中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Variability of the behavior of the bottomside (B0, B1) parameters obtained from the ground-based ionograms at China's low latitude station

文献类型:期刊论文

作者Zhang, M. -L.1; Wan, W.1; Liu, L.1; Shi, J. K.2
刊名ADVANCES IN SPACE RESEARCH
出版日期2008-08-18
卷号42期号:4页码:695-702
关键词low latitude ionosphere ionospheric variability IRI model ionospheric modeling
ISSN号0273-1177
DOI10.1016/j.asr.2007.07.022
文献子类Article
英文摘要In this paper, data of (B0, B1) parameters deduced from the electron density profiles that are inverted from the ionograms recorded at Hainan (19.4 degrees N, 109.0 degrees E), China during a three year period from March 2002 to February 2005 are used to study the diurnal and seasonal variation of (B0, B1) parameters at low latitude. The observational results are compared with the IR12001 model predictions. Variability study of (B0, B1) in terms of percentage ratio of the inter-quartiles to the median values and correlative analysis between (B0, B 1) parameters and other ionospheric characteristics such as hmF2 and M(3000)F2 are also made. Our present study showed that: (1) for daytime hours, the IR12001 model results with new table option (B0_Tab) is in a better agreement with the observational results (B0_Obs) than the JR12001 model results with Gulyaeva option (B0_Gul) for summer season, whereas B0_Gul is in a better agreement with B0_Obs than B0_Tab for winter season. For nighttime, in general, B0_Gul is in a better agreement with B0_Obs than B0_Tab. For other occasions, both B0_Tab and B0_Gul showed some systematic deviations from the observational ones. Moreover, the deviations of B0_Tab and B0_Gul from B0_Obs showed opposite trends; (2) the monthly upper (lower) quartiles of (B0, B1) parameter showed a good linear relationship with the monthly median values, this makes it possible to do the regression analysis between the monthly upper (lower) quartiles and the monthly median values, which can give a measure of the variability of these parameters. In terms of the percentage ratio of the inter-quartiles to the median values, the variability of 130 showed a diurnal variation ranging between 22% and 36% with maximum value occurring at pre-sunrise hours, whereas the variability of B1 showed a diurnal variation ranging between 15% and 30% with higher value by daytime than at night; (3) B0 shows high linear correlative relationships with hmF2 and M(3000)F2 for most of the local time period of a day except for a few hours around midnight, whereas B1 showed high linear correlations with B0, hmF2 for daytime hours, but not for nighttime hours. This suggests that it maybe is possible to obtain the synthetic database of (B0, B1) parameter or to construct the model of (B0, B1) using database of hmF2 or M(3000)F2 which is much easier to obtain from experimental measurements. (c) 2007 COSPAR. Published by Elsevier Ltd. All rights reserved.
WOS关键词INTERNATIONAL REFERENCE IONOSPHERE ; PROFILE PARAMETERS ; IRI-2001 MODEL ; SOLAR-ACTIVITY ; MIDLATITUDE
WOS研究方向Astronomy & Astrophysics ; Geology ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000258127000013
出版者ELSEVIER SCI LTD
源URL[http://ir.iggcas.ac.cn/handle/132A11/68734]  
专题中国科学院地质与地球物理研究所
通讯作者Zhang, M. -L.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Ctr Space Sci & Appl Res, Key Lab Space Weather, Beijing 100080, Peoples R China
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Zhang, M. -L.,Wan, W.,Liu, L.,et al. Variability of the behavior of the bottomside (B0, B1) parameters obtained from the ground-based ionograms at China's low latitude station[J]. ADVANCES IN SPACE RESEARCH,2008,42(4):695-702.
APA Zhang, M. -L.,Wan, W.,Liu, L.,&Shi, J. K..(2008).Variability of the behavior of the bottomside (B0, B1) parameters obtained from the ground-based ionograms at China's low latitude station.ADVANCES IN SPACE RESEARCH,42(4),695-702.
MLA Zhang, M. -L.,et al."Variability of the behavior of the bottomside (B0, B1) parameters obtained from the ground-based ionograms at China's low latitude station".ADVANCES IN SPACE RESEARCH 42.4(2008):695-702.

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来源:地质与地球物理研究所

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