一种GNSS大网数据快速高效处理策略

针对当前大型GNSS网络数据处理需求与现有处理策略和能力的矛盾,介绍基于不动点理论所建立的Ambizap网解新算法,将分布式计算技术引入到GNSS数据处理中,设计并利用.NET框架下的分布式技术实现分布式环境下基于Ambizap算法的大型GNSS网数据分布式处理流程,通过多个算例验证了Ambizap算法的精度和其分布式应用的高效性。     

DIAGNOSIS OF NWP SYSTEMATIC FORECAST ERRORS IN ZONAL MEAN CIRCULATION

It is proved in this paper that NWP systematic forecast errors in the zonal mean circulation aredue to the difference in westerly acceleration process during the forecasting period between model andreal atmospheres.Those forcing factors which evoke the zonal mean wind variation can be split into various linearterms according to the non-acceleration theorem in a primitive equation system,By applying this tech-nique to the diagnosis of the forecast produets of the T42L9 model in January 1992 and in July 1992,it is indicated that the model has the ability to forecast the zonal mean wind to a reasonable extent,but there are still some errors in several places,especially in the upper troposphere and lower strato-sphere in the mid-latitude region as well as near the surface.The results of analysis by employing thisscheme reveal the reason responsible for the systematic forecast errors of the zonal mean wind in themodel and the possible way of improving it.It is also shown that non-acceleration theorem can be used as an efficient tool to diagnose thephysical processes of NWP models.     

近场波动数值模拟稳定性问题分析

本文利用分析一维双曲型偏微分方程初边值问题数值稳定性的GKS定理的物理解释的推广，以出平面波动为例，分析了集中质量显式有限元方法及中心有限差分方法分别与多次透射公式简单结合构成的封闭数值求解系统的稳定性，并用数值试验进行了验证。旨在从概念上说明讨论人工边界稳定性时，必须与计算区域内的具体算法结合分析才有意义，单纯地说人工边界在数值计算中稳定或不稳定是不正确的。     

Fast hyperbolic deconvolutive Radon transform using generalized Fourier slice theorem

The hyperbolic Radon transform has a long history of applications in seismic data processing because of its ability to focus/sparsify the data in the transform domain. Recently, deconvolutive Radon transform has also been proposed with an improved time resolution which provides improved processing results. The basis functions of the (deconvolutive) Radon transform, however, are time-variant, making the classical Fourier based algorithms ineffective to carry out the required computations. A direct implementation of the associated summations in the time–space domain is also computationally expensive, thus limiting the application of the transform on large data sets. In this paper, we present a new method for fast computation of the hyperbolic (deconvolutive) Radon transform. The method is based on the recently proposed generalized Fourier slice theorem which establishes an analytic expression between the Fourier transforms associated with the data and Radon plane. This allows very fast computations of the forward and inverse transforms simply using fast Fourier transform and interpolation procedures. These canonical transforms are used within an efficient iterative method for sparse solution of (deconvolutive) Radon transform. Numerical examples from synthetic and field seismic data confirm high performance of the proposed fast algorithm for filling in the large gaps in seismic data, separating primaries from multiple reflections, and performing high-quality stretch-free stacking.     

三维层结大气随高度变化基流的不稳定性及半椭圆定理

本文应用Ｈｏｗａｒｄ（１９６１）所用的精巧积分方法研究了三维非静力平衡层结大气随高度变化基流上重力内波的不稳定性质。给出了不稳定产生的必要条件和相速度在相速复平面上的分布规律；发展了Ｍｉｌｅｓ定理和Ｈｏｗａｒｄ半圆定理；得到了有限深度气层的半椭圆定理。并指出在随高度变化的基流中，重力内波的不稳定范围与基流的垂向结构及波传播方向有关；半椭圆的位置和长轴分别重合于Ｈｏｗａｒｄ半圆的位置和直径，而短轴则依赖于与Ｒｉｃｈａｒｄｓｏｎ数相关的参数Ｊ０，Ｒ０和波数｜ｋ｜及流场厚度参数ｋ０     

不稳定横波型扰动谱点分布的半圆定理

作者在理论上对不稳定横波型扰动的谱点分布作了分析,得到了该不稳定扰动谱点分布的半圆定理,即谱点分布在复平面上以原点为圆心、以R0为半径的下半圆域上;并发现扰动的波长越短、模式层顶越高、静力稳定度参数的绝对值越大、基流的垂直切变越大、纬度越高则该半径就越大.     

土-结爆炸冲击相互作用模爆试验相似设计方法

模爆试验是研究爆炸冲击荷载作用下地基动力性能、土-结爆炸冲击相互作用及埋地防护结构抗爆能力与破坏机理等的重要手段之一。模型相似设计是确保模爆试验能够尽可能真实地反映原型爆炸冲击动力性状的关键之一。以上覆饱和砂土层对浅埋地下圆拱直墙式防护隧道免遭炸弹触地爆炸触发地冲击波破坏的保护效应为研究目的,基于目前广泛应用的Bockinghamπ定理,采用量纲分析方法,并且结合考虑土-结体系非线性爆炸冲击动力响应、土-结接触面爆炸冲击动力响应以及爆炸地冲击波-结构动力相互作用等的相似性,求解土-结爆炸冲击相互作用模爆试验的模型设计相似关系。     

路堤下土工合成材料加固软土地基的极限分析

路堤或堤坝工程中土工合成材料加固软土地基得到广泛应用,但其计算方法仍有不足之处。从极限分析的角度来研究,引入滑移线法来改进极限分析上限法,推导出一种新的地基极限分析方法,并基于推导的极限承载力计算公式,把路堤破坏宽度作为变量,求解出路堤极限高度。工程实例对比分析表明,路堤极限高度计算结果与实测结果相差不大。其研究结论为软土地基路堤设计提供了一个新的和有效的方法。     

采样率不足引起的反应谱计算误差

本文从分析谐波的反应谱计算误差及其产生原因入手,研究了常规反应谱方法的计算误差,指出选择采样率不仅要参照信号的奈奎斯特频率,还要注意使用采样数据时恢复被采信号所用的内插方法和容许的内插误差,文中强调山农采样定理所说的采样率大于２倍奈奎斯特频率时可完全恢复被采信号是针对内插函数ｈａ（ｔ－ｎ．Ｔ）而言的,文中以用典型的加速度反应谱合成的５条地震加速度里程及一系列谐波里程为例,研究了由于采样率不足而引起     

基于贝叶斯理论的AVO三参数波形反演

在实际的AVO反演问题中,叠前数据体中的噪声或其他因素严重影响了AVO反演问题的适定性,而采用先验地质信息作为AVO反演问题的约束条件是解决AVO反演问题不适定的一种可行方法. 文中的似然函数采用了[WTBX]ι[WTBX]p范数的解,并用Cauchy分布表示先验模型参数的分布. 以此为基础,在反演中建立了测井数据的参数协方差矩阵对反演过程进行约束,并采用了共轭梯度算法实现多参数非线性的反演过程. 同时,为了提高反演精度,避免动校正拉伸及依赖于炮检距的调谐效应对参数估计的影响,反演采用动校前地震数据进行参数估计. 从应用效果分析来看,即使叠前道集的信噪比不高,反演的结果也能较好地与实际情况相匹配,为识别储层流体性质提供了新的手段.