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A magnetohydrodynamic simulation of reconnection in the magnetotail during intervals with southward interplanetary magnetic fieldResults are reported from a simulation of the interaction between the solar wind and the earth magnetosphere, using a time-dependent three-dimensional MHD model. The calculation was performed for several orientations of the IMF between dawnward pointing and southward. When the IMF has a dawnward component, the plasma sheet rotates northward on the dawnside of the tail and toward the south on the duskside. As the southward component becomes larger, the plasma sheet becomes thinner and develops a wavy cross section because of patchy or localized tail reconnection. The field-aligned currents (FACs) associated with this localized reconnection have a filamentary layered structure. When projected onto the polar cap the filamentary FACs are located in the same region as the tail region 1 currents. At lower latitudes strong region 2 sense currents that originate in the plasma sheet are found. FACs are found on field lines that map to the polar cap even for southward IMF. These currents have many of the properties of the observed polar-cusp currents. The polar-cusp FACs evolve from the polar-cap NB(z) FACs as the IMF is rotated from northward to southward.
Document ID
19880059320
Acquisition Source
Legacy CDMS
Document Type
Conference Proceedings
Authors
Walker, R. J.
(California Univ. Los Angeles, CA, United States)
Ashour-Abdalla, M.
(California, University Los Angeles, United States)
Ogino, T.
(California, University Los Angeles; Nagoya University, Toyokawa, Japan)
Date Acquired
August 13, 2013
Publication Date
January 1, 1987
Subject Category
Geophysics
Accession Number
88A46547
Funding Number(s)
CONTRACT_GRANT: NAGW-78
CONTRACT_GRANT: NSF ATM-82-18746
Distribution Limits
Public
Copyright
Other

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