Types of pulsating aurora: Comparison of model and EISCAT electron density observations

Energetic particle precipitation associated with pulsating aurora (PsA) can reach down to lower mesospheric altitudes and deplete ozone. It is well documented that pulsating aurora is a common phenomenon during substorm recovery phases. This indicates that using magnetic indices to model the chemist...

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Published in:Annales Geophysicae
Main Authors: Tesema, Fasil, Partamies, Noora, Whiter, Daniel K., Ogawa, Yasunobu
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://hdl.handle.net/11250/2997237
https://doi.org/10.5194/angeo-40-1-2022
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author Tesema, Fasil
Partamies, Noora
Whiter, Daniel K.
Ogawa, Yasunobu
author_facet Tesema, Fasil
Partamies, Noora
Whiter, Daniel K.
Ogawa, Yasunobu
author_sort Tesema, Fasil
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
container_issue 1
container_start_page 1
container_title Annales Geophysicae
container_volume 40
description Energetic particle precipitation associated with pulsating aurora (PsA) can reach down to lower mesospheric altitudes and deplete ozone. It is well documented that pulsating aurora is a common phenomenon during substorm recovery phases. This indicates that using magnetic indices to model the chemistry induced by PsA electrons could underestimate the energy deposition in the atmosphere. Integrating satellite measurements of precipitating electrons in models is considered to be an alternative way to account for such an underestimation. One way to do this is to test and validate the existing ion chemistry models using integrated measurements from satellite and ground-based observations. By using satellite measurements, an average or typical spectrum of PsA electrons can be constructed and used as an input in models to study the effects of the energetic electrons in the atmosphere. In this study, we compare electron densities from the EISCAT (European Incoherent Scatter scientific radar system) radars with auroral ion chemistry and the energetics model by using pulsating aurora spectra derived from the Polar Operational Environmental Satellite (POES) as an energy input for the model. We found a good agreement between the model and EISCAT electron densities in the region dominated by patchy pulsating aurora. However, the magnitude of the observed electron densities suggests a significant difference in the flux of precipitating electrons for different pulsating aurora types (structures) observed. publishedVersion
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genre EISCAT
genre_facet EISCAT
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op_doi https://doi.org/10.5194/angeo-40-1-2022
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https://hdl.handle.net/11250/2997237
https://doi.org/10.5194/angeo-40-1-2022
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Annales Geophysicae. 2022, 40 (1), 1-10.
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
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spelling ftunivbergen:oai:bora.uib.no:11250/2997237 2025-01-16T21:41:58+00:00 Types of pulsating aurora: Comparison of model and EISCAT electron density observations Tesema, Fasil Partamies, Noora Whiter, Daniel K. Ogawa, Yasunobu 2022 application/pdf https://hdl.handle.net/11250/2997237 https://doi.org/10.5194/angeo-40-1-2022 eng eng Copernicus Publications urn:issn:0992-7689 https://hdl.handle.net/11250/2997237 https://doi.org/10.5194/angeo-40-1-2022 cristin:2023039 Annales Geophysicae. 2022, 40 (1), 1-10. Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Copyright Author(s) 2022 Annales Geophysicae 1-10 40 1 Journal article Peer reviewed 2022 ftunivbergen https://doi.org/10.5194/angeo-40-1-2022 2023-03-14T17:38:52Z Energetic particle precipitation associated with pulsating aurora (PsA) can reach down to lower mesospheric altitudes and deplete ozone. It is well documented that pulsating aurora is a common phenomenon during substorm recovery phases. This indicates that using magnetic indices to model the chemistry induced by PsA electrons could underestimate the energy deposition in the atmosphere. Integrating satellite measurements of precipitating electrons in models is considered to be an alternative way to account for such an underestimation. One way to do this is to test and validate the existing ion chemistry models using integrated measurements from satellite and ground-based observations. By using satellite measurements, an average or typical spectrum of PsA electrons can be constructed and used as an input in models to study the effects of the energetic electrons in the atmosphere. In this study, we compare electron densities from the EISCAT (European Incoherent Scatter scientific radar system) radars with auroral ion chemistry and the energetics model by using pulsating aurora spectra derived from the Polar Operational Environmental Satellite (POES) as an energy input for the model. We found a good agreement between the model and EISCAT electron densities in the region dominated by patchy pulsating aurora. However, the magnitude of the observed electron densities suggests a significant difference in the flux of precipitating electrons for different pulsating aurora types (structures) observed. publishedVersion Article in Journal/Newspaper EISCAT University of Bergen: Bergen Open Research Archive (BORA-UiB) Annales Geophysicae 40 1 1 10
spellingShingle Tesema, Fasil
Partamies, Noora
Whiter, Daniel K.
Ogawa, Yasunobu
Types of pulsating aurora: Comparison of model and EISCAT electron density observations
title Types of pulsating aurora: Comparison of model and EISCAT electron density observations
title_full Types of pulsating aurora: Comparison of model and EISCAT electron density observations
title_fullStr Types of pulsating aurora: Comparison of model and EISCAT electron density observations
title_full_unstemmed Types of pulsating aurora: Comparison of model and EISCAT electron density observations
title_short Types of pulsating aurora: Comparison of model and EISCAT electron density observations
title_sort types of pulsating aurora: comparison of model and eiscat electron density observations
url https://hdl.handle.net/11250/2997237
https://doi.org/10.5194/angeo-40-1-2022