基于全波形激光雷达数据分解方法的研究     

梁敏  王仁礼  李国新 《地理信息世界》2016,(5):51-54

波形分解是全波形激光雷达数据处理的关键技术之一,通过雅克比矩阵更新与否以及阻尼系数的调整,对优化LM(Levenberg-Marquard)算法进行了研究。实验表明,该方法可最优化求解足印内各波形分量的振幅、中心位置和半宽,而不必每次迭代时都需计算雅克比矩阵,简化了计算过程,提高了计算效率,最终得到的模拟波形能够非常好地拟合原始波形。  相似文献   

球谐分析及合成并行计算     

肖华东  陆洋 《测绘科学》2007,32(1):21-23

本文介绍了球谐合成和分析问题的数值计算原理,研究分析了其内在的并行性,提出了区域划分和聚合通信的并行计算策略。基于傅立叶变换技术,应用MPI(消息传递接口)并行编程模式,实现了球谐分析及合成计算的并行化。实验结果表明,较之串行实现,并行实现大大缩短了计算时间,获得了近似线形加速比,取得很高的并行效率。  相似文献   

海洋大数据序列时-空变化主成分分析方法     

方文东  宋运法 《热带海洋学报》1998,(3)

介绍海洋要素时－空变化大数据量主成分分析方法,讨论并澄清主成分分析在海洋大数据序列应用中的一些问题和易混淆的概念。根据美国国家海洋与大气局（NOAA）卫星观测的海表面温度红外资料,对加拿大温哥华岛西部大陆架区8个夏季海表面温度的空间变化进行主成分分析,以促进主成分方法在海洋大数据序列分析中的应用。  相似文献   

华北汛期旱涝与中高纬大气环流异常   总被引：42，自引：10，他引：32  

赵声蓉  宋正山 《高原气象》1999,18(4):535-540

利用１９８０￣１９９４年ＮＣＥＰ／ＮＣＡＲ月平均高度场和我国测站降水量资料,通过奇异值分解方法探讨了华北汛期降水与５００,２００ｈＰａ欧亚吭纬大气环流这关系,得到与华北汛期旱涝有关的两类异常环流型。  相似文献   

High-pressure decomposition of MCr2O4 spinels (M=Mg, Mn, Zn) by ab initio methods     

M. Catti  F. Freyria Fava  C. Zicovich  R. Dovesi 《Physics and Chemistry of Minerals》1999,26(5):389-395

The high-pressure equation of state of the normal spinels MgCr₂O₄ (picrochromite), MnCr₂O₄ and ZnCr₂O₄, and their reaction of decomposition into Cr₂O₃ (eskolaite) and MO (rocksalt-type) component oxides, were investigated by periodic unrestricted Hartree-Fock calculations. All-electron basis sets, and an a posteriori correction for the electron correlation energy, based on Density-Functional-Theory, were employed. Interpolation of results by the P-V Murnaghan equation of state yielded the equilibrium volume and energy, and the bulk modulus and its pressure derivative, for each of the seven phases (three spinels, three rocksalt oxides and eskolaite) considered. The simulated behaviour of interatomic distances vs pressure shows similar compressibilities of M-O bonds in both octahedral and tetrahedral coordinations. Binding energies and formation enthalpies of spinels from oxides are also computed and compared to available experimental data. The predicted decomposition pressures of Mg, Mn and Zn chromium spinels are 19, 23 and 34 GPa, respectively. The greater stability of ZnCr₂O₄ is related to Zn²⁺ being better suited to tetrahedral coordination than the other M²⁺ cations. Such results are strongly supported by the excellent agreement previously obtained between simulated (11 GPa) and experimental (13 GPa) pressures of the decomposition of MgAl₂O₄ spinel into corundum and periclase. Received: 9 February 1998 / Accepted: 12 October 1998  相似文献   

经验模态法在中国沿岸海平面变化中的应用研究   总被引：4，自引：0，他引：4  

王卫强  陈宗镛  左军成 《海洋学报》1999,21(6):102-109

我国现代海平面变化的系统研究,开始于80年代前后,主要集中于海平面年变率和预测。早期所采用的方法有直线回归法、周期法外推预测等,之后有本征分析方法、随机动态预测模型及灰色系统方法等,以上方法各有利弊,但都因为不能较精确得到海平面变化中的各种周期变化而使得预测精度较差,尤其是对于海平面变化中较长周期的分辨方面。  相似文献   

