2016
DOI: 10.1002/2016jd025015
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Mesospheric ozone destruction by high‐energy electron precipitation associated with pulsating aurora

Abstract: Energetic particle precipitation into the upper atmosphere creates excess amounts of odd nitrogen and odd hydrogen. These destroy mesospheric and upper stratospheric ozone in catalytic reaction chains, either in situ at the altitude of the energy deposition or indirectly due to transport to other altitudes and latitudes. Recent statistical analysis of satellite data on mesospheric ozone reveals that the variations during energetic electron precipitation from Earth's radiation belts can be tens of percent. Here… Show more

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Cited by 91 publications
(130 citation statements)
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“…Turunen et al, 2016). Results indicate that SPEs are linked to an~5-10% decrease in ozone at~20 km altitude.…”
Section: Discussionmentioning
confidence: 94%
“…Turunen et al, 2016). Results indicate that SPEs are linked to an~5-10% decrease in ozone at~20 km altitude.…”
Section: Discussionmentioning
confidence: 94%
“…The largest enhancement of NO x concentration is approximately a factor of 8.3 and occurs around 72 km. After the electron forcing, the NO x recovery is mainly due to the photodestruction of NO, which is gradual and relatively slow (Turunen et al, ). About 71% of the excess NO x produced by the forcing of 10 MeV monoenergetic electrons at ∼72 km remains beyond the end of the 2 day simulation period (see Figure ).…”
Section: Resultsmentioning
confidence: 99%
“…CNA values typically exceed 0.5 dB during energetic particle precipitation and may occasionally reach values as high as 10 dB. However, the pulsating aurora events studied by Milan et al [] and recently Turunen et al [] exhibit CNA of the order of 0.5–1 dB.…”
Section: Resultsmentioning
confidence: 99%
“…In particular, conjunctions between the Japanese Arase (ERG) satellite [ Miyoshi et al , ] and ground‐based instruments in northern Fennoscandia in the postmidnight and morning magnetic local time sectors could be exploited to study pulsating aurora even outside of the dark season, using KAIRA instead of the optical instruments. This may prove important to study the atmospheric effects of high‐energy precipitation during pulsating aurora events, as was initiated by Turunen et al [].…”
Section: Discussionmentioning
confidence: 99%