CINRAD/SA雷达闪码故障的诊断分析     

蔡勤  柴秀梅  周红根  李冰峰  杨莹  朱毅 《气象》2011,37(8):1045-1048

2009年2月8日至16日徐州天气雷达开机过程中,产品出现断断续续的拉丝现象,产品拉丝处图像掩盖了实际回波,而检查雷达的各项标校参数,其值均在正常范围且无任何报警,雷达回波异常,使雷达不能正常发挥其有效的作用。通过对CINRAD/A雷达伺服信号链路进行分析,查找闪码故障的产生原因和检测检修方法,为雷达技术保障人员提供现场维修、维护方面的经验。  相似文献   

X波段双偏振雷达探测数据分析与校验   总被引：1，自引：0，他引：1  

尹春光  王勤典  胡平  陈浩君 《气象科技》2011,39(5):608-614

保证移动X波段双偏振多普勒天气雷达在野外探测中雷达探测数据源的正确性,是预报员开展后续应用研究的重要前提。简要分析了差分反射率、相关系数、差分传播相移与差分相移系数的理论意义,同时结合多次观测经验,重点研究并验证了各双偏振产品在纯降水中的数值,研究双偏振参数对雷达硬件故障的指示意义,确保在探测时及时发现硬件故障与差损,提高探测数据质量。讨论了双偏振参数自测试校验,进行水平通道与垂直通道参数偏差校验,确保在探测之前获得双偏振通道的一致性。  相似文献   

双线偏振雷达判别降水粒子类型技术及其检验   总被引：5，自引：3，他引：5  

曹俊武  刘黎平 《高原气象》2007,26(1):116-127

在综合分析国内外降水粒子相态识别方法的基础上,结合我国双线偏振雷达的应用需求,建立了一套利用双线偏振雷达探测资料识别降水粒子类型的识别模式,并根据美国KOUN雷达观测资料对该模式进行了分析验证,同时检验了模式中的几个偏振参数:差分反射率因子ZDR、差传播相移KDP、水平偏振和垂直偏振回波功率零滞后互相关系数ρHV(0)对不同降水粒子的识别效果。通过分析认为:利用该识别模式得到的结果基本合理,可以反映降水区域内降水粒子的相态结构,但还需要对资料作进一步的研究。同时在识别各类降水粒子方面,ZDR的效果要高于KDP和ρHV(0),在缺乏相关资料的情况下可以考虑用ZH和ZDR配对识别的结果作为真实的结果。  相似文献   

雷达资料在云南一次强降水过程中的三维变分同化试验   总被引：2，自引：0，他引：2  

李华宏  王曼  曹杰  闵颖  赵韬 《热带气象学报》2014,30(5):881-893

鉴于云南观测信息相对不足、局地强降水突出的现状,利用WRF(Weather Research and Forecasting)模式及其变分同化系统进行雷达反射率因子和反演风场的三维变分同化试验。通过对2012年9月12日00:00—13日00:00发生在云南的一次强降水过程进行数值模拟和对比分析,结果表明,同时同化雷达反演风场和基本反射率因子,对区域模式同化系统中风矢量、相对湿度、位势高度几个基本分析量都有明显影响。雷达资料的同化,有利于区域模式初始场中强降水区域的上游中低层空气湿度增加、水汽输送增强和强降水发生区域的风场辐合加强,从而改善区域模式对强降水落区、强度的预报质量。对于切变线等天气尺度系统影响下的强降水过程,雷达资料的同化持续时间选取3 h、同化间隔为1 h较适宜。另外,雷达反演风场和基本反射率因子的同化均对降水预报改善有明显贡献,且多种资料的同化效果好于单一资料同化。  相似文献   

CFL-03型风廓线雷达收发对接技术的改进   总被引：1，自引：0，他引：1  

任京伟  孙健  孙祥  肖震宇  杨彬  王德伦  陈润浩 《河南气象》2014,(4):109-113

在风廓线雷达的数据应用过程中,雷达获取数据的准确性至关重要,而风廓线雷达的收发对接过程又直接影响获取数据的准确性,因此,对雷达的收发对接技术进行研究非常重要。一般来说,对于该类型风廓线雷达的对接方法采用一种间接测试的方法,对接过程中要反复调整频综脉冲、发射脉冲、收发开关脉冲、封闭脉冲等的波形作用时间和脉宽。另外,收发开关脉冲的后沿并非标准矩形脉冲的后沿,位置难以确定,其后沿设置的位置离发射脉冲太近会产生高频头被击穿烧毁的现象,太远则会影响低层风的测风质量。以CFL-03型风廓线雷达为例,介绍了风廓线雷达的一般收发对接技术和改进的对接技术,以及频综、发射脉冲、收发开关脉冲、封闭脉冲等相关时序的确定方法。经过实践验证,两种对接技术都满足了设备的使用要求,而改进的收发对接技术,更直观形象,易于操作。  相似文献   

Ground penetrating radar inversion in 1-D: an approach for the estimation of electrical conductivity, dielectric permittivity and magnetic permeability   总被引：1，自引：0，他引：1  

