利用方向场进行指纹图像快速分区     

陈晖  舒欣  殷建平 《武汉大学学报(信息科学版)》2012,37(2):165-169,124

指纹方向场真实地反映了指纹图像中本质的纹理特征,包括指纹的基本形状、结构和走势。方向场图像在局部区域表现相对一致,而在全局范围则表现出较大的差异。基于方向场对指纹图像进行分区,可以提供一种有用的辅助性全局特征。本文提出了一种指纹图像快速分区方法,并结合一种基于局部描述子的指纹图像匹配算法给出了其应用实例。在FVC2004DB1数据集上设计了实验,结果表明,这种分区方法能有效地提高识别率,同时缩短处理时间。  相似文献   

基于COM-GIS的软件模版快速搭建及应用   总被引：2，自引：1，他引：1  

卓云  何政伟  赵银兵  南希  李旭龙 《地理空间信息》2012,10(4):105-106,109

针对GIS平台,介绍了在Microsoft Visual Studio平台下进行用户自定义常用基础功能函数模版的提前编写和集成。为了方便C/S、B/S系统架构下的集成,根据项目需求,快速抽取了相应的基础功能函数,完成了基础功能集成。基础功能函数的开放性和兼容性对项目的快速搭建、项目核心功能处理有重大影响。  相似文献   

一种适用于黄土斜坡地震稳定性快速评估的综合判别方法——以宁夏西吉县为例          下载免费PDF全文

杨顺  常晁瑜  余思汗  王银  刘超 《地震工程学报》2022,44(1):54-61

选取宁夏西吉县为目标区,对区内1920年海原8.5级特大地震所诱发的347处黄土地震滑坡进行野外调查,获取了详实的基础数据.在此基础上结合遥感影像解译,总结了研究区内黄土地震滑坡的分布特征,并依此提出了宏观、定性的黄土斜坡地震稳定性快速判别方法.基于分布特征选取了坡高、坡角、坡向及地震动强度作为基本参数,应用MLP神经...  相似文献   

A Composite Approach of Radar Echo Extrapolation Based on TREC Vectors in Combination with Model-Predicted Winds   总被引：3，自引：0，他引：3  

LIANG Qiaoqian  FENG Yerong  DENG Wenjian  HU Sheng  HUANG Yanyan  ZENG Qin  CHEN Zitong 《大气科学进展》2010,27(5):1119-1130

Extending the lead time of precipitation nowcasts is vital to improvements in heavy rainfall warning, flood mitigation, and water resource management. Because the TREC vector (tracking radar echo by correlation) represents only the instantaneous trend of precipitation echo motion, the approach using derived echo motion vectors to extrapolate radar reflectivity as a rainfall forecast is not satisfactory if the lead time is beyond 30 minutes. For longer lead times, the effect of ambient winds on echo movement should be considered. In this paper, an extrapolation algorithm that extends forecast lead times up to 3 hours was developed to blend TREC vectors with model-predicted winds. The