Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds
This study focuses on the poorly known effect of polar cap patches (PCPs) on the ion-neutral coupling in the F-region. The PCPs were identified by total electron content measurements from the Global Navigation Satellite System (GNSS) and the ionospheric parameters from the Defense Meteorological Sat...
Published in: | Journal of Geophysical Research: Space Physics |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Uppsala universitet, Institutet för rymdfysik, Uppsalaavdelningen
2024
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-536982 https://doi.org/10.1029/2024JA032819 |
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ftuppsalauniv:oai:DiVA.org:uu-536982 2024-09-30T14:34:20+00:00 Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds Cai, L. Aikio, A. Oyama, S. Ivchenko, N. Vanhamaki, H. Virtanen, I. Buchert, Stephan Mekuriaw, M. L. Zhang, Y. 2024 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-536982 https://doi.org/10.1029/2024JA032819 eng eng Uppsala universitet, Institutet för rymdfysik, Uppsalaavdelningen Univ Oulu, Space Phys & Astron, Oulu, Finland. Nagoya Univ, Inst Space Earth Environm Res, Nagoya, Japan.;Natl Inst Polar Res, Tachikawa, Japan. KTH, EECS, Space & Plasma Phys, Stockholm, Sweden. Johns Hopkins Univ, Appl Phys Lab, Laurel, MD USA. Journal of Geophysical Research - Space Physics, 2169-9380, 2024, 129:8, orcid:0000-0003-2158-6074 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-536982 doi:10.1029/2024JA032819 ISI:001282546900001 info:eu-repo/semantics/openAccess upper thermospheric wind polar cap patches ionosphere-thermosphere ion-neutral coupling blobs high-latitude electrodynamics Fusion Plasma and Space Physics plasma och rymdfysik Aerospace Engineering Rymd- och flygteknik Article in journal info:eu-repo/semantics/article text 2024 ftuppsalauniv https://doi.org/10.1029/2024JA032819 2024-09-11T00:07:01Z This study focuses on the poorly known effect of polar cap patches (PCPs) on the ion-neutral coupling in the F-region. The PCPs were identified by total electron content measurements from the Global Navigation Satellite System (GNSS) and the ionospheric parameters from the Defense Meteorological Satellite Program spacecraft. The EISCAT incoherent scatter radars on Svalbard and at Troms & oslash;, Norway observed that PCPs entered the nightside auroral oval from the polar cap and became plasma blobs. The ionospheric convection further transported the plasma blobs to the duskside. Simultaneously, long-lasting strong upper thermospheric winds were detected in the duskside auroral oval by a Fabry-Perot Interferometer (FPI) at Troms & oslash; and in the polar cap by the Gravity Recovery and Climate Experiment satellite. Using EISCAT ion velocities and plasma parameters as well as FPI winds, the ion drag acting on neutrals and the time constant for the ion drag could be estimated. Due to the arrival of PCPs/blobs and the accompanied increase in the F-region electron densities, the ion drag is enhanced between about 220 and 500 km altitudes. At the F peak altitudes near 300 km, the median ion drag acceleration affecting neutrals more than doubled and the associated median e-folding time decreased from 4.4 to 2 hr. The strong neutral wind was found to be driven primarily by the ion drag force due to large-scale ionospheric convection. Our results provide a new insight into ionosphere-thermosphere coupling in the presence of PCPs/blobs. This study investigates how the evolution of the polar cap patches (PCPs) affects the upper layer of the Earth's atmosphere, termed the thermosphere. PCPs are dense patches of charged particles that move from the dayside to the nightside of the high-latitude ionosphere through the polar cap region. Using the measurements by multiple ground-based instruments and satellites, this study found that PCPs can enhance the formation of strong upper thermospheric winds. The winds are ... Article in Journal/Newspaper EISCAT Svalbard Troms Uppsala University: Publications (DiVA) Norway Svalbard Journal of Geophysical Research: Space Physics 129 8 |
institution |
Open Polar |
collection |
Uppsala University: Publications (DiVA) |
op_collection_id |
ftuppsalauniv |
language |
English |
topic |