O. Lzaro-Mancilla  E. Gmez-Trevio 《Journal of Applied Geophysics》2000,43(2-4)

This paper presents a method for inverting ground penetrating radargrams in terms of one-dimensional profiles. We resort to a special type of linearization of the damped E-field wave equation to solve the inverse problem. The numerical algorithm for the inversion is iterative and requires the solution of several forward problems, which we evaluate using the matrix propagation approach. Analytical expressions for the derivatives with respect to physical properties are obtained using the self-adjoint Green's function method. We consider three physical properties of materials; namely dielectrical permittivity, magnetic permeability and electrical conductivity. The inverse problem is solved minimizing the quadratic norm of the residuals using quadratic programming optimization. In the iterative process to speed up convergence we use the Levenberg–Mardquardt method. The special type of linearization is based on an integral equation that involves derivatives of the electric field with respect to magnetic permeability, electrical conductivity and dielectric permittivity; this equation is the result of analyzing the implication of the scaling properties of the electromagnetic field. The ground is modeled using thin horizontal layers to approximate general variations of the physical properties. We show that standard synthetic radargrams due to dielectric permittivity contrasts can be matched using electrical conductivity or magnetic permeability variations. The results indicate that it is impossible to differentiate one property from the other using GPR data.  相似文献   

Evaluation of pile foundation response to lateral spreading   总被引：7，自引：0，他引：7  

Tarek Abdoun  Ricardo Dobry 《Soil Dynamics and Earthquake Engineering》2002,22(9-12):1051-1058

The effects of liquefaction on deep foundations are very damaging and costly, and they keep recurring in many earthquakes. The first part of the paper reviews the field experience of deep foundations affected by liquefaction during earthquakes in the last few decades, as well as the main lessons learned. The second part of the paper presents results of physical modeling of deep foundations in the presence of liquefaction conducted by the authors and others at the 100g-ton RPI centrifuge. In the last decade centrifuge modeling has been identified as a key tool to identify and quantify mechanisms, calibrate analyses and evaluate retrofitting strategies for pile foundations. Results are presented of centrifuge models of instrumented pile foundations subjected to lateral spreading, including single pile and pile groups, 2- and 3-layer soil profiles, mass and stiffening elements above ground to incorporate the effect of the superstructure, and evaluation of proposed retrofitting strategies. Interpretations of these centrifuge experiments and their relation to field observations and soil properties.  相似文献   

粤北一次降雹过程的成因分析     

郝建平  曹刚  李斌  魏璐 《广东气象》2014,36(6):20-23

利用常规气象观测资料、以及雷达观测资料对发生在粤北地区的一次降雹过程进行分析,结果发现:该次降雹过程是在高低空急流、切变线、地面辐合线、弱冷空气的共同作用下产生的;雷达基本反射率产品、VIL产品以及VWP产品对降雹云具有较好的识别作用。  相似文献   

雷达资料在一次大范围冰雹天气过程中的同化试验分析     

张小娟  张诚忠  齐大鹏  黄钰  朱文达 《气象》2022,48(1):61-72

基于华南区域高分辨率数值模式,采用牛顿连续松弛逼近法(nudging)同化C波段多普勒雷达反射率资料,针对2018年4月2日贵州一次大范围冰雹天气过程进行了数值模拟试验.分析结果表明:在模式中进行雷达反射率因子信息nudging同化后,调整了分析场中的水凝物信息和热力场结构,对流层中层的雨水和冰相粒子含量均增加,水凝物...  相似文献   

Characteristics of the Submarine Topography and its Profile Type of the Coast of China     

CAO Chao  CAI Feng  LI Yan  ZHENG Yongling  WU Chenqiang  LU Huiquan  BAO Jingjing  XU Yan 《《地质学报》英文版》2013,87(6):1724-1742

Based on the latest submarine topography data of the China 908 Project （China offshore marine environmental comprehensive investigation and assessment）,we analyzed the general China offshore submarine topographical characteristics and the factors influencing its development.The submarine topography off the coast of China follows the NW-SE trend of the land topography.The gradient of the submarine topography ranges from 0.2％ to 1.6％ with an average gradient of about 0.8％.The depth contours run mostly parallel to the coast,and extend out to sea in estuary areas.The submarine topography is dominated by the geological structure,which shows the typical characteristics of two uplifts and two subsidence events from north to south.The geological structure combined with the different sedimentary environments and complex hydrodynamic conditions produced topography that can be characterized by three types：sedimentary basins,compressionuplift,and transition form.In the sedimentary basin and compression-uplift regions,the topographical undulation is small,sediments are fine-grained,and the currents flow in a single direction,leading to bays with sedimentary plains and underwater accumulation slopes,which are of the same tectonic origin.Transition-type topography is characterized by strong undulations and mixed-size sediment particles,terraces and scarps inshore and shelf plains and erosion-deposition landforms offshore.This is a result of incomplete fault block development and repeated transgressions.In the deposition reformation regions （transition form type）,the topography has strong undulations,the sediments are coarse,tidal sand ridges are well-developed at terrigenoussupplied estuaries and convergence zones,and the Holocene sediments are thick,transformed by tides,river runoff,and currents.  相似文献