Quantitative magnetotail characteristics of different magnetospheric states

Quantitative relationships allowing one to compute the lobe magnetic field, flaring angle and tail radius, and to evaluate magnetic flux based on solar wind/IMF parameters and spacecraft position are obtained for the middle magnetotail, <i>X</i>=(–15,–35)<i>R<sub>E</sub>...

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Main Authors: M. A. Shukhtina, N. P. Dmitrieva, V. A. Sergeev
Format: Article
Language:English
Published: Copernicus Publications 2004-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/1019/2004/angeo-22-1019-2004.pdf
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spelling doaj-3c54192df73d43ce8ea8007e341d2bbb2020-11-25T01:58:24ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-03-01221019103210.5194/angeo-22-1019-2004Quantitative magnetotail characteristics of different magnetospheric statesM. A. Shukhtina0N. P. Dmitrieva1V. A. Sergeev2V. A. Fock Institute of Physics, St.-Petersburg State University, St.-Petersburg, RussiaV. A. Fock Institute of Physics, St.-Petersburg State University, St.-Petersburg, RussiaV. A. Fock Institute of Physics, St.-Petersburg State University, St.-Petersburg, RussiaQuantitative relationships allowing one to compute the lobe magnetic field, flaring angle and tail radius, and to evaluate magnetic flux based on solar wind/IMF parameters and spacecraft position are obtained for the middle magnetotail, <i>X</i>=(–15,–35)<i>R<sub>E</sub></i>, using 3.5 years of simultaneous Geotail and Wind spacecraft observations. For the first time it was done separately for different states of magnetotail including the substorm onset (SO) epoch, the steady magnetospheric convection (SMC) and quiet periods (Q). In the explored distance range the magnetotail parameters appeared to be similar (within the error bar) for Q and SMC states, whereas at SO their values are considerably larger. In particular, the tail radius is larger by 1–3 <i>R<sub>E</sub></i> at substorm onset than during Q and SMC states, for which the radius value is close to previous magnetopause model values. The calculated lobe magnetic flux value at substorm onset is ~1GWb, exceeding that at Q (SMC) states by ~50%. The model magnetic flux values at substorm onset and SMC show little dependence on the solar wind dynamic pressure and distance in the tail, so the magnetic flux value can serve as an important discriminator of the state of the middle magnetotail.<br><br> <b>Key words.</b> Magnetospheric physics (solar windmagnetosphere- interactions, magnetotail, storms and substorms)https://www.ann-geophys.net/22/1019/2004/angeo-22-1019-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. A. Shukhtina
N. P. Dmitrieva
V. A. Sergeev
spellingShingle M. A. Shukhtina
N. P. Dmitrieva
V. A. Sergeev
Quantitative magnetotail characteristics of different magnetospheric states
Annales Geophysicae
author_facet M. A. Shukhtina
N. P. Dmitrieva
V. A. Sergeev
author_sort M. A. Shukhtina
title Quantitative magnetotail characteristics of different magnetospheric states
title_short Quantitative magnetotail characteristics of different magnetospheric states
title_full Quantitative magnetotail characteristics of different magnetospheric states
title_fullStr Quantitative magnetotail characteristics of different magnetospheric states
title_full_unstemmed Quantitative magnetotail characteristics of different magnetospheric states
title_sort quantitative magnetotail characteristics of different magnetospheric states
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2004-03-01
description Quantitative relationships allowing one to compute the lobe magnetic field, flaring angle and tail radius, and to evaluate magnetic flux based on solar wind/IMF parameters and spacecraft position are obtained for the middle magnetotail, <i>X</i>=(–15,–35)<i>R<sub>E</sub></i>, using 3.5 years of simultaneous Geotail and Wind spacecraft observations. For the first time it was done separately for different states of magnetotail including the substorm onset (SO) epoch, the steady magnetospheric convection (SMC) and quiet periods (Q). In the explored distance range the magnetotail parameters appeared to be similar (within the error bar) for Q and SMC states, whereas at SO their values are considerably larger. In particular, the tail radius is larger by 1–3 <i>R<sub>E</sub></i> at substorm onset than during Q and SMC states, for which the radius value is close to previous magnetopause model values. The calculated lobe magnetic flux value at substorm onset is ~1GWb, exceeding that at Q (SMC) states by ~50%. The model magnetic flux values at substorm onset and SMC show little dependence on the solar wind dynamic pressure and distance in the tail, so the magnetic flux value can serve as an important discriminator of the state of the middle magnetotail.<br><br> <b>Key words.</b> Magnetospheric physics (solar windmagnetosphere- interactions, magnetotail, storms and substorms)
url https://www.ann-geophys.net/22/1019/2004/angeo-22-1019-2004.pdf
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AT vasergeev quantitativemagnetotailcharacteristicsofdifferentmagnetosphericstates
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