Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc

In this paper we study the presence of irregularities and scintillation in relation to the nightside part of a long-lived, Sun-aligned transpolar arc on 15 January 2015. The arc was observed in DMSP UV and particle data and lasted at least 3 h between 1700 and 2000 UT. The arc was more intense than...

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Published in:Journal of Geophysical Research: Space Physics
Main Authors: van der Meeren, Christer, Oksavik, Kjellmar, Lorentzen, Dag Arne, Paxton, Larry J., Clausen, Lasse Boy Novock
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2016
Subjects:
Online Access:https://hdl.handle.net/1956/12990
https://doi.org/10.1002/2016ja022708
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author van der Meeren, Christer
Oksavik, Kjellmar
Lorentzen, Dag Arne
Paxton, Larry J.
Clausen, Lasse Boy Novock
author_facet van der Meeren, Christer
Oksavik, Kjellmar
Lorentzen, Dag Arne
Paxton, Larry J.
Clausen, Lasse Boy Novock
author_sort van der Meeren, Christer
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
container_issue 6
container_start_page 5723
container_title Journal of Geophysical Research: Space Physics
container_volume 121
description In this paper we study the presence of irregularities and scintillation in relation to the nightside part of a long-lived, Sun-aligned transpolar arc on 15 January 2015. The arc was observed in DMSP UV and particle data and lasted at least 3 h between 1700 and 2000 UT. The arc was more intense than the main oval during this time. From all-sky imagers on Svalbard we were able to study the evolution of the arc, which drifted slowly westward toward the dusk cell. The intensity of the arc as observed from ground was 10–17 kR in 557.7 nm and 2–3.5 kR in 630.0 nm, i.e., significant emissions in both green and red emission lines. We have used high-resolution raw data from global navigation satellite systems (GNSS) receivers and backscatter from Super Dual Auroral Radar Network (SuperDARN) radars to study irregularities and scintillation in relation to the polar cap arc. Even though the literature has suggested that polar cap arcs are potential sources for irregularities, our results indicate only very weak irregularities. This may be due to the background density in the northward IMF polar cap being too low for significant irregularities to be created. publishedVersion
format Article in Journal/Newspaper
genre Svalbard
genre_facet Svalbard
geographic Svalbard
geographic_facet Svalbard
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op_doi https://doi.org/10.1002/2016ja022708
op_relation Mesoscale ionospheric plasma irregularities and scintillation over Svalbard
urn:issn:2169-9380
https://hdl.handle.net/1956/12990
https://doi.org/10.1002/2016ja022708
op_rights Attribution-NonCommercial-NoDerivs CC BY-NC-ND
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Copyright 2016 The Authors
op_source Journal of Geophysical Research: Space Physics
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spelling ftunivbergen:oai:bora.uib.no:1956/12990 2025-01-17T01:02:21+00:00 Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc van der Meeren, Christer Oksavik, Kjellmar Lorentzen, Dag Arne Paxton, Larry J. Clausen, Lasse Boy Novock 2016-06-18 application/pdf https://hdl.handle.net/1956/12990 https://doi.org/10.1002/2016ja022708 eng eng American Geophysical Union Mesoscale ionospheric plasma irregularities and scintillation over Svalbard urn:issn:2169-9380 https://hdl.handle.net/1956/12990 https://doi.org/10.1002/2016ja022708 Attribution-NonCommercial-NoDerivs CC BY-NC-ND http://creativecommons.org/licenses/by-nc-nd/4.0/ Copyright 2016 The Authors Journal of Geophysical Research: Space Physics 121 6 5723-5736 VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 Peer reviewed Journal article 2016 ftunivbergen https://doi.org/10.1002/2016ja022708 2023-03-14T17:41:08Z In this paper we study the presence of irregularities and scintillation in relation to the nightside part of a long-lived, Sun-aligned transpolar arc on 15 January 2015. The arc was observed in DMSP UV and particle data and lasted at least 3 h between 1700 and 2000 UT. The arc was more intense than the main oval during this time. From all-sky imagers on Svalbard we were able to study the evolution of the arc, which drifted slowly westward toward the dusk cell. The intensity of the arc as observed from ground was 10–17 kR in 557.7 nm and 2–3.5 kR in 630.0 nm, i.e., significant emissions in both green and red emission lines. We have used high-resolution raw data from global navigation satellite systems (GNSS) receivers and backscatter from Super Dual Auroral Radar Network (SuperDARN) radars to study irregularities and scintillation in relation to the polar cap arc. Even though the literature has suggested that polar cap arcs are potential sources for irregularities, our results indicate only very weak irregularities. This may be due to the background density in the northward IMF polar cap being too low for significant irregularities to be created. publishedVersion Article in Journal/Newspaper Svalbard University of Bergen: Bergen Open Research Archive (BORA-UiB) Svalbard Journal of Geophysical Research: Space Physics 121 6 5723 5736
spellingShingle VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
van der Meeren, Christer
Oksavik, Kjellmar
Lorentzen, Dag Arne
Paxton, Larry J.
Clausen, Lasse Boy Novock
Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc
title Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc
title_full Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc
title_fullStr Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc
title_full_unstemmed Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc
title_short Scintillation and irregularities from the nightside part of a Sun-aligned polar cap arc
title_sort scintillation and irregularities from the nightside part of a sun-aligned polar cap arc
topic VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
topic_facet VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
url https://hdl.handle.net/1956/12990
https://doi.org/10.1002/2016ja022708