| 大气掩星反演误差特性初步分析 |
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| 引用本文： | 宫晓艳,胡雄,吴小成,张训械.大气掩星反演误差特性初步分析[J].地球物理学报,2007,50(4):1017-1029. |
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| 作者姓名： | 宫晓艳 胡雄 吴小成 张训械 |
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| 作者单位： | 1.中国科学院空间科学与应用研究中心，北京100080 2 中国科学院研究生院，北京 100049 3 中国科学院武汉物理与数学研究所，武汉 430071 |
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| 基金项目： | 国家自然科学基金(40204011)，中国科学院知识创新方向性项目(KGCX2-SW-408)资助. |
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| 摘 要： | GPS大气掩星探测技术可以获得全球大气折射率、气压、密度、温度和水汽压等气象参数，该技术基本原理是基于几何光学近似的Abel积分反演.地球扁率、电离层传播时间延迟、大气大尺度水平梯度、多路径传播现象等因素在某些高度范围影响大气反演的精度.本文采用模拟的方法，分析其中地球扁率及电离层对反演结果的影响，并讨论局部圆弧修正及电离层修正的效果.利用CHAMP掩星实测轨道数据和有关电离层和大气经验模式、采用三维射线追踪方法模拟计算几种情形下的GPS掩星观测附加相位数据，对模拟数据进行反演，将反演气象参量剖面与模拟时给定模式剖面进行比较，得到了0～60 km高度范围内的反演误差.误差统计分析结果表明，局部圆弧中心的修正以及电离层修正，对于高精度的GPS掩星反演是非常重要的；电离层修正残差仍是制约30～60 km高度范围内反演精度的重要因素，进一步完善和优化大气掩星反演需要发展新的电离层修正算法.
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| 关 键 词： | GPS 大气掩星 地球扁率 电离层修正 几何光学反演方法 反演误差 |
| 文章编号： | 0001-5733（2007）04-1017-13 |
| 收稿时间： | 2006-5-27 |
| 修稿时间： | 2006-05-27 |
Preliminary analysis of error characteristics in atmospheric inversion of GPS radio occultation |
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| GONG Xiao-Yan,HU Xiong,WU Xiao-Cheng,ZHANG Xun-Xie.Preliminary analysis of error characteristics in atmospheric inversion of GPS radio occultation[J].Chinese Journal of Geophysics,2007,50(4):1017-1029. |
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| Authors: | GONG Xiao-Yan HU Xiong WU Xiao-Cheng ZHANG Xun-Xie |
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| Institution: | 1.Center for Space Science and Applied Research, Chinese Academy of Sciences, Beijing 100080, China 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China 3 Wuhan Institute of Physics and Mathematics, Chinese Academy of Sciences, Wuhan 430071, China |
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| Abstract: | GPS radio atmospheric occultation technique can measure the profiles of the global meteorological fields of the neutral atmosphere, from which we can obtain the atmosphere refractivity, pressure, density, temperature, and water vapor. The basic theory of the technique is the inversion method of Abel integration. Some factors such as the Earth's oblateness, the ionospheric dalay, the large-scale horizontal refractive index gradients in the atmosphere,and atmospheric multipath can influence the precision of retrieval. In this paper, we discuss the effect of the Earth's oblateness and ionosphere on the retrieval, and analyze the result of the local curvature correction and the ionosphere calibration. The excess phase delay is simulated by using the observed CHAMP orbit data, the ionospheric model and experiential atmospheric model, and the method of 3D-tracing technology. Inversion errors of the height from 0 to 60 km are obtained by comparison of the retrieval parameter profile and model profile, and studied by using statistical methods for several occultations. The result shows that local curvature calibration and ionosphere calibration are very important for GPS occultation inversion of high precision. Ionospheric residual influence is the main reason of restricting the retrieval precision from 30 km to 60 km, and it is necessary to develop new ionosphere calibration methods for atmosphere inversion of higher precision. |
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| Keywords: | GPS Atmospheric occultation The Earth's oblateness Ionosphere calibration Inversion method of geometric optics Inversion error |
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