A simplified method for simulation of strong ground motion using finite rupture model of the earthquake source     

A.?JoshiEmail author  S.?Midorikawa 《Journal of Seismology》2004,8(4):467-484

We present a simplified method to simulate strong ground motion for a realistic representation of a finite earthquake source burried in a layered earth. This method is based on the stochastic simulation method of Boore (Boore, D. M., 1983, Bull. Seism. Soc. Am. 73, 1865–1894) and the Empirical Greens Function (EFG) method of Irikura (Irikura, K., 1986, Proceedings of the 7th Japan Earthquake symposium, pp. 151–156). The rupture responsible for an earthquake is represented by several subfaults. The geometry of subfaults and their number is decided by the similarity relationships. For simulation of ground motion using the stochastic simulation technique we used the shapping window based on the kinetic source model of the rupture plane. The shaping window deepens on the geometry of the earthquake source and the propagation characteristics of the energy released by various subfaults. The division of large fault into small subfaults and the method for accounting their contribution at the surface is identical to the EGF. The shapping window has been modified to take into account the effect of the transmission of energy released form the finite fault at various boundaries of the layered earth model above the source. In the present method we have applied the correction factor to adjust slip time function of small and large earthquakes. The correction factor is used to simulate strong motion records having basic spectral shape of ² source model in broad frequency range. To test this method we have used the strong motion data of the Geiyo earthquake of 24th March 2001, Japan recorded by KiK network. The source of this earthquake is modelled by a simple rectangular rupture of size 24 × 15 km, burried at a depth of 31 km in a multilayered earth model. This rupture plane is divided into 16 rectangular subfaults of size 6.0 × 3.75 km each. Strong motion records at eight selected near-field stations were simulated and compared with the observed records in terms of the acceleration and velocity records and their response spectrum. The comparison confirms the suitability of proposed rupture model responsible for this earthquake and the efficacy of the approach in predicting the strong motion scenario of earthquakes in the subduction zone. Using the same rupture model of the Geiyo earthquake, we compared the simulated records from our and the EGF techniques at one near-field station. The comparison shows that this technique gives records which matches in a wide frequency range and that too from simple and easily accessible parameters of burried rupture.  相似文献   

三维城市模型的构建及其在噪音污染分析中的应用   总被引：1，自引：0，他引：1  

谭仁春  李长辉  王红新 《测绘科学》2006,31(3):101-103

本文提出了综合利用二维矢量数据、航空影像和激光测距与距离修正数据建立三维城市模型的技术路线,并在此基础上探索了城市噪音污染信息在现有三维城市模型中的建模和可视化方法。  相似文献   

GNSS接收机晶振参数对载波相位测量的影响分析     

张提升  郑建生  章红平  严昆仑 《武汉大学学报(信息科学版)》2012,37(12):1413-1416,1447

分析了射频与基带时钟不同源对载波相位测量的影响,构建了由晶振各类误差源引起的载波环跟踪误差模型。分析与实验结果表明,时钟不同源会导致载波相位测量出错,晶振引起的载波环测量误差随环路噪声带宽增大而减小,减小晶振的h系数和g灵敏度可提高测量精度。选用单一稳定度高、g灵敏度小的晶振作为GNSS接收机时钟,可改善载波相位精度。  相似文献   

基于灰度归一化的HJ-1A星HSI图像条带噪声去除方法     

兰穹穹  张立福  吴太夏 《国土资源遥感》2012,(2):45-49

针对HJ -1A星HSI图像上的条带噪声,在分析传统条带噪声去除方法的基础上,提出了一种新的基于灰度归一化去除条带噪声的方法.首先,设计孤立点检测窗口,将随机斑点噪声与条带噪声分离;然后,利用灰度归一化方法建立图像各列像元灰度级与基准列像元灰度级对应的查找表,根据查找表对HSI图像条带噪声进行消除.实验结果表明,该方法在很好地保留图像光谱信息的情况下,能够有效地消除图像条带噪声和随机斑点噪声.  相似文献   

一种基于极值检测与自适应滤波的图像去噪算法     

陈超  周绍光 《测绘工程》2012,21(4):13-16

标准中值滤波及其一些改进算法对于被低密度脉冲噪声污染图像的处理可取得令人满意的效果,图像被严重污染时,这些算法得到的结果均不理想。针对这一缺陷,基于文献[1]提出的一种滤波算法进行改进。首先,利用极值法对图像进行检测,判断出噪声及非噪声点;其次,设置滤波模板的最小及最大尺寸,对噪声点进行窗口逐渐增大的滤波处理。计算机模拟实验结果及对SAR图像滤波结果表明:该滤波算法在噪声去除及边缘和图像细节保持上优于标准中值滤波及其一些改进算法。  相似文献   

