Far Ultraviolet Remote Sensing of the Nighttime Ionosphere Using the OI 130.4‐nm Emission

2020 ◽  
Vol 125 (6) ◽  
Author(s):  
Jianqi Qin
1993 ◽  
Vol 31 (5) ◽  
pp. 931-945 ◽  
Author(s):  
I. Oznovich ◽  
A. Ravitz ◽  
M. Tur ◽  
I. Glaser ◽  
R.E. Huffman ◽  
...  

2005 ◽  
Vol 110 (A11) ◽  
Author(s):  
C. Blockx ◽  
J.-C. Gérard ◽  
M. Meurant ◽  
B. Hubert ◽  
V. Coumans

2003 ◽  
Vol 31 (4) ◽  
pp. 813-818 ◽  
Author(s):  
Larry J. Paxton ◽  
Daniel Morrison ◽  
Douglas J. Strickland ◽  
M.Geoff McHarg ◽  
Yongliang Zhang ◽  
...  

2010 ◽  
Vol 30 (6) ◽  
pp. 1816-1821
Author(s):  
Zhang Zhenduo ◽  
Wang Shurong ◽  
Li Futian ◽  
Huang Yu ◽  
Qu Yi Lin Guanyu

2019 ◽  
Author(s):  
Harold K. Knight

Abstract. Coincident auroral far ultraviolet (FUV) and ground-based ionosonde observations are compared for the purpose of determining whether auroral FUV remote sensing algorithms that assume pure electron precipitation are biased in the presence of proton precipitation. Auroral particle transport and optical emission models, such as the Boltzmann 3-Constituent (B3C) model, predict that maximum E region electron density (NmE) values derived from auroral Lyman-Birge-Hopfield (LBH) emission assuming electron precipitation will be biased high by up to ~ 20 % for pure proton aurora, while comparisons between LBH radiances and radiances derived from in situ particle flux observations (i.e., Knight et al., 2008, 2012) indicate that the bias associated with proton aurora should be much larger. Surprisingly, in the comparisons with ionosonde observations described here, no bias associated with proton aurora is found in FUV-derived auroral NmE, which means that auroral FUV remote sensing methods for NmE are more accurate in the presence of proton precipitation than was suggested in the aforementioned earlier works. Possible explanations for the discrepancy with the earlier results are discussed.


2021 ◽  
Author(s):  
Yingcheng Lu ◽  
Ziyi Suo ◽  
jianqiang liu ◽  
Jing Ding ◽  
Dayi Yin ◽  
...  

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