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Detailed Reference Information |
Pulkkinen, T.I., Baker, D.N., Mitchell, D.G., McPherron, R.L., Huang, C.Y. and Frank, L.A. (1994). Thin current sheets in the magnetotail during substorms: CDAW 6 revisited. Journal of Geophysical Research 99: doi: 10.1029/93JA03234. issn: 0148-0227. |
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The global magnetic field configuration during the growth phase of the CDAW 6 substorm (March 22, 1979, 1054 UT) is modeled using data from two suitably located spacecraft and temporally evolving variations of the Tsyganenko magnetic field model. These results are compared with a local calculation of the current sheet location and thickness carried out by McPherron et al. (1987) and Sanny et al. (this issue). Both models suggest that during the growth phase the current sheet rotated away from its nominal location, and simultaneously thinned strongly. The locations and thicknesses obtained from the two models are in good agreement. The global model suggests that the peak current density is ~120 nA/m2, and that the cross-tail current almost doubled its intensity during this very strong growth phase. The global model predicts a field configuration that is sufficiently stretched to scatter thermal electrons, which may be conducive to the onset of ion tearing in the tail. The electron plasma data further support this scenario, as the anisotropy present in the low-energy electrons disappears close to the substorm onset. The electron contribution to the intensifying current in this case is of the order of 10% before the isotropization of the distribution. ¿ American Geophysical Union 1994 |
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Abstract |
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Keywords
Magnetospheric Physics, Storms and substorms, Magnetospheric Physics, Current systems, Magnetospheric Physics, Magnetospheric configuration and dynamics, Magnetospheric Physics, Magnetotail |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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