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Surveys on magnetospheric plasmas based on the Double Star Project (DSP) exploration
Shen, C.; Liu, Z. X.; Escoubet, C. P.; Carr, C. M.; Reme, H.; Fazakerley, A.; Laakso, H.; Shi, Q. Q.; Dandouras, I.; Zhang, T. L.; Wang, S. J.; Yang, X. C.; Dunlop, M.; Cao, J. B.; 北京8701信箱
Department空间天气学国家重点实验室
Source PublicationScience in China Series E-Technological Sciences
2008
Volume51Issue:10Pages:1639-1647
ISSN1006-9321
Language英语
KeywordEarth's Magnetosphere Space Exploration Geomagnetic Field Space Plasmas Spacecraft Instrument
AbstractThe equatorial and polar satellites of the Double Star Project (DSP) were launched successfully on December 29, 2003 and July 25, 2004, respectively, and both of them are operating smoothly. The DSP provides a good opportunity for investigating the structure of the magnetosphere. Based on the DSP data collected during 2004, we have surveyed the distribution of the magnetic fields and plasmas in the magnetosphere. It is found that: (1) Near the Earth's equatorial plane within geocentric distances of less than 7 RE, the Earth's magnetic field is dipolar. In the vicinity of the magnetopause, the magnetic field is enhanced by a factor of about 1.5, and on the nightside, the magnetic field can vary significantly from the Earth's dipole field, likely caused by the presence of the near-Earth tail current sheet. (2) In the day-side magnetosheath, the electron and ion densities are usually both in the range of 10-30 cm(-3); the ion and electron temperatures are usually about 200 and 50 eV, respectively. The flow pattern is usually smooth, with a low velocity in the subsolar region and with significantly higher velocities in the dawn and dusk flanks. (3) In the region between the magnetopause and plasmasphere the density is low, approximately 0.5-5 cm(-3), and the temperature is high, about 1-10 keV for ions and 0.1-5 keV for electrons. The ion temperature has an apparent anisotropy, with the ratio of the perpendicular and parallel temperatures being about 1.0-1.3 for the night- and dusk-side magnetosphere and about 1.3-2.0 for the day- and dawn-side magnetosphere. There is an evident sunward convection of about 50 km/s in the magnetosphere. On the dawn side, the flow becomes somewhat turbulent, and in the vicinity of the night-noon meridian plane, the convection is rather slow. (4) The high-energy electrons with energies higher than 2 MeV are mainly located in the regions with 3 < L < 4.5; the size of the high-energy electrons area varies with time, it may expand and shrink occasionally according to different solar wind conditions and magnetic activities.
Indexed BySCI
Funding Project中国科学院空间科学与应用研究中心
Document Type期刊论文
Identifierhttp://ir.nssc.ac.cn/handle/122/1108
Collection空间科学部
Corresponding Author北京8701信箱
Recommended Citation
GB/T 7714
Shen, C.,Liu, Z. X.,Escoubet, C. P.,et al. Surveys on magnetospheric plasmas based on the Double Star Project (DSP) exploration[J]. Science in China Series E-Technological Sciences,2008,51(10):1639-1647.
APA Shen, C..,Liu, Z. X..,Escoubet, C. P..,Carr, C. M..,Reme, H..,...&北京8701信箱.(2008).Surveys on magnetospheric plasmas based on the Double Star Project (DSP) exploration.Science in China Series E-Technological Sciences,51(10),1639-1647.
MLA Shen, C.,et al."Surveys on magnetospheric plasmas based on the Double Star Project (DSP) exploration".Science in China Series E-Technological Sciences 51.10(2008):1639-1647.
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