upper thermospheric wind polar cap patches ionosphere-thermosphere ion-neutral coupling blobs high-latitude electrodynamics Fusion Plasma and Space Physics plasma och rymdfysik Aerospace Engineering Rymd- och flygteknik |
spellingShingle |
upper thermospheric wind polar cap patches ionosphere-thermosphere ion-neutral coupling blobs high-latitude electrodynamics Fusion Plasma and Space Physics plasma och rymdfysik Aerospace Engineering Rymd- och flygteknik Cai, L. Aikio, A. Oyama, S. Ivchenko, N. Vanhamaki, H. Virtanen, I. Buchert, Stephan Mekuriaw, M. L. Zhang, Y. Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds |
topic_facet |
upper thermospheric wind polar cap patches ionosphere-thermosphere ion-neutral coupling blobs high-latitude electrodynamics Fusion Plasma and Space Physics plasma och rymdfysik Aerospace Engineering Rymd- och flygteknik |
description |
This study focuses on the poorly known effect of polar cap patches (PCPs) on the ion-neutral coupling in the F-region. The PCPs were identified by total electron content measurements from the Global Navigation Satellite System (GNSS) and the ionospheric parameters from the Defense Meteorological Satellite Program spacecraft. The EISCAT incoherent scatter radars on Svalbard and at Troms & oslash;, Norway observed that PCPs entered the nightside auroral oval from the polar cap and became plasma blobs. The ionospheric convection further transported the plasma blobs to the duskside. Simultaneously, long-lasting strong upper thermospheric winds were detected in the duskside auroral oval by a Fabry-Perot Interferometer (FPI) at Troms & oslash; and in the polar cap by the Gravity Recovery and Climate Experiment satellite. Using EISCAT ion velocities and plasma parameters as well as FPI winds, the ion drag acting on neutrals and the time constant for the ion drag could be estimated. Due to the arrival of PCPs/blobs and the accompanied increase in the F-region electron densities, the ion drag is enhanced between about 220 and 500 km altitudes. At the F peak altitudes near 300 km, the median ion drag acceleration affecting neutrals more than doubled and the associated median e-folding time decreased from 4.4 to 2 hr. The strong neutral wind was found to be driven primarily by the ion drag force due to large-scale ionospheric convection. Our results provide a new insight into ionosphere-thermosphere coupling in the presence of PCPs/blobs. This study investigates how the evolution of the polar cap patches (PCPs) affects the upper layer of the Earth's atmosphere, termed the thermosphere. PCPs are dense patches of charged particles that move from the dayside to the nightside of the high-latitude ionosphere through the polar cap region. Using the measurements by multiple ground-based instruments and satellites, this study found that PCPs can enhance the formation of strong upper thermospheric winds. The winds are ... |
format |
Article in Journal/Newspaper |
author |
Cai, L. Aikio, A. Oyama, S. Ivchenko, N. Vanhamaki, H. Virtanen, I. Buchert, Stephan Mekuriaw, M. L. Zhang, Y. |
author_facet |
Cai, L. Aikio, A. Oyama, S. Ivchenko, N. Vanhamaki, H. Virtanen, I. Buchert, Stephan Mekuriaw, M. L. Zhang, Y. |
author_sort |
Cai, L. |
title |
Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds |
title_short |
Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds |
title_full |
Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds |
title_fullStr |
Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds |
title_full_unstemmed |
Effect of Polar Cap Patches on the High-Latitude Upper Thermospheric Winds |
title_sort |
effect of polar cap patches on the high-latitude upper thermospheric winds |
publisher |
Uppsala universitet, Institutet för rymdfysik, Uppsalaavdelningen |
publishDate |
2024 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-536982 https://doi.org/10.1029/2024JA032819 |
geographic |
Norway Svalbard |
geographic_facet |
Norway Svalbard |
genre |
EISCAT Svalbard Troms |
genre_facet |
EISCAT Svalbard Troms |
op_relation |
Journal of Geophysical Research - Space Physics, 2169-9380, 2024, 129:8, orcid:0000-0003-2158-6074 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-536982 doi:10.1029/2024JA032819 ISI:001282546900001 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2024JA032819 |
container_title |
Journal of Geophysical Research: Space Physics |
container_volume |
129 |
container_issue |
8 |
_version_ |
1811637984366166016 |