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磁梯度张量系统测量精度受到单磁传感器系统误差与传感器阵列间非对准误差的严重影响。为了获得精确的张量测量输出，建立了单磁传感器零漂、标度因子与非正交角等系统误差和多传感器轴系间非对准误差的集成数学模型，提出了基于十字磁梯度张量系统最小二乘非线性集成校正方法。相比两步标量校正，利用建立的集成数学模型能够一次性估计出十字形张量系统的48个误差参数，以"人造"平台输出为参考实现低成本矢量校正，极大提高了校正效率和参数估计准确率。仿真和实测表明，张量系统误差参数仿真估计准确率高于99.75%，实验校正后总场输出均方根误差（root mean square error，RMSE）小于2 nT，张量分量RMSE小于50 nT/m，参数估计具有较高的鲁棒性。 相似文献
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回归分析是统计分析中常用的方法之一。传统的回归模型不具备全域分析能力,而变量场之间的关系多采用SVD（Singular Value Decomposition）进行分析,与传统的回归分析有所脱节。更为广义的线性回归模型是传统线性回归模型的延拓,在标量情况下,该模型可转化为传统线性回归模型。该模型的基本特征包含乘法不可互易性、等价于传统线性回归（因子项为标量时）、可分析性、延拓性、降维特征及容错性等。该模型解决了传统的线性回归模型不具备全域分析能力及模型表达能力受限于模型维数的现实问题。本文采用了NCEP（National Centers for Environmental Prediction）降水、高度场、风场月平均资料及国家气候中心西太平洋副热带高压指数资料,利用该模型和传统回归方案进行对比分析,分析结果表明,该模型具有一定的实用参考价值。 相似文献
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利用卫星高度计资料和再分析资料，本文分析研究了东海黑潮强度与东亚冬季风的关系，并初步探讨了二者相互作用的可能机制。结果表明，位置相近的断面，其流强变化具有相似的特征；在年际尺度上，冬季风与东海黑潮存在相互作用。当冬季风偏强，将削弱次年2-4月SC、SD断面的流强，弱冬季风年的情况相反。冬季风对流强影响的动力过程主要通过改变Ekman输送来实现；热力过程则表现为强（弱）冬季风增大（减少）了黑潮向大气释放的热通量，从而削弱（增强）流强，这一过程主要为冬季风对黑潮的影响。当冬季风偏强时，次年10-12月黑潮中下游流强偏弱，弱冬季风年的情况相反。这一过程与2-4月情况不同，其热力过程主要表现为黑潮对冬季风的影响。强冬季风通过准两年振荡对次年冬季的黑潮流强产生影响，由此构成了一个包含海洋和大气耦合过程的正反馈机制。黑潮流域的海气相互作用过程可能受冬季风和黑潮流强相对强弱的调制，海洋过程和大气过程主导一方的转换中存在一个“临界值”。 相似文献
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《Journal of Atmospheric and Solar》2005,67(12):1063-1073
The performance of a computer program, called Autoscala, for the automatic scaling of foF2 and MUF(3000)F2 from ionograms has been extensively tested. Results of comparisons between automatically and manually scaled data are shown both for Autoscala and for ARTIST (release 4.01). Particular attention has been paid to the cases in which the ionograms have a truncated trace. The problem of the rejection of bad quality ionograms has been also considered. The analysis of data shows that the reliability of values automatically given as output by Autoscala is good. For the data set considered Autoscala seems to operate better than ARTIST. 相似文献
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This paper investigates the pull-out behaviour (particularly the bearing resistance) of a steel grid reinforcement embedded in silty sand using laboratory tests and numerical analyses. It is demonstrated that the various common analytical equations for calculating the bearing component of pull-out resistance give a wide range of calculated values, up to about 200% disparity. The disparity will increase further if the issue of whether to use the peak or critical state friction angle is brought in. Furthermore, these equations suggest that the bearing resistance factor, Nq, is only a function of soil friction angle which is not consistent with some design guidelines. In this investigation, a series of large scale laboratory pull-out tests under different test pressures were conducted. The test results unambiguously confirmed that the Nq factor is a function of test pressure. A modified equation for calculating Nq is also proposed. To have more in-depth understanding of the pull-out behaviour, the tests were modelled numerically. The input parameters for the numerical analysis were obtained from laboratory triaxial tests. The analysis results were compared with the experimental results. Good agreement between experimental and numerical results was achieved if the strain-softening behaviour from peak strength to critical state condition was captured by the soil model used. 相似文献
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利用CAM5模式设计敏感性试验,研究了中国东部夏季降水对青藏高原地面辐射异常变化的响应和可能的物理机制。试验结果表明：当高原北部、中部等区域夏季地面辐射减小,中国东部夏季降水整体上增多,但南部、东部沿海区域降水异常减少。青藏高原地面辐射的变化,对青藏高压、西太平洋副热带高压和季风等天气系统具有一定影响,进而影响中国东部地区的夏季降水。当青藏高原地面辐射减小,青藏高压中心位置偏西,强度减弱;东亚季风和南亚季风强度增大,中国东部大部分地区850 hPa风场强度增强;西太平洋副热带高压位置偏东,强度减弱,中国南部、东部沿海区域夏季降水受其影响而减少,但华中、华北、东北等地夏季降水整体上增多。故中国东部夏季降水异常变化与青藏高原地面辐射之间具有显著的相关关系。 相似文献
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