Physics
Scientific paper
Dec 2010
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010agufmsm41a1838t&link_type=abstract
American Geophysical Union, Fall Meeting 2010, abstract #SM41A-1838
Physics
[2730] Magnetospheric Physics / Magnetosphere: Inner, [2753] Magnetospheric Physics / Numerical Modeling, [2764] Magnetospheric Physics / Plasma Sheet, [2790] Magnetospheric Physics / Substorms
Scientific paper
To investigate the consequences of a localized violation of frozen-in flux in the plasma sheet at the end of a substorm growth phase, we have carried out a series of simulations using the Rice Convection Model Equilibrium (RCM-E) model, which consists of the RCM model coupled to an equilibrium magnetic field. The simulation was started with an RCM-E-computed growth-phase magnetic field that is highly stretched in the inner plasma sheet and has a large region of nearly uniform entropy parameter. Violation of frozen-in flux because of an electric field Ey>0 in the plasma rest frame implies that magnetic field lines slip on the plasma, creating a plasma bubble (region of reduced entropy parameter) just earthward of the disruption and a plasma blob (region of increased entropy) on the tailward side. To represent this in the model, a bubble and blob were imposed on the RCM-E-computed growth-phase configuration, and then the subsequent evolution was followed using the RCM-E. Because the configuration is interchange unstable, the bubble surges earthward, the blob moves tailward, and the z-component of the magnetic field between the bubble and blob decreases significantly, resulting in a thinning of the current sheet and an increase in the cross-tail current density. We will present results of simulations that involve various model scenarios, including one that uses various cross polar cap potential to assess the impact on the bubble/blob motion of the background convection electric field. We speculate that, in the magnetosphere, the positive feedback that results from the bubble-blob pair would cause the current sheet to continue to thin, eventually making the current sheet favorable for reconnection.
Hu Beilai
Toffoletto Frank
Wolf Richard A.
Yang Jaek-Jin
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