Effects of the low-frequency zonal wind variation on the high frequency atmospheric variability over the tropics     

K. P. Sooraj  Daehyun Kim  Jong-Seong Kug  Sang-Wook Yeh  Fei-Fei Jin  In-Sik Kang 《Climate Dynamics》2009,33(4):495-507

Recently, there is increasing evidence on the interaction of atmospheric high-frequency (HF) variability with climatic low-frequency (LF) variability. In this study, we examine this relationship of HF variability with large scale circulation using idealized experiments with an aqua-planet Atmospheric GCM (with zonally uniform SST), run in different zonal momentum forcing scenarios. The effect of large scale circulation changes to the HF variability is demonstrated here. The HF atmospheric variability is enhanced over the westerly forced region, through easterly vertical shear. Our study also manifests that apart from the vertical wind shear, strong low-level convergence and horizontal zonal wind shear are also important for enhancing the HF variance. This is clearly seen in the eastern part of the forcing, where the HF activity shows relatively maximum increase, in spite of similar vertical shear over the forced regions. The possible implications for multi-scale interaction (e.g. MJO–ENSO interaction) are also discussed.  相似文献   

风廓线雷达估算大气返回信号功率方法研究   总被引：3，自引：1，他引：2  

马建立  阮征  葛润生  何建新 《气象科技》2009,37(1):89-92

基于风廓线雷达大气返回信号功率谱中噪声电平的估算方法,统计分析了北京延庆对流层风廓线雷达（CFL-08）2006年10～12月的探测数据。对该频段风廓线雷达环境噪声的空间和时间变化进行了分析,观测期间环境噪声在5km以下随高度递减,10月的平均环境噪声大于11月、12月的平均分布。给出目前风廓线雷达用信噪比估算大气返回信号功率的两种方法,并对两种方法进行了环境噪声的剔除,经过修正后的大气返回信号功率输出结果趋于一致。  相似文献   

基于风廓线雷达资料的暴雨天气过程分析   总被引：4，自引：1，他引：3  

董保举  刘劲松  高月忠 《气象科技》2009,37(4):411-414

2008年6月1～2日大理市暴雨过程的风廓线雷达资料和每小时的雨量资料分析发现：暴雨过程具有明显的中小尺度系统影响特征,雷达水平风廓线资料可以很直观地显示随时间变化风场的垂直结构;高空气流的向下脉动与降水强度的增强有着紧密的联系;风廓线雷达产品（垂直速度、折射率结构常数和信号噪声比）清楚地反映降水的开始、结束以及降水的强度。  相似文献   

风廓线雷达回波信号强度定标方法   总被引：4，自引：1，他引：3       下载免费PDF全文

钟刘军  阮征  葛润生  陈钟荣  任京伟  沈祥林  张哲  魏艳强 《应用气象学报》2010,21(5):598-605

风廓线雷达返回信号功率定标通常通过返回信号信噪比和系统噪声功率的估算得到。该方法存在着噪声电平的确定、外部噪声等不确定性因素,影响了定标的精度。采用信号源分别对接收机和信号处理器进行定量测试,进而对雷达系统进行定标,是另一种可行的办法,该文利用这种方法对CFL-03风廓线雷达进行了定标,并利用该雷达在东莞2009年7月和8月探测资料与广州S波段天气雷达和地面雨量计资料进行比较。结果表明:用该定标方法得到的回波强度与天气雷达回波强度和地面雨量计资料估算的回波强度基本一致,平均标准差在1 dB左右,表明这种定标方法是可行的。  相似文献   

中国季降水量的气候噪声和潜在可预报性估计   总被引：2，自引：1，他引：1  

赵晓川  吴洪宝  何浪 《南京气象学院学报》2008,31(6):819-827

利用中国130个测站1961—2004年的日降水量资料,使用低频白噪声延伸法和方差分析法估计了中国季降水量的气候噪声方差和潜在可预报性。结果表明：中国季降水量的气候噪声方差由南向北、由沿海向内陆逐渐减小,且有明显的季节变化,夏季最高,其次是春秋季,冬季最小,而且内陆的季节变化比东南沿海的季节变化显著。季降水量的潜在可预报性有较大的季节和区域差异,但总体来说,全国大部分地区的季降水量是潜在可预报的。以绝对误差小于均方差0.68倍作为预测正确标准,全国大部分地区季降水量的预报正确率上限为50%-60%。  相似文献