Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99

The temporal and spatial behaviour of the ionospheric parameters <i>f</i>oF2 and h'F during isolated substorms are examined using data from ionospheric stations distributed across Europe and western Asia. The main purpose is finding the forerunners of the substorm disturbanc...

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Main Authors: D. V. Blagoveshchensky, O. A. Maltseva, A. S. Rodger
Format: Article
Language:English
Published: Copernicus Publications 2003-05-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/21/1141/2003/angeo-21-1141-2003.pdf
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spelling doaj-aff714b5c16f45719f650ea47906f3b42020-11-25T01:04:27ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762003-05-01211141115110.5194/angeo-21-1141-2003Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99D. V. Blagoveshchensky0O. A. Maltseva1A. S. Rodger2University of Aerospace Instrumentation, St. Petersburg, 190000, RussiaInstitute of Physics, Rostov University, Rostov-on-Don, 344090, RussiaBritish Antarctic Survey, Madingley Road, Cambridge, CB3 OET, UKThe temporal and spatial behaviour of the ionospheric parameters <i>f</i>oF2 and h'F during isolated substorms are examined using data from ionospheric stations distributed across Europe and western Asia. The main purpose is finding the forerunners of the substorm disturbances and a possible prediction of these disturbances. During the period from March 1998 to March 1999, 41 isolated substorms with intensities I = 60 - 400 nT were identified and studied. The study separated occasions when the local magnetometers were affected by the eastward electrojet (positive substorms) from those influenced by the westward electrojet (negative substorms). The deviations of the ionospheric parameters from their monthly medians (<i><font face="Symbol">D</font>f</i>oF2 and <i><font face="Symbol">D</font></i>h'F) have been used to determine the variations through the substorm. Substorm effects occurred simultaneously (&lt; 1 h) across the entire observatory network. For negative substorms, <i><font face="Symbol">D</font>f</i>oF2-values increase &gt; 6 h before substorm onset, T<sub>o</sub>, reaching a maximum 2–3 h before T<sub>o</sub>. A second maximum occurs 1–2 h after the end of the substorm. The <i><font face="Symbol">D</font></i>h'F values 3–4 h before To have a small minimum but then increase to a maximum at T<sub>o</sub>. There is a second maximum at the end of the expansion phase before <font face="Symbol"><i>d</i></font>h'F drops to a minimum 2–3 h after ending the expansion phase. For positive substorms, the timing of the first maximum of the <i><font face="Symbol">d</font>f</i>oF2 and <font face="Symbol"><i>d</i></font>h'F values depends on the substorm length – if it is longer, the position is closer to T<sub>o</sub>. The effects on the ionosphere are significant: <i><font face="Symbol">D</font>f</i>oF2 and <i><font face="Symbol">D</font></i>h'F reach 2–3 MHz (<i><font face="Symbol">d</font>f</i>oF2 = 50–70% from median value) and 50–70 km (<i><font face="Symbol">D</font></i> h'F = 20–30% from median value), respectively. Regular patterns of occurrence ahead of the first substorm signature on the magnetometer offer an excellent possibility to improve short-term forecasting of radio wave propagation conditions.<br><br><b>Key words. </b>Ionosphere (ionospheric disturbances) – Magnetospheric physics (storms and substorms) Radio science (ionospheric physics)https://www.ann-geophys.net/21/1141/2003/angeo-21-1141-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. V. Blagoveshchensky
O. A. Maltseva
A. S. Rodger
spellingShingle D. V. Blagoveshchensky
O. A. Maltseva
A. S. Rodger
Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99
Annales Geophysicae
author_facet D. V. Blagoveshchensky
O. A. Maltseva
A. S. Rodger
author_sort D. V. Blagoveshchensky
title Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99
title_short Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99
title_full Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99
title_fullStr Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99
title_full_unstemmed Ionosphere dynamics over Europe and western Asia during magnetospheric substorms 1998–99
title_sort ionosphere dynamics over europe and western asia during magnetospheric substorms 1998–99
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2003-05-01
description The temporal and spatial behaviour of the ionospheric parameters <i>f</i>oF2 and h'F during isolated substorms are examined using data from ionospheric stations distributed across Europe and western Asia. The main purpose is finding the forerunners of the substorm disturbances and a possible prediction of these disturbances. During the period from March 1998 to March 1999, 41 isolated substorms with intensities I = 60 - 400 nT were identified and studied. The study separated occasions when the local magnetometers were affected by the eastward electrojet (positive substorms) from those influenced by the westward electrojet (negative substorms). The deviations of the ionospheric parameters from their monthly medians (<i><font face="Symbol">D</font>f</i>oF2 and <i><font face="Symbol">D</font></i>h'F) have been used to determine the variations through the substorm. Substorm effects occurred simultaneously (&lt; 1 h) across the entire observatory network. For negative substorms, <i><font face="Symbol">D</font>f</i>oF2-values increase &gt; 6 h before substorm onset, T<sub>o</sub>, reaching a maximum 2–3 h before T<sub>o</sub>. A second maximum occurs 1–2 h after the end of the substorm. The <i><font face="Symbol">D</font></i>h'F values 3–4 h before To have a small minimum but then increase to a maximum at T<sub>o</sub>. There is a second maximum at the end of the expansion phase before <font face="Symbol"><i>d</i></font>h'F drops to a minimum 2–3 h after ending the expansion phase. For positive substorms, the timing of the first maximum of the <i><font face="Symbol">d</font>f</i>oF2 and <font face="Symbol"><i>d</i></font>h'F values depends on the substorm length – if it is longer, the position is closer to T<sub>o</sub>. The effects on the ionosphere are significant: <i><font face="Symbol">D</font>f</i>oF2 and <i><font face="Symbol">D</font></i>h'F reach 2–3 MHz (<i><font face="Symbol">d</font>f</i>oF2 = 50–70% from median value) and 50–70 km (<i><font face="Symbol">D</font></i> h'F = 20–30% from median value), respectively. Regular patterns of occurrence ahead of the first substorm signature on the magnetometer offer an excellent possibility to improve short-term forecasting of radio wave propagation conditions.<br><br><b>Key words. </b>Ionosphere (ionospheric disturbances) – Magnetospheric physics (storms and substorms) Radio science (ionospheric physics)
url https://www.ann-geophys.net/21/1141/2003/angeo-21-1141-2003.pdf
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