EGU2020-381
https://doi.org/10.5194/egusphere-egu2020-381
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

The nighttime poleward wind responses to SAPS simulated by TIEGCM: a universal time effect

Kedeng Zhang1, Hui Wang1, Wenbin Wang2, Jing Liu2, Shunrong Zhang3, and Cheng Sheng4
Kedeng Zhang et al.
  • 1Wuhan University, Electronic Information School, Department of Space Physics, Wuhan, China (ninghe_zkd@whu.edu.cn)
  • 2High Altitude Observatory, National Center for Atmospheric Research, Boulder, Colorado, USA
  • 3Haystack Observatory, Massachusetts Institute of Technology, Westford, Massachusetts, USA
  • 4Department of Physics, University of Texas at Arlington, Arlington, Texas, USA

The present work investigates the nighttime meridional wind (30º-50º magnetic latitude and 19-22 magnetic local time) in response to subauroral polarization streams (SAPS) that commence at different universal time (UT) by using Thermosphere Ionosphere Electrodynamics General Circulation Model (TIEGCM) under geomagnetically disturbed conditions that are closely related to the southward interplanetary magnetic field (IMF) carried by the solar wind. The SAPS effects on the meridional winds show a remarkable UT variation, with larger 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 the 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 to a large component of ion drag in geographically northward (southward) direction due to the SAPS channel orientation 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.

How to cite: Zhang, K., Wang, H., Wang, W., Liu, J., Zhang, S., and Sheng, C.: The nighttime poleward wind responses to SAPS simulated by TIEGCM: a universal time effect, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-381, https://doi.org/10.5194/egusphere-egu2020-381, 2019

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