基于经验模态分解的分数维地震随机噪声衰减方法          下载免费PDF全文

颜中辉  栾锡武  王赟  潘军  方刚  施剑 《地球物理学报》2017,60(7):2845-2857

经验模态分解算法(EMD)是一种基于有效波和噪声尺度差异进行波场分离的随机噪声压制方法,但由于实际地震数据波场复杂,导致模态混叠较严重,仅凭该方法进行去噪很难达到理想效果.本文基于EMD算法对信号多尺度的分解特性,结合Hausdorff维数约束条件,提出一种用于地震随机噪声衰减的新方法.首先对地震数据进行EMD自适应分解,得到一系列具有不同尺度的、分形自相似性的固有模态分量(IMF);在此基础上,基于有效信号和随机噪声的Hausdorff维数差异,识别混有随机噪声的IMF分量,对该分量进行相关的阈值滤波处理,从而实现有效信号和随机噪声的有效分离.文中从仿真信号试验出发,到模型地震数据和实际地震数据的测试处理,同时与传统的EMD处理结果相对比.结果表明,本文方法对地震随机噪声的衰减有更佳的压制效果.  相似文献   

基于Low-rank分解的复杂TI介质纯qP波正演模拟与逆时偏移   总被引：2，自引：2，他引：0       下载免费PDF全文

黄金强  李振春 《地球物理学报》2017,60(2):704-721

近年来,面向实际应用的TI介质准P波正演模拟与逆时偏移成像技术受到空前的关注.基于常规耦合型传播方程的正演模拟方法不仅存在伪横波及频散假象干扰,而且还遭受模型参数限制(η0)和不稳定影响;而纯qP波方程的推导繁琐,且由于方程中包含拟微分算子造成求解难度大且精度有限.为此,本文首先构建了一种适用于任意TI介质的纯qP波传播算子,然后借助Low-rank分解求取该算子中的空间-波数域矩阵,同时引入Cerjan衰减边界条件来压制边界反射干扰,最终实现了一种间接的纯qP波波场外推方案,并将其成功应用于复杂TI介质正演模拟与逆时偏移成像中.通过开展数值模拟,并与其他方法对比表明:①该方法既避免了纯qP波方程的繁琐推导,又克服了耦合型方程对模型参数的限制;②还彻底消除了残余伪横波噪音及数值频散;③且能适应较大时间或空间步长及高频震源,是一种相对准确且稳定的各向异性纵波正演与成像策略.  相似文献   

2017年九寨沟地震前重力场异常特征提取   总被引：2，自引：2，他引：0  

刘芳  祝意青  赵云峰  刘涛 《中国地震》2017,33(4):532-539

2017年8月8日九寨沟发生7.0级地震,此次地震发生在塔藏断裂、岷江断裂和虎牙断裂附近,震源机制为走滑型。重力场静态异常和动态异常变化可为研究深地壳结构性质提供重要的物理场信息。本文利用WGM计算的布格重力异常数据及实测流动重力数据进行小波多尺度分解,分离得到不同深度场源特征的地壳介质横向不均匀性。结果表明,WGM布格重力异常数据和实测重力数据的小波多尺度结果较为一致,通过对比分析发现,九寨沟地震发生在区域重力场的四象限分布中心位置,不同时空尺度的重力场变化对于深入认识潜在地震危险性趋势具有一定的科学意义。  相似文献   

DEEP STRUCTURE OF NORTHERN HENAN PROVINCE AND ADJACENT AREAS DERIVED FROM GRAVITY AND SEISMIC SOUNDING DATA IN RELATION TO DISTRIBUTION OF EARTHQUAKES          下载免费PDF全文

JIANG Lei  XU Zhi-ping  FANG Sheng-ming  YANG Li-pu  LI Yi-qing  XU Shun-qiang 《地震地质》2018,40(2):323-336

We conduct the wave field separation of the gravity field for northern Henan Province and adjacent areas by the wavelet multi-scale decomposition method, and obtain multi-order gravity wavelet details and regional gravity field information. Then the Parker density surface inversion is used to invert the Moho interface. Based on the analysis of wavelet details in different orders and results of three seismic sounding profiles available in this area, we attempt to reveal the deep crustal structure of the study area. Research results show that the crustal structure is dominated by uneven density distribution accompanied by uplifts and depressions in the region with obvious heterogeneities of the density in horizontal and vertical directions. The gravity field characteristics in the middle-upper crust correspond to the surface topography, the lower crust is dominated by the large-scale high-low gravity anomalies, and several major depression basins show the characteristics of low velocity and low density. At the same time, the depth of the Moho interface changes greatly, which forms the block structure pattern of the regional crustal thickness. Among these features, the area with relatively large variations of the Moho is located in the transition zone of the basin to the Taihang Mountains, or exactly the Moho mutation belt. The Moho interface of the basin area as a whole is dominated by the uplift intertwined with local variations, of which the least and largest depths are 31km and 37km, respectively. Due to the gravity isostasy, the crustal thickness is larger(about 41km)in the northwest of the Taihang Mountains, with less average crustal density. In the study area, earthquakes tend to occur around the transition zone with density changes where the Moho is locally convex. The seismogenic mechanism may be associated with upwelling of upper mantle materials, low-velocity and low-density structures in the middle-lower crust and connection of deep large faults. Moreover, the deep large faults play a controlling role in the distribution of regional earthquakes.  相似文献