在2022年3月13-14日的暴风雨期间,高度中性密度变化的半球间不对称性
Qingyu Zhu1, Gang Lu2, Sarah Vines3
1William B Hanson Center for Space Sciences University of Texas at Dallas Richardson TX USA.
概括
在2022年暴风雨期间观察到强烈的高度中性质量密度异常 (HDAs). 这些由GITM建模的异常揭示了黎明触发的跨极干扰和显著的半球间不对称性.
科学领域:
- 空间物理 空间物理
- 大气科学 大气科学
- 地质物理学 地质物理学
背景情况:
- 强烈的太空天气事件,如地磁风暴,显著影响地球上层大气层.
- 准确建模中性质密度变化对于卫星运行和理解大气动态至关重要.
研究的目的:
- 调查2022年3月暴风雨恢复阶段高度中性质量密度异常 (HDAs) 的性质和起源.
- 分析这些密度变化的半球间不对称性 (IHA) 以及它们与能量沉积和热层条件的关系.
主要方法:
- 利用卫星观测来检测高度的中性质量密度峰值.
- 采用全球电离层热层模型 (GITM) 来准确模拟和分析观察到的现象.
- 调查HDAs,朱尔加热和热层背景条件之间的相关性.
主要成果:
- 在风暴恢复阶段,在两个半球大约500公里处检测到强烈的高度中性质密度尖峰 (HDAs).
- GITM模拟证实HDA是高度中性密度的重要特征,起源于在黎明侧触发的跨极移动大气干扰.
- 在HDA的大小,速度和方向上确定了显著的半球间不对称性 (IHA),与焦尔加热和热层条件中的不对称性有关.
结论:
- HDA是暴风雨时期高度中性密度变化的关键特征.
- 在黎明侧启动的跨极移动大气干扰是产生HDA的原因.
- HDA中的半球间不对称性是由能量沉积和背景热层条件的不对称性驱动的,为太空天气影响提供了一个动态的视角.
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