Multiple responses of magnetotail to the enhancement and fluctuation of solar wind dynamic pressure and the southward turning of interplanetary magnetic field
文献类型:期刊论文
作者 | Li, L. Y.; Cao, J. B.; Zhou, G. C.; Zhang, T. L.; Zhang, D.; Dandouras, I.; Reme, H.; Carr, C. M. |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS |
出版日期 | 2011 |
卷号 | 116页码:A12223 |
ISSN号 | 0148-0227 |
通讯作者 | Li, LY (reprint author), Beihang Univ, Sch Astronaut, Beijing 100191, Peoples R China. |
中文摘要 | During the interval from 06:15 to 07:30 UT on 24 August 2005, the Chinese Tan-Ce 1 (TC1) satellite observed the multiple responses of the near-Earth magnetotail to the combined changes in solar wind dynamic pressure and interplanetary magnetic field (IMF). The magnetotail was highly compressed by a strong interplanetary shock because of the dynamic pressure enhancement (similar to 15 nPa), and the large shrinkage of magnetotail made a northern lobe and plasma mantle move inward to the position of the inbound TC1 that was initially in the plasma sheet. Meanwhile, the dynamic pressure fluctuations (similar to 0.5-3 nPa) behind the shock drove the quasi-periodic oscillations of the magnetopause, lobe-mantle boundary, and geomagnetic field at the same frequencies: one dominant frequency was around 3 mHz and the other was around 5 mHz. The quasi-periodic oscillations of the lobe-mantle boundary caused the alternate entries of TC1 into the northern lobe and the plasma mantle. In contrast to a single squeezed or deformed magnetotail by a solar wind discontinuity moving tailward, the compressed and oscillating magnetotail can better indicate the dynamic evolution of magnetotail when solar wind dynamic pressure increases and fluctuates remarkably, and the near-Earth magnetotail is quite sensitive even to some small changes in the solar wind dynamic pressure when it is highly compressed. Furthermore, it is found that a considerable amount of oxygen ions (O(+)) appeared in the lobe after the southward turning of IMF. |
英文摘要 | During the interval from 06:15 to 07:30 UT on 24 August 2005, the Chinese Tan-Ce 1 (TC1) satellite observed the multiple responses of the near-Earth magnetotail to the combined changes in solar wind dynamic pressure and interplanetary magnetic field (IMF). The magnetotail was highly compressed by a strong interplanetary shock because of the dynamic pressure enhancement (similar to 15 nPa), and the large shrinkage of magnetotail made a northern lobe and plasma mantle move inward to the position of the inbound TC1 that was initially in the plasma sheet. Meanwhile, the dynamic pressure fluctuations (similar to 0.5-3 nPa) behind the shock drove the quasi-periodic oscillations of the magnetopause, lobe-mantle boundary, and geomagnetic field at the same frequencies: one dominant frequency was around 3 mHz and the other was around 5 mHz. The quasi-periodic oscillations of the lobe-mantle boundary caused the alternate entries of TC1 into the northern lobe and the plasma mantle. In contrast to a single squeezed or deformed magnetotail by a solar wind discontinuity moving tailward, the compressed and oscillating magnetotail can better indicate the dynamic evolution of magnetotail when solar wind dynamic pressure increases and fluctuates remarkably, and the near-Earth magnetotail is quite sensitive even to some small changes in the solar wind dynamic pressure when it is highly compressed. Furthermore, it is found that a considerable amount of oxygen ions (O(+)) appeared in the lobe after the southward turning of IMF. |
学科主题 | 空间物理 |
资助信息 | NSFC [41074119, 40604018, 41174141]; State Science and Technology Sustentation Program [2008BAC35B02-1]; 973 Program [2011CB811404]; State Key Laboratories; Space Research Institute of the Austrian Academy of Sciences |
收录类别 | SCI |
语种 | 英语 |
公开日期 | 2014-12-15 |
源URL | [http://ir.nssc.ac.cn/handle/122/3224] |
专题 | 国家空间科学中心_空间科学部 |
推荐引用方式 GB/T 7714 | Li, L. Y.,Cao, J. B.,Zhou, G. C.,et al. Multiple responses of magnetotail to the enhancement and fluctuation of solar wind dynamic pressure and the southward turning of interplanetary magnetic field[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS,2011,116:A12223. |
APA | Li, L. Y..,Cao, J. B..,Zhou, G. C..,Zhang, T. L..,Zhang, D..,...&Carr, C. M..(2011).Multiple responses of magnetotail to the enhancement and fluctuation of solar wind dynamic pressure and the southward turning of interplanetary magnetic field.JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS,116,A12223. |
MLA | Li, L. Y.,et al."Multiple responses of magnetotail to the enhancement and fluctuation of solar wind dynamic pressure and the southward turning of interplanetary magnetic field".JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS 116(2011):A12223. |
入库方式: OAI收割
来源:国家空间科学中心
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