Can. J. Chem., 47, 1783,1969; Pavlov, 2014]. The first positive N2, second positive N2, first negative N2+, and Lyman-Birge-Hopfield (LBH) N2 band systems that have been documented in sprites [e.g., Liu et al., GRL, 33, L01101, 2006, and references therein], all contribute to photodetachment of electrons from O-, O2-, and OH- ions. Due to the relatively high affinity of NO3- (3.94 eV), only second positive N2 and N2 LBH band systems contribute to photodetachment of electrons from NO3-.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2019
- Bibcode:
- 2019AGUFMAE31B3105J
- Keywords:
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- 3304 Atmospheric electricity;
- ATMOSPHERIC PROCESSES;
- 3324 Lightning;
- ATMOSPHERIC PROCESSES;
- 3394 Instruments and techniques;
- ATMOSPHERIC PROCESSES