Effects of solar wind density on auroral electrojets and brightness under influence of substorms

Using the auroral electrojet indices and Polar Ultraviolet Imager auroral images, we examined two fortuitous events during which the solar wind density had clear enhancements while the other solar wind parameters were relatively constant. Two electrojet enhancements were found in each event. Th...

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Main Authors: J.-H. Shue, Y. Kamide, J. W. Gjerloev
Format: Article
Language:English
Published: Copernicus Publications 2009-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/27/113/2009/angeo-27-113-2009.pdf
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spelling doaj-b8779c8042b94fe2894ea937b46930a92020-11-24T23:23:22ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762009-01-012711311910.5194/angeo-27-113-2009Effects of solar wind density on auroral electrojets and brightness under influence of substormsJ.-H. Shue0Y. Kamide1J. W. Gjerloev2Institute of Space Science, National Central University, Jhongli City, Taoyuan County 32001, TaiwanResearch Institute for Sustainable Humanosphere, Kyoto University, Uji 611-0011, JapanApplied Physics Laboratory, Johns Hopkins University, 11100 Johns Hopkins Road, Laurel 20723-6099, USAUsing the auroral electrojet indices and Polar Ultraviolet Imager auroral images, we examined two fortuitous events during which the solar wind density had clear enhancements while the other solar wind parameters were relatively constant. Two electrojet enhancements were found in each event. The first electrojet enhancement was likely to be related to a substorm in which an auroral bulge appeared at premidnight. The second electrojet enhancement was driven by the density enhancement in the solar wind. The auroral oval became wider in latitude and the auroral distribution became dispersed after the density enhancement arrived at the Earth. The total auroral power integrated over the entire nightside region from 50 to 80° MLAT, however, did not increase significantly in response to the density enhancement. Our interpretation is that the substorm that occurred prior to the solar wind density enhancement had drained out a significant portion of the stored energy in the magnetotail; therefore, less precipitation energy was deposited into the auroral ionosphere by the density enhancement.https://www.ann-geophys.net/27/113/2009/angeo-27-113-2009.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J.-H. Shue
Y. Kamide
J. W. Gjerloev
spellingShingle J.-H. Shue
Y. Kamide
J. W. Gjerloev
Effects of solar wind density on auroral electrojets and brightness under influence of substorms
Annales Geophysicae
author_facet J.-H. Shue
Y. Kamide
J. W. Gjerloev
author_sort J.-H. Shue
title Effects of solar wind density on auroral electrojets and brightness under influence of substorms
title_short Effects of solar wind density on auroral electrojets and brightness under influence of substorms
title_full Effects of solar wind density on auroral electrojets and brightness under influence of substorms
title_fullStr Effects of solar wind density on auroral electrojets and brightness under influence of substorms
title_full_unstemmed Effects of solar wind density on auroral electrojets and brightness under influence of substorms
title_sort effects of solar wind density on auroral electrojets and brightness under influence of substorms
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2009-01-01
description Using the auroral electrojet indices and Polar Ultraviolet Imager auroral images, we examined two fortuitous events during which the solar wind density had clear enhancements while the other solar wind parameters were relatively constant. Two electrojet enhancements were found in each event. The first electrojet enhancement was likely to be related to a substorm in which an auroral bulge appeared at premidnight. The second electrojet enhancement was driven by the density enhancement in the solar wind. The auroral oval became wider in latitude and the auroral distribution became dispersed after the density enhancement arrived at the Earth. The total auroral power integrated over the entire nightside region from 50 to 80° MLAT, however, did not increase significantly in response to the density enhancement. Our interpretation is that the substorm that occurred prior to the solar wind density enhancement had drained out a significant portion of the stored energy in the magnetotail; therefore, less precipitation energy was deposited into the auroral ionosphere by the density enhancement.
url https://www.ann-geophys.net/27/113/2009/angeo-27-113-2009.pdf
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