GOLD 和 SABER 对 2023 年 4 月 23-24 日地磁风暴热层成分和温度响应的同步观测

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Xuguang Cai, Wenbin Wang, Richard W. Eastes, Liying Qian, Martin G. Mlynczak, J. S. Evans, Ningchao Wang, Nabil Nowak, Nicholas Pedatella, Kun Wu
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引用次数: 0

摘要

利用全球尺度肢盘观测(GOLD)和利用宽带发射辐射测量法探测大气层(SABER)仪器调查了热层成分和温度对2023年4月23日至24日地磁风暴的响应。全球尺度肢体和星盘观测观测到,4 月 24 日世界时(UT)12 点风暴结束后,南半球(SH)热大气层 O 与 N2 的柱密度比(ΣO/N2)恢复较快。4 月 25 日世界时 12 点之后,两个半球的 ΣO/N2 已基本恢复。在 4 月 24 日风暴结束后的 4-6 小时内,北纬 30 度至 60 度、西经 100 度至西经 30 度之间的热层温度持续上升,而在西经 45 度至西经 15 度、南纬 40 度至北纬 50 度之间的热层温度低于风暴前的静止日(4 月 17 日)。西经 100 度和西经 45 度、北纬 30 度和南纬 55 度之间的 Tdisk 有所恢复。此外,太阳辐照度从 4 月 17 日到 25 日下降了 15%-20%,这表明 4 月 25 日较低的 Tdisk 来自风暴和太阳辐照度的变化。Tdisk和SABER观测到的一氧化氮(NO)冷却率的纬度变化表明,4月25日一氧化氮冷却是北半球中高纬度地区Tdisk较低的关键因素。这些结果提供了直接证据,表明风暴恢复阶段的热层温度比风暴前的平静时期要低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Concurrent GOLD and SABER Observations of Thermosphere Composition and Temperature Responses to the April 23–24, 2023 Geomagnetic Storm

The Global-scale Observations of Limb and Disk (GOLD) and Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) instruments were used to investigate the thermospheric composition and temperature responses to the geomagnetic storm on 23–24 April, 2023. Global-scale Observations of Limb and Disk observed a faster recovery of thermospheric column density ratio of O to N2 (ΣO/N2) in the southern hemisphere (SH) after the storm ended at 12 Universal time (UT) on 24 April. After 12 UT on 25 April, ΣO/N2 had mostly recovered in both hemispheres. Global-scale Observations of Limb and Disk also observed an increase of middle thermospheric temperature (140–200 km) (Tdisk) on 24 April with a maximum of 340 K. Within 4–6 hr of the storm ending on 24 April, Tdisk enhancement persisted between 30°N and 60°N, 100°W and 30°W, while Tdisk lower than pre-storm quiet day (17 April) was observed between 45°W and 15°W, 40°S and 50°N. Tdisk recovered between 100°W and 45°W, 30°N and 55°S. On 25 April, Tdisk was lower than on 17 April across the entire GOLD Field-of-Regard (FOR) by ∼50–110 K. Additionally, solar irradiance decreased by 15%–20% from 17 to 25 April, indicating that the lower Tdisk on 25 April resulted from both storm and solar irradiance variations. Latitudinal variations of Tdisk and the SABER observed Nitric Oxide (NO) cooling rate revealed that NO cooling is crucial for the lower Tdisk in the northern hemisphere (NH) mid-high latitudes on 25 April. These results provide direct evidence of decreased thermospheric temperature during storm recovery phase than pre-storm quiet times.

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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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