Observations of GPS scintillation during an isolated auroral substorm

Abstract This paper reports simultaneous observations of ionospheric scintillation during an auroral substorm that were made using an all-sky full-color digital single-lens reflex (DSLR) camera (ASC) and a Global Positioning System (GPS) ionospheric scintillation and total electron content monitor (...

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Main Authors: Hosokawa, Keisuke, Otsuka, Yuichi, Ogawa, Yasunobu, Tsugawa, Takuya
Format: Other/Unknown Material
Language:English
Published: BioMed Central Ltd. 2014
Subjects:
Online Access:http://www.progearthplanetsci.com/content/1/1/16
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spelling ftbiomed:oai:biomedcentral.com:2197-4284-1-16 2023-05-15T18:34:41+02:00 Observations of GPS scintillation during an isolated auroral substorm Hosokawa, Keisuke Otsuka, Yuichi Ogawa, Yasunobu Tsugawa, Takuya 2014-08-04 http://www.progearthplanetsci.com/content/1/1/16 en eng BioMed Central Ltd. http://www.progearthplanetsci.com/content/1/1/16 Copyright 2014 Hosokawa et al.; licensee Springer. Auroral ionosphere GPS scintillation Auroral substorm Ionospheric density irregularities Research 2014 ftbiomed 2014-08-17T00:37:51Z Abstract This paper reports simultaneous observations of ionospheric scintillation during an auroral substorm that were made using an all-sky full-color digital single-lens reflex (DSLR) camera (ASC) and a Global Positioning System (GPS) ionospheric scintillation and total electron content monitor (GISTM) in Tromsø (69.60 N, 19.20 E), Norway. On the night of November 19, 2009, a small substorm occurred in northern Scandinavia. The ASC captured its temporal evolution from the beginning of the growth phase to the end of the recovery phase. The amplitude scintillation, as monitored by the S 4 index from the GISTM, did not increase in any substorm phase. By contrast, phase scintillation, as measured by the σ φ index, occurred when discrete auroral arcs appeared on the GPS signal path. In particular, the phase scintillation was significantly enhanced for a few minutes immediately after the onset of the expansion phase. During this period, bright and discrete auroral forms covered the entire sky, which implies that structured precipitation on the scale of a few kilometers to a few tens of kilometers dominated the electron density distribution in the E region. Such inhomogeneous ionization structures probably produced significant changes in the refractive index and eventually resulted in the enhancement of the phase scintillation. Other/Unknown Material Tromsø BioMed Central Norway Tromsø
institution Open Polar
collection BioMed Central
op_collection_id ftbiomed
language English
topic Auroral ionosphere
GPS scintillation
Auroral substorm
Ionospheric density irregularities
spellingShingle Auroral ionosphere
GPS scintillation
Auroral substorm
Ionospheric density irregularities
Hosokawa, Keisuke
Otsuka, Yuichi
Ogawa, Yasunobu
Tsugawa, Takuya
Observations of GPS scintillation during an isolated auroral substorm
topic_facet Auroral ionosphere
GPS scintillation
Auroral substorm
Ionospheric density irregularities
description Abstract This paper reports simultaneous observations of ionospheric scintillation during an auroral substorm that were made using an all-sky full-color digital single-lens reflex (DSLR) camera (ASC) and a Global Positioning System (GPS) ionospheric scintillation and total electron content monitor (GISTM) in Tromsø (69.60 N, 19.20 E), Norway. On the night of November 19, 2009, a small substorm occurred in northern Scandinavia. The ASC captured its temporal evolution from the beginning of the growth phase to the end of the recovery phase. The amplitude scintillation, as monitored by the S 4 index from the GISTM, did not increase in any substorm phase. By contrast, phase scintillation, as measured by the σ φ index, occurred when discrete auroral arcs appeared on the GPS signal path. In particular, the phase scintillation was significantly enhanced for a few minutes immediately after the onset of the expansion phase. During this period, bright and discrete auroral forms covered the entire sky, which implies that structured precipitation on the scale of a few kilometers to a few tens of kilometers dominated the electron density distribution in the E region. Such inhomogeneous ionization structures probably produced significant changes in the refractive index and eventually resulted in the enhancement of the phase scintillation.
format Other/Unknown Material
author Hosokawa, Keisuke
Otsuka, Yuichi
Ogawa, Yasunobu
Tsugawa, Takuya
author_facet Hosokawa, Keisuke
Otsuka, Yuichi
Ogawa, Yasunobu
Tsugawa, Takuya
author_sort Hosokawa, Keisuke
title Observations of GPS scintillation during an isolated auroral substorm
title_short Observations of GPS scintillation during an isolated auroral substorm
title_full Observations of GPS scintillation during an isolated auroral substorm
title_fullStr Observations of GPS scintillation during an isolated auroral substorm
title_full_unstemmed Observations of GPS scintillation during an isolated auroral substorm
title_sort observations of gps scintillation during an isolated auroral substorm
publisher BioMed Central Ltd.
publishDate 2014
url http://www.progearthplanetsci.com/content/1/1/16
geographic Norway
Tromsø
geographic_facet Norway
Tromsø
genre Tromsø
genre_facet Tromsø
op_relation http://www.progearthplanetsci.com/content/1/1/16
op_rights Copyright 2014 Hosokawa et al.; licensee Springer.
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