Physics
Scientific paper
Dec 2005
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005agufmsm53a..05o&link_type=abstract
American Geophysical Union, Fall Meeting 2005, abstract #SM53A-05
Physics
2736 Magnetosphere/Ionosphere Interactions (2431), 2753 Numerical Modeling, 2784 Solar Wind/Magnetosphere Interactions
Scientific paper
Recent analyses of an isolated solar wind density pulse on 10 January 1997, while the interplanetary electric field remained steady, identified a dramatic increase in the transpolar potential (TP) from 130 to 220 kV. The TP models of neither Weimer nor Siscoe-Hill predict such an increase. However, magnetohydrodynamic (MHD) simulations of the event do predict a TP increase consistent with satellite measurements. The response is transient, decaying on time scales of tens of minutes toward a final equilibrium close to the original potential. The simulated TP enhancement derives from significant erosion of the dayside magnetopause and transport of newly opened magnetic flux across the polar cap. The exponential decay of the TP results from inductance in the magnetosphere-ionosphere circuit. MHD simulation results for different solar wind density increases/decreases will be presented and discussed. The time dependent TP for varying solar wind density conditions can be fairly well described using the dayside merging rate derived from the MHD simulations to power an LR circuit model of the magnetosphere-ionosphere system.
Burke Brian
Maynard Nc.
Ober D.
Siebert K.
Wilson Grant
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