TY - JOUR
T1 - Empirical values of branching ratios in the three-body recombination reaction for O( 1 S) and O 2 (0,0) airglow chemistry
AU - Amaro-Rivera, Yolián
AU - Huang, Tai Yin
AU - Urbina, Julio
AU - Vargas, Fabio
N1 - Funding Information:
Y. Amaro-Rivera would like to thank the Alfred Sloan Foundation for providing financial support. We thank G. Shepherd and Y-M. Cho for providing WINDII data for our study. This study used the NRLMSISE-00 model (Picone et al. 2002) from the CEDAR Database at the National Center for Atmospheric Research, which is supported by the National Science Foundation of the United States of America.
Publisher Copyright:
© 2018 COSPAR
PY - 2018/11/1
Y1 - 2018/11/1
N2 - The branching ratios ε and α in the three-body recombination reaction for O( 1 S) greenline and O 2 (0,0) atmospheric band airglow chemistry represent the fraction of O 2 that branch into the b 1 ∑ g + and c 1 ∑ u - electronic states, respectively. In the present work, the empirical values of these branching ratios have been deduced using a numerical optimization approach. They were obtained using the optimization scheme known as the Covariance Matrix Adaptation Evolution Strategy (CMA-ES) with our MACD-00 model and simultaneous volume emission rate (VER) measurements of the O( 1 S) greenline and O 2 (0,0) atmospheric band emissions. The CMA-ES was employed as the optimization algorithm that would match the O( 1 S) and O 2 (0,0) VER profiles simulated by the MACD-00 model to observations made by OXYGEN/S35, S310.10, NASA Flight 4.339, ETON flights P229H and P230H, OASIS, SOAP/WINE, MULTIFOT, and WINDII. We found that most of the values deduced for ε were in the [0.1, 0.3] range, while most of the values of α were in the [0.01, 0.03] range. Excluding the outliers, the average branching ratio values involving the production of O 2 (b 1 ∑ g + ) and O 2 (c 1 ∑ u - ) were determined to be ε = 0.15 ± 0.02 and α = 0.018 ± 0.004, respectively. Overall, the simulations showed good agreement with the observations albeit with some discrepancies in the peak altitudes and shape of the profiles, possibly due to small perturbations in the observed VER profiles that are not considered in our simulations.
AB - The branching ratios ε and α in the three-body recombination reaction for O( 1 S) greenline and O 2 (0,0) atmospheric band airglow chemistry represent the fraction of O 2 that branch into the b 1 ∑ g + and c 1 ∑ u - electronic states, respectively. In the present work, the empirical values of these branching ratios have been deduced using a numerical optimization approach. They were obtained using the optimization scheme known as the Covariance Matrix Adaptation Evolution Strategy (CMA-ES) with our MACD-00 model and simultaneous volume emission rate (VER) measurements of the O( 1 S) greenline and O 2 (0,0) atmospheric band emissions. The CMA-ES was employed as the optimization algorithm that would match the O( 1 S) and O 2 (0,0) VER profiles simulated by the MACD-00 model to observations made by OXYGEN/S35, S310.10, NASA Flight 4.339, ETON flights P229H and P230H, OASIS, SOAP/WINE, MULTIFOT, and WINDII. We found that most of the values deduced for ε were in the [0.1, 0.3] range, while most of the values of α were in the [0.01, 0.03] range. Excluding the outliers, the average branching ratio values involving the production of O 2 (b 1 ∑ g + ) and O 2 (c 1 ∑ u - ) were determined to be ε = 0.15 ± 0.02 and α = 0.018 ± 0.004, respectively. Overall, the simulations showed good agreement with the observations albeit with some discrepancies in the peak altitudes and shape of the profiles, possibly due to small perturbations in the observed VER profiles that are not considered in our simulations.
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U2 - 10.1016/j.asr.2018.07.018
DO - 10.1016/j.asr.2018.07.018
M3 - Article
AN - SCOPUS:85050854425
SN - 0273-1177
VL - 62
SP - 2679
EP - 2691
JO - Advances in Space Research
JF - Advances in Space Research
IS - 9
ER -