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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Online Access: | https://www.ann-geophys.net/16/376/1998/angeo-16-376-1998.pdf |
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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 |
work_keys_str_mv |
AT zkaymaz imp8magnetosheathfieldcomparisonswithmodels |
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1725503606196535296 |