Nighttime meridional neutral wind responses to SAPS simulated by the TIEGCM: A universal time effect

The present work uses the Thermosphere Ionosphere Electrodynamics General Circulation Model (TIEGCM), under geomagnetically disturbed conditions that are closely related to the southward interplanetary magnetic field (IMF), to investigate how the nighttime poleward wind (30 degrees-50 degrees magnetic latitude and 19-22 magnetic local time) responds to subauroral polarization streams (SAPS) that commence at different universal times (UTs). The SAPS effects on the poleward winds show a remarkable UT variation, with weaker magnitudes at 00 and 12 UT than at 06 and 18 UT. The strongest poleward wind emerges when SAPS commence at 06 UT, and the weakest poleward wind develops when SAPS occur at 00 UT. A diagnostic analysis of model results shows that the pressure gradient is more prominent for the developing of the poleward wind at 00 and 12 UT. Meanwhile, the effect of ion drag is important in the modulation of the poleward wind velocity at 06 and 18 UT. This is caused by the misalignment of the geomagnetic and geographic coordinate systems, resulting in a large component of ion drag in the geographically northward (southward) direction due to channel orientation of the SAPS at 06 and 18 UT (00 and 12 UT). The Coriolis force effect induced by westward winds maximizes (minimizes) when SAPS commence at 12 UT (00 UT). The centrifugal force due to the accelerated westward winds shows similar UT variations as the Coriolis force, but with an opposite effect.

Automated summary

This study investigates the effects of SAPS on poleward winds using the TIEGCM model, finding varying responses to SAPS starting at different UTs. Results show that poleward winds are strongest when SAPS commence at 06 UT, and weakest when SAPS occur at 00 UT. Pressure gradient is more prominent for developing poleward winds at 00 and 12 UT, while ion drag plays a crucial role in modulating poleward wind velocity at 06 and 18 UT. The misalignment of geomagnetic and geographic coordinate systems leads to significant ion drag in the northward (southward) direction, affecting the poleward wind velocity.