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• W2116452981 endingPage "7296" @default.
• W2116452981 startingPage "7281" @default.
• W2116452981 abstract "Abstract By performing a global magnetohydrodynamic (MHD) simulation, we have demonstrated for the first time that an electrojet at the dayside magnetic equator can be reversed and an overshielding condition can be established in the inner magnetosphere after substorm onset without northward turning of the interplanetary magnetic field. Near the substorm onset, the plasma pressure is highly enhanced in the inner magnetosphere on the nightside. The Region 2 field‐aligned current diverges from the diamagnetic current on the surface of the dayside extension of the high‐pressure region, which is connected to the ionosphere in the relatively low‐conductivity region a few degrees equatorward of the main auroral oval that is formed as the projection of the plasma sheet. The separation of the equatorward boundary of the auroral region and the equatorward boundary of the Region 2 current results in dusk‐dawn electric fields that generate a counter electrojet (CEJ) at the dayside magnetic equator. Poleward electric fields in a narrow latitudinal width, which may be regarded as subauroral ion drift and subauroral polarization stream, are simultaneously intensified. The dusk‐dawn electric fields may propagate to the inner magnetosphere along a field line as shear Alfvén waves. Then, the inner magnetosphere is completely constrained by the overshielding condition. The intensity and polarity of the CEJ depend largely on at least the ionospheric conductivity that is related to the plasma pressure (probably associated with diffuse aurora). This may explain the observational fact that overshielding does not always occur after onset." @default.
• W2116452981 created "2016-06-24" @default.
• W2116452981 creator A5004527387 @default.
• W2116452981 creator A5004899555 @default.
• W2116452981 creator A5054691687 @default.
• W2116452981 date "2014-09-01" @default.
• W2116452981 modified "2023-10-10" @default.
• W2116452981 title "Counter equatorial electrojet and overshielding after substorm onset: Global MHD simulation study" @default.
• W2116452981 cites W1515329070 @default.
• W2116452981 cites W1528847393 @default.
• W2116452981 cites W1532053572 @default.
• W2116452981 cites W1928710271 @default.
• W2116452981 cites W1958328415 @default.
• W2116452981 cites W1965521228 @default.
• W2116452981 cites W1965611677 @default.
• W2116452981 cites W1966563658 @default.
• W2116452981 cites W1966856590 @default.
• W2116452981 cites W1969113607 @default.
• W2116452981 cites W1970513636 @default.
• W2116452981 cites W1971790441 @default.
• W2116452981 cites W1971920394 @default.
• W2116452981 cites W1973970316 @default.
• W2116452981 cites W1975715418 @default.
• W2116452981 cites W1977161621 @default.
• W2116452981 cites W1977271084 @default.
• W2116452981 cites W1977770729 @default.
• W2116452981 cites W1980720319 @default.
• W2116452981 cites W1982564903 @default.
• W2116452981 cites W1982903954 @default.
• W2116452981 cites W1982984903 @default.
• W2116452981 cites W1985183210 @default.
• W2116452981 cites W1985229723 @default.
• W2116452981 cites W1985856830 @default.
• W2116452981 cites W1989189152 @default.
• W2116452981 cites W1989429621 @default.
• W2116452981 cites W1993572102 @default.
• W2116452981 cites W2000986159 @default.
• W2116452981 cites W2001379484 @default.
• W2116452981 cites W2003679820 @default.
• W2116452981 cites W2006321605 @default.
• W2116452981 cites W2010031777 @default.
• W2116452981 cites W2011329375 @default.
• W2116452981 cites W2011598811 @default.
• W2116452981 cites W2012222069 @default.
• W2116452981 cites W2012472528 @default.
• W2116452981 cites W2012985101 @default.
• W2116452981 cites W2013104913 @default.
• W2116452981 cites W2013393618 @default.
• W2116452981 cites W2014713407 @default.
• W2116452981 cites W2020108213 @default.
• W2116452981 cites W2025260803 @default.
• W2116452981 cites W2026253822 @default.
• W2116452981 cites W2030741823 @default.
• W2116452981 cites W2032024005 @default.
• W2116452981 cites W2036261181 @default.
• W2116452981 cites W2036307648 @default.
• W2116452981 cites W2037912732 @default.
• W2116452981 cites W2042646605 @default.
• W2116452981 cites W2045201401 @default.
• W2116452981 cites W2045516402 @default.
• W2116452981 cites W2046465620 @default.
• W2116452981 cites W2047170888 @default.
• W2116452981 cites W2052012982 @default.
• W2116452981 cites W2055489564 @default.
• W2116452981 cites W2056077897 @default.
• W2116452981 cites W2058237910 @default.
• W2116452981 cites W2064765069 @default.
• W2116452981 cites W2065116016 @default.
• W2116452981 cites W2067608175 @default.
• W2116452981 cites W2073886560 @default.
• W2116452981 cites W2073970885 @default.
• W2116452981 cites W2077475039 @default.
• W2116452981 cites W2083372669 @default.
• W2116452981 cites W2087972095 @default.
• W2116452981 cites W2090065735 @default.
• W2116452981 cites W2091980246 @default.
• W2116452981 cites W2100821995 @default.
• W2116452981 cites W2105782571 @default.
• W2116452981 cites W2117233461 @default.
• W2116452981 cites W2118703271 @default.
• W2116452981 cites W2122980079 @default.
• W2116452981 cites W2124287763 @default.
• W2116452981 cites W2127587635 @default.
• W2116452981 cites W2127610356 @default.
• W2116452981 cites W2128022129 @default.
• W2116452981 cites W2139172392 @default.
• W2116452981 cites W2140923705 @default.
• W2116452981 cites W2145951254 @default.
• W2116452981 cites W2151296816 @default.
• W2116452981 cites W2152488614 @default.
• W2116452981 cites W2155225394 @default.
• W2116452981 cites W2159841850 @default.
• W2116452981 cites W2162127492 @default.
• W2116452981 cites W2171392479 @default.
• W2116452981 doi "https://doi.org/10.1002/2014ja020065" @default.
• W2116452981 hasPublicationYear "2014" @default.
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