2022
DOI: 10.1029/2021ja030170
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A Comparison of the Midlatitude Nickel and Sodium Layers in the Mesosphere: Observations and Modeling

Abstract: The layer of nickel (Ni) atoms in the upper mesosphere and lower thermosphere (MLT) as well the layers of other metals (Fe, Na, Mg, Ca, and K) produced by meteoric ablation provide a unique means of observing the physics and chemistry of the atmosphere between 75 and 110 km (Plane, 2003;Plane et al., 2015). Although the Ni layer was only observed for the first time in 2012 (Collins et al., 2015), much progress in understanding the characteristic features of the layer has been made in the past 5 years. This has… Show more

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Cited by 12 publications
(21 citation statements)
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“…The main Ni and Na layers peak around 85 and 92 km, respectively, and main [Ni]/[Na] ratios are ∼0.1, consistent with the results of Jiao et al. (2022). The probable explanations include the more efficient ablation of Na from cosmic dust than Ni, the more rapid neutralization of Na + than Ni + between 90 and 100 km, and the significant differences in the neutral chemistries of these two metals below 90 km (Jiao et al., 2022).…”
Section: Discussionsupporting
confidence: 90%
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“…The main Ni and Na layers peak around 85 and 92 km, respectively, and main [Ni]/[Na] ratios are ∼0.1, consistent with the results of Jiao et al. (2022). The probable explanations include the more efficient ablation of Na from cosmic dust than Ni, the more rapid neutralization of Na + than Ni + between 90 and 100 km, and the significant differences in the neutral chemistries of these two metals below 90 km (Jiao et al., 2022).…”
Section: Discussionsupporting
confidence: 90%
“…However, these oxide ions also react with O, reducing them back to Ni + and this process competes with dissociative recombination, thereby slowing the conversion of Ni + to Ni. Thus, the relative electron to O concentrations control the rate of dissociative recombination (Bones et al., 2020; Jiao et al., 2022).…”
Section: Discussionmentioning
confidence: 99%
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