• ISSN 2097-1893
    • CN 10-1855/P

    径向行星际磁场对亚极光区极化流半球不对称性的调控

    Radial interplanetary magnetic field modulates hemispheric asymmetry of subauroral polarization streams

    • 摘要: 本研究基于2015—2022年DMSP卫星观测数据,系统探究了行星际磁场(IMF)Bx对亚极光极化流(SAPS)强度及磁纬分布的调控作用,重点分析了不同IMF Bx极性条件下SAPS在南北半球及晨昏侧的响应特征. 结果表明,SAPS对IMF Bx的响应表现出显著的半球不对称性:在黄昏侧,北半球(NH)SAPS在IMF圆锥角 ≥ 135°(IMF Bx < 0)条件下更强,而南半球(SH)SAPS 在IMF圆锥角 ≤ 45°(IMF Bx > 0)条件下更强. 在晨侧,NH SAPS在IMF圆锥角 ≤ 45°时更强,而SH SAPS在IMF圆锥角 ≥ 135°时更强. 进一步分析表明,SAPS的增强并非由场向电流(FACs)峰值电流密度的变化直接决定,而是与FACs的宏观形态改变密切相关,尤其是1区(R1)与2区(R2)电流系统的磁纬间距. 在黄昏侧,R1与R2 FACs间距的扩大导致总积分电流增强,进而驱动更强的极化电场并引起SAPS速度增强;在晨侧,IMF Bx对SAPS的调控主要体现为SAPS强度及其磁纬分布的显著半球不对称性. 此外,黄昏侧电离层离子上行与SAPS表现出一致的半球不对称响应:IMF Bx > 0时南半球离子上行更强,IMF Bx <0时北半球更强,与SAPS的响应模式高度一致,表明SAPS在驱动离子垂直运动中具有重要作用;相比之下,晨侧离子上行对IMF Bx的响应较弱,且与SAPS变化并不完全一致,表明晨昏两侧离子上行的相关物理机制存在差异. 研究结果表明,IMF Bx是调控SAPS半球不对称性的重要驱动因素,为改进空间天气预报模型提供了关键参考.

       

      Abstract: In this study, DMSP satellite observations from 2015–2022 are used to systematically investigate the control of the interplanetary magnetic field (IMF) Bx over the strength and latitude distribution of subauroral polarization streams (SAPS), with particular emphasis on the SAPS response under different IMF Bx polarities in the two hemispheres and in the dusk and dawn sectors. The SAPS response to IMF Bx exhibits a marked hemispheric asymmetry. At dusk, SAPS are stronger in the Northern Hemisphere (NH) under IMF cone angles ≥ 135° (IMF Bx < 0). Conversely, in the Southern Hemisphere (SH), SAPS are stronger under IMF cone angles ≤ 45° (IMF Bx > 0). This hemispheric preference reverses on the dawnside. On the dawnside, NH SAPS is stronger when the IMF cone angle ≤ 45°, while SH SAPS is stronger when the IMF cone angle ≥ 135°. Further analysis indicates that SAPS enhancement is not caused by changes in the peak density of field-aligned currents (FACs), but is closely associated with alterations in their macroscopic morphology, particularly the latitudinal spacing between the Region 1 (R1) and Region 2 (R2) current systems. On the duskside, the widening of the FACs gap leads to an increase in integrated current, which drives a stronger polarization electric field and thus higher SAPS flow velocity. On the dawnside, the influence of IMF Bx on SAPS is mainly manifested as hemispheric asymmetries in SAPS intensity and magnetic latitude distribution. In addition, ion upflow in the duskside ionosphere exhibits a hemispherically asymmetric response consistent with that of SAPS: ion upflow is stronger in the SH under IMF cone angles ≤ 45°, and stronger in the NH under IMF cone angle ≥ 135°. This close correspondence with the SAPS response pattern indicates that SAPS plays an important role in driving vertical ion motion. In contrast, ion upflow on the dawnside shows a weaker response to IMF Bx and is not fully consistent with the SAPS variation, indicating that the physical processes associated with ion upflow differ between the dusk and dawn sectors. These results establish IMF Bx as an important driver of SAPS hemispheric asymmetry, providing critical insights for improving space weather forecasting models.

       

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