Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion

We investigate the ability of the cylindrically symmetric force-free magnetic cloud (MC) fitting model of Lepping et al. (1990) to faithfully reproduce actual magnetic field observations by examining two quantities: (1) a <i>difference angle</i>, called β, i.e., the angle between the...

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Main Authors: R. P. Lepping, T. W. Narock, H. Chen
Format: Article
Language:English
Published: Copernicus Publications 2007-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/25/2641/2007/angeo-25-2641-2007.pdf
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spelling doaj-496c1d2ee4c2497c8a9beff66a031c572020-11-25T00:37:37ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762007-01-01252641264810.5194/angeo-25-2641-2007Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansionR. P. Lepping0T. W. Narock1T. W. Narock2H. Chen3NASA, Goddard Space Flight Center, Heliophysics Science Division, Greenbelt, MD 20771, USAGoddard Earth and Science Technology Center, University of Maryland, Baltimore County, MD, USANASA, Goddard Space Flight Center, Heliophysics Science Division, Greenbelt, MD 20771, USARiver Hill High School, Clarksville MD 21029, USAWe investigate the ability of the cylindrically symmetric force-free magnetic cloud (MC) fitting model of Lepping et al. (1990) to faithfully reproduce actual magnetic field observations by examining two quantities: (1) a <i>difference angle</i>, called β, i.e., the angle between the direction of the observed magnetic field (<i>B<sub>obs</sub></i>) and the derived force free model field (<i>B<sub>mod</sub></i>) and (2) the <i>difference in magnitudes<i> between the observed and modeled fields, i.e., &Delta;<i>B</i>(=|<i>B</i><sub>obs</sub>|&minus;|</i>B</i><sub>mod</sub>|), and a <i>normalized</i> &Delta;<i>B</i> (i.e., &Delta;<i>B</i>/&lt;<i>B</i>&gt;) is also examined, all for a judiciously chosen set of 50 WIND interplanetary MCs, based on quality considerations. These three quantities are developed as a percent of MC duration and averaged over this set of MCs to obtain average profiles. It is found that, although <&Delta;<i>B</i>> and its normalize version are significantly enhanced (from a broad central average value) early in an average MC (and to a lesser extent also late in the MC), the angle <&beta;> is small (less than 8&deg;) and <i>approximately constant</i> all throughout the MC. The field intensity enhancements are due mainly to interaction of the MC with the surrounding solar wind plasma causing field <i>compression</i> at front and rear. For example, for a typical MC, &Delta;<i>B</i>/<<i>B</i>> is: 0.21&plusmn;0.27 very early in the MC, &minus;0.11&plusmn;0.10 at the center (and &minus;0.085&plusmn;0.12 averaged over the full "central region," i.e., for 30% to 80% of duration), and 0.05&plusmn;0.29 very late in the MC, showing a double sign change as we travel from front to center to back, in the MC. When individual MCs are examined we find that over 80% of them possess field enhancements within several to many hours of the front boundary, but only about 30% show such enhancements at their rear portions. The enhancement of the MC's front field is also due to MC expansion, but this is usually a lesser effect compared to compression. It is expected that this compression is manifested as significant distortion to the MC's cross-section from the ideal circle, first suggested by Crooker et al. (1990), into a more elliptical/oval shape, as some global MC studies seem to confirm (e.g., Riley and Crooker, 2004) and apparently also as confirmed for local studies of MCs (e.g., Hidalgo et al., 2002; Nieves-Chinchilla et al., 2005).https://www.ann-geophys.net/25/2641/2007/angeo-25-2641-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. P. Lepping
T. W. Narock
T. W. Narock
H. Chen
spellingShingle R. P. Lepping
T. W. Narock
T. W. Narock
H. Chen
Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
Annales Geophysicae
author_facet R. P. Lepping
T. W. Narock
T. W. Narock
H. Chen
author_sort R. P. Lepping
title Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
title_short Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
title_full Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
title_fullStr Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
title_full_unstemmed Comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
title_sort comparison of magnetic field observations of an average magnetic cloud with a simple force free model: the importance of field compression and expansion
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2007-01-01
description We investigate the ability of the cylindrically symmetric force-free magnetic cloud (MC) fitting model of Lepping et al. (1990) to faithfully reproduce actual magnetic field observations by examining two quantities: (1) a <i>difference angle</i>, called β, i.e., the angle between the direction of the observed magnetic field (<i>B<sub>obs</sub></i>) and the derived force free model field (<i>B<sub>mod</sub></i>) and (2) the <i>difference in magnitudes<i> between the observed and modeled fields, i.e., &Delta;<i>B</i>(=|<i>B</i><sub>obs</sub>|&minus;|</i>B</i><sub>mod</sub>|), and a <i>normalized</i> &Delta;<i>B</i> (i.e., &Delta;<i>B</i>/&lt;<i>B</i>&gt;) is also examined, all for a judiciously chosen set of 50 WIND interplanetary MCs, based on quality considerations. These three quantities are developed as a percent of MC duration and averaged over this set of MCs to obtain average profiles. It is found that, although <&Delta;<i>B</i>> and its normalize version are significantly enhanced (from a broad central average value) early in an average MC (and to a lesser extent also late in the MC), the angle <&beta;> is small (less than 8&deg;) and <i>approximately constant</i> all throughout the MC. The field intensity enhancements are due mainly to interaction of the MC with the surrounding solar wind plasma causing field <i>compression</i> at front and rear. For example, for a typical MC, &Delta;<i>B</i>/<<i>B</i>> is: 0.21&plusmn;0.27 very early in the MC, &minus;0.11&plusmn;0.10 at the center (and &minus;0.085&plusmn;0.12 averaged over the full "central region," i.e., for 30% to 80% of duration), and 0.05&plusmn;0.29 very late in the MC, showing a double sign change as we travel from front to center to back, in the MC. When individual MCs are examined we find that over 80% of them possess field enhancements within several to many hours of the front boundary, but only about 30% show such enhancements at their rear portions. The enhancement of the MC's front field is also due to MC expansion, but this is usually a lesser effect compared to compression. It is expected that this compression is manifested as significant distortion to the MC's cross-section from the ideal circle, first suggested by Crooker et al. (1990), into a more elliptical/oval shape, as some global MC studies seem to confirm (e.g., Riley and Crooker, 2004) and apparently also as confirmed for local studies of MCs (e.g., Hidalgo et al., 2002; Nieves-Chinchilla et al., 2005).
url https://www.ann-geophys.net/25/2641/2007/angeo-25-2641-2007.pdf
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