磁暴期间高纬顶部电离层离子上行特征——DMSP卫星观测   总被引：2，自引：1，他引：1       下载免费PDF全文

周康俊  蔡红涛  程力君  马淑英  占卫家  沈格  李飞 《地球物理学报》2014,57(11):3541-3550

本文利用DMSP F13和F15卫星观测数据,对2001—2005年58个磁暴(-472 nT≤Min.Dst≤-71 nT)期间高纬顶部电离层离子整体上行特征进行了统计研究.观测表明,磁暴期间,顶部电离层离子上行主要发生在极尖区和夜间极光椭圆区.在北半球,磁正午前,高速的离子上行(≥500 m·s^-1)多集中在65° MLat以上;午后,高速离子上行区向低纬度扩展,上行速度要略高于午前;在南半球,磁午夜前,DMSP卫星在考察区域内几乎所有的纬度上都观测到了高速上行的离子;午夜后,各纬度上观测到上行离子的速度明显降低.离子上行期间,DMSP卫星在极区顶部电离层高度上也频繁地观测到电子/离子增温,且电子增温发生的频率要远高于离子增温.O⁺密度变化分析显示,DMSP卫星磁暴期间观测到的上行离子更多地源于顶部电离层高度.这些结果表明电子增温在驱动暴时电离层离子整体上行过程中起着重要作用.  相似文献   

运用H-k扫描和人工读取震相到时两种方法对比研究云南地区地壳结构   总被引：1，自引：0，他引：1  

龙飞  胡家富  杨海燕  陈俊磊 《地震研究》2014,37(4)

利用云南及其邻区59个宽频地震台站记录到的30°~100°远震资料,采用P波接收函数方法对云南地区的地壳厚度和地壳平均泊松比分布进行分析。研究结果显示:用H-k扫描和人工读取震相到时两种方法得到的云南地区地壳厚度和泊松比分布情况较为吻合。研究区域内Moho面埋深南浅北深,横向变化达30~40 km。在川滇菱形块体东南缘,地壳厚度等值线呈东南向舌状突出。泊松比呈块体分布特征,断裂两侧差异显著。高泊松比的分布主要集中在滇缅泰块体内和研究区域北部以及小江断裂附近,这与该区处于印度板块与欧亚板块碰撞俯冲前缘的特殊地理位置有关。  相似文献   

福建省地下流体观测干扰因素综合查询系统的设计与实现     

陈小云  李毅伟  黄永模  薛飞  江宁 《华南地震》2014,(4):51-54

将福建省地下流体观测网内观测井各测项在观测期间内出现的干扰事件进行汇总,并进行分类入库保存,实现地下流体干扰因素的录入、查询、检查、修改、计算。编制一个操作界面友好、功能全面的观测井各测项的正常动态与干扰因素综合查询系统,更好地发挥观测数据共享的作用,为分析预报人员查找干扰资料提供方便,同时为福建省地震地下流体观测井的效能评价提供指导作用。  相似文献   

面向对象的高分辨率影像单值分类耕地提取方法研究     

徐世武  杨双  孙飞  郭庆华 《测绘通报》2014,(10):78-81

遥感技术已广泛地应用于土地覆盖/土地利用分类中。在专题应用中,用户只对某一类地物感兴趣,例如耕地提取,即单类别分类问题。随着影像分辨率的提高,基于像元的分类算法难以满足高分辨率影像高精度信息提取的需求。本文采用结合面向对象分类思想和基于正样本、未标记样本遥感单值（PUL）分类方法从多源高分辨率影像中提取耕地信息,并与基于像素的分类实验进行对比分析。结果表明,在缺少部分地类的不完全训练集下,基于面向对象的单值分类较传统神经网络分类有更较稳定的表现,并且远优于基于像素的分类结果。  相似文献   

地震仪器设备管理系统的设计与实现     

刘爱华  刘英华  龚飞 《地震地磁观测与研究》2014,35(5)

利用Java语言,使用Microsoft SQL Server 2005数据库,利用MyEclipse工具研发地震仪器设备管理系统.使用该系统进行台站仪器设备信息管理,便于保存、查询、更新信息,实现数据资料的完整、准确、长期保存,工作效率增加.  相似文献   

基于无线Mesh网络技术的应急通信技术应用   总被引：2，自引：0，他引：2  

付荣国  肖飞 《地震学刊》2014,(6):778-783

强烈地震发生后,灾区现场通信网络设施往往遭到破坏,因此快速建立有效且覆盖面大的应急通信网络,及时传递灾情信息,对现场组织救灾及指挥调度等救援工作具有重大意义。无线网络具有组网简单快速、成本低等技术特点,适合作为现场应急通信的网络平台。本文提出了一种基于无线Mesh网络技术的地震现场应急通信方法,在灾区现场迅速组建无线局域网,从而实现信息传递和共享,整个系统组网快捷、健壮性好,并且通过卫星通信技术可以将各局域网组成灾区广域网并进一步接入互联网,该方法能满足地震现场应急通信信息传输的基本要求。  相似文献   

