On the Magnetic Field Configuration of the Magnetosheath

The magnetosheath is the region where the shocked solar wind interacts directly with the magnetosphere. Here we examine the magnetic field throughout the equatorial magnetosheath as a function of the solar wind IMF direction using observational data sets (Geotail and Wind) spanning 9.5 years. In gen...

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Main Author: Steven Michael Petrinec
Format: Article
Language:English
Published: Springer 2013-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v242p265.pdf
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author Steven Michael Petrinec
author_facet Steven Michael Petrinec
author_sort Steven Michael Petrinec
collection DOAJ
description The magnetosheath is the region where the shocked solar wind interacts directly with the magnetosphere. Here we examine the magnetic field throughout the equatorial magnetosheath as a function of the solar wind IMF direction using observational data sets (Geotail and Wind) spanning 9.5 years. In general, the synoptic maps of the magnetosheath magnetic field are in agreement with the predictions of Rankine-Hugoniot conditions at the bow shock and with global numerical models. Qualitative comparisons with recent analytic magnetosheath magnetic field models are also performed and show that the compression of the magnetosheath magnetic field between the two boundaries (bow shock and magnetopause) used in such models is greater than that which is observed.
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spelling doaj.art-a2681aeec5c4413fb37f0f868f11f5b72022-12-22T02:27:07ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802013-01-0124226510.3319/TAO.2012.10.17.02(SEC)1130On the Magnetic Field Configuration of the MagnetosheathSteven Michael PetrinecThe magnetosheath is the region where the shocked solar wind interacts directly with the magnetosphere. Here we examine the magnetic field throughout the equatorial magnetosheath as a function of the solar wind IMF direction using observational data sets (Geotail and Wind) spanning 9.5 years. In general, the synoptic maps of the magnetosheath magnetic field are in agreement with the predictions of Rankine-Hugoniot conditions at the bow shock and with global numerical models. Qualitative comparisons with recent analytic magnetosheath magnetic field models are also performed and show that the compression of the magnetosheath magnetic field between the two boundaries (bow shock and magnetopause) used in such models is greater than that which is observed. http://tao.cgu.org.tw/images/attachments/v242p265.pdf MagnetosheathBow shockMHD discontinuitiesMagnetopause
spellingShingle Steven Michael Petrinec
On the Magnetic Field Configuration of the Magnetosheath
Terrestrial, Atmospheric and Oceanic Sciences
Magnetosheath
Bow shock
MHD discontinuities
Magnetopause
title On the Magnetic Field Configuration of the Magnetosheath
title_full On the Magnetic Field Configuration of the Magnetosheath
title_fullStr On the Magnetic Field Configuration of the Magnetosheath
title_full_unstemmed On the Magnetic Field Configuration of the Magnetosheath
title_short On the Magnetic Field Configuration of the Magnetosheath
title_sort on the magnetic field configuration of the magnetosheath
topic Magnetosheath
Bow shock
MHD discontinuities
Magnetopause
url http://tao.cgu.org.tw/images/attachments/v242p265.pdf
work_keys_str_mv AT stevenmichaelpetrinec onthemagneticfieldconfigurationofthemagnetosheath