IMP 8 magnetosheath field comparisons with models

This study presents cross-sectional vector maps of the magnetic field derived from IMP 8 magnetometer in the magnetosheath at 30 R<sub>e</sub> behind the Earth. In addition the vector patterns of the magnetosheath field for northward, southward, and east-west interplanetary magnetic...

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Main Author: Z. Kaymaz
Format: Article
Language:English
Published: Copernicus Publications 1998-04-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/16/376/1998/angeo-16-376-1998.pdf
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spelling doaj-b6f2e3539ef94e3d8f73599795391a742020-11-24T23:42:39ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761998-04-011637638710.1007/s00585-998-0376-3IMP 8 magnetosheath field comparisons with modelsZ. Kaymaz0Istanbul Technical University, Faculty of Aeronautics and Astronautics, Maslak, 80626, Istanbul, TurkeyThis study presents cross-sectional vector maps of the magnetic field derived from IMP 8 magnetometer in the magnetosheath at 30 R<sub>e</sub> behind the Earth. In addition the vector patterns of the magnetosheath field for northward, southward, and east-west interplanetary magnetic field (IMF) directions are qualitatively compared with those obtained from the Spreiter-Stahara gas dynamic (GD) and Fedder-Lyon magnetohydrodynamic models (MHD). The main purpose is to display the cross-sectional differences in relation to the dayside merging with different IMF directions, allowing the reader to make direct visual comparisons of the vector patterns. It is seen that for east-west IMF directions, the data-based and MHD-based patterns differ noticeably in a similar way from the GD model, presumably reflecting the influence of dayside magnetic merging of the Earth's magnetic field with the y-component of the interplanetary magnetic field. All three northward IMF cross sections show comparable field draping patterns as expected for a closed magnetosphere. For southward IMF case, on the other hand, differences between the three cross-sectional patterns are greater as seen in the field vector sizes and directions, especially closer to the magnetopause where more disturbed magnetospheric conditions are known to be exist. The data comparisons with the MHD and GD models show that the differences result from the magnetic field-flow coupling and that the effects of dayside reconnection are present in IMP 8 magnetic field measurements.<br><br><b>Keywords.</b> Vector maps · IMP 8 magnetometer · Inter-planetary magnetic fieldshttps://www.ann-geophys.net/16/376/1998/angeo-16-376-1998.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Z. Kaymaz
spellingShingle Z. Kaymaz
IMP 8 magnetosheath field comparisons with models
Annales Geophysicae
author_facet Z. Kaymaz
author_sort Z. Kaymaz
title IMP 8 magnetosheath field comparisons with models
title_short IMP 8 magnetosheath field comparisons with models
title_full IMP 8 magnetosheath field comparisons with models
title_fullStr IMP 8 magnetosheath field comparisons with models
title_full_unstemmed IMP 8 magnetosheath field comparisons with models
title_sort imp 8 magnetosheath field comparisons with models
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 1998-04-01
description This study presents cross-sectional vector maps of the magnetic field derived from IMP 8 magnetometer in the magnetosheath at 30 R<sub>e</sub> behind the Earth. In addition the vector patterns of the magnetosheath field for northward, southward, and east-west interplanetary magnetic field (IMF) directions are qualitatively compared with those obtained from the Spreiter-Stahara gas dynamic (GD) and Fedder-Lyon magnetohydrodynamic models (MHD). The main purpose is to display the cross-sectional differences in relation to the dayside merging with different IMF directions, allowing the reader to make direct visual comparisons of the vector patterns. It is seen that for east-west IMF directions, the data-based and MHD-based patterns differ noticeably in a similar way from the GD model, presumably reflecting the influence of dayside magnetic merging of the Earth's magnetic field with the y-component of the interplanetary magnetic field. All three northward IMF cross sections show comparable field draping patterns as expected for a closed magnetosphere. For southward IMF case, on the other hand, differences between the three cross-sectional patterns are greater as seen in the field vector sizes and directions, especially closer to the magnetopause where more disturbed magnetospheric conditions are known to be exist. The data comparisons with the MHD and GD models show that the differences result from the magnetic field-flow coupling and that the effects of dayside reconnection are present in IMP 8 magnetic field measurements.<br><br><b>Keywords.</b> Vector maps · IMP 8 magnetometer · Inter-planetary magnetic fields
url https://www.ann-geophys.net/16/376/1998/angeo-16-376-1998.pdf
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