膝关节痛风性关节炎的CT与MRI分析     

袁健祥  张家雄  方挺松  衣利磊  孙洋 《CT理论与应用研究》2014,(3):489-496

目的：探讨膝关节痛风性关节炎的CT和MRI影像特征。方法：回顾分析经手术病理证实的21例膝关节痛风性关节炎的CT和MRI表现,其中12例CT,14例MRI。结果：所有病例均能发现痛风结节,CT显示45个,MRI显示48个,痛风结节位于肌腱和韧带共58个,滑膜或关节腔内15个,骨内11个,其他软组织9个。形态呈条块状31个,结节状31个,线状4个,不规则形27个。骨质破坏CT共发现21处,MRI发现24处,位于骨边缘共30处;MRI显示5处骨质破坏周围骨髓水肿。痛风结节在T1WI均呈低至中等信号;T2WI上39个呈混杂信号,6个呈高信号,3个呈低信号。在5例均行CT及MRI检查膝关节比较中：CT显示痛风结节21个,MRI显示痛风结节18个;CT和MRI在显示骨质破坏的部位均为12处,MRI显示骨髓水肿4处;MRI显示软骨异常共5处。结论：膝关节痛风性关节炎在影像上有一定的特征性,CT更容易发现痛风结节,而MRI更合适于评估软组织情况及炎性改变,综合分析两种影像资料有助于准确诊断痛风性关节炎。  相似文献   

A model study of the Copper River plume and its effects on the northern Gulf of Alaska     

Yuan Wang  Huijie Xue  Fei Chai  Yi Chao  John Farrara 《Ocean Dynamics》2014,64(2):241-258

A three-level nested Regional Ocean Modeling System was used to examine the seasonal evolution of the Copper River (CR) plume and how it influences the along- and across-shore transport in the northern Gulf of Alaska (NGoA). A passive tracer was introduced in the model to delineate the growth and decay of the plume and to diagnose the spread of the CR discharge in the shelf, into Prince William Sound (PWS) and offshore. Furthermore, a model experiment with doubled discharge was conducted to investigate potential impacts of accelerated glacier melt in future climate scenarios. The 2010 and 2011 simulation revealed that the upstream (eastward) transport in the NGoA is negligible. About 60 % of the passive tracer released in the CR discharge is transported southwestward on the shelf, while another one third goes into PWS with close to 60 % of which exiting PWS to the shelf from Montague Strait. The rest few percent is transported across the shelf break and exported to the GoA basin. The downstream transport and the transport into PWS are strongly regulated by the downwelling-favorable wind, while the offshore transport is related to the accumulation of plume water in the shelf, frontal instability, and the Alaskan Stream. It takes weeks in spring for the buoyancy to accumulate so that a bulge forms outside of the CR estuary. The absence of strong storms as in the summer of 2010 allows the bulge continue growing to trigger frontal instability. These frontal features can interact with the Alaskan Stream to induce transport pulses across the shelf break. Alternatively as in 2011, a downwelling-favorable wind event in early August (near the peak discharge) accelerates the southwestward coastal current and produces an intense downstream transport event. Both processes result in fast drains of the buoyancy and the plume content, thereby rapid disintegration of the plume in the shelf. The plume in the doubled discharge case can be two to three times in size, which affects not only the magnitude but also the timing of certain transport events. In particular, the offshore transport increases by several folds because the plume appears to be more easily entrained by the seaward flow along the side of Hinchinbrook Canyon.  相似文献   

Seismic traveltime inversion of 3D velocity model with triangulated interfaces          下载免费PDF全文

Fei Li  Tao Xu  Minghui Zhang  Zhenbo Wu  Chenglong Wu  Zhongjie Zhang  Jiwen Teng 《地震科学（英文版）》2014,27(2):127-136

Seismic traveltime tomographic inversion has played an important role in detecting the internal structure of the solid earth. We use a set of blocks to approximate geologically complex media that cannot be well described by layered models or cells. The geological body is described as an aggregate of arbitrarily shaped blocks, which are separated by triangulated interfaces. We can describe the media as homogenous or heterogeneous in each block. We define the velocities at the given rectangle grid points for each block, and the heterogeneous velocities in each block can be calculated by a linear interpolation algorithm. The parameters of the velocity grid positions are independent of the model parameterization, which is advantageous in the joint inversion of the velocities and the node depths of an interface. We implement a segmentally iterative ray tracer to calculate traveltimes in the 3D heterogeneous block models. The damped least squares method is employed in seismic traveltime inversion, which includes the partial derivatives of traveltime with respect to the depths of nodes in the triangulated interfaces and velocities defined in rectangular grids. The numerical tests indicate that the node depths of a triangulated interface and homogeneous velocity distributions can be well inverted in a stratified model.  相似文献   

The four dimensional variational data assimilation with multiple regularization parameters as a weak constraint (Tikh-4D-Var) and its preliminary application on typhoon initialization     

Jian Zhong  JianFang Fei  XiaoPing Cheng  XiaoGang Huang 《中国科学:地球科学(英文版)》2014,57(11):2690-2701

Traditional variational data assimilation (VDA) with only one regularization parameter constraint cannot produce optimal error tuning for all observations. In this paper, a new data assimilation method of “four dimensional variational data assimilation (4D-Var) with multiple regularization parameters as a weak constraint (Tikh-4D-Var)” is proposed by imposing different regularization parameters for different observations. Meanwhile, a new multiple regularization parameters selection method, which is suitable for actual high-dimensional data assimilation system, is proposed based on the posterior information of 4D-Var system. Compared with the traditional single regularization parameter selection method, computation of the proposed multiple regularization parameters selection method is smaller. Based on WRF3.3.1 4D-Var data assimilation system, initialization and simulation of typhoon Chaba (2010) with the new Tikh-4D-Var method are compared with its counterpart 4D-Var to demonstrate the effectiveness of the new method. Results show that the new Tikh-4D-Var method can accelerate the convergence with less iterations. Moreover, compared with 4D-Var method, the typhoon track, intensity (including center surface pressure and maximum wind speed) and structure prediction are obviously improved with Tikh-4D-Var method for 72-h prediction. In addition, the accuracy of the observation error variances can be reflected by the multiple regularization parameters.  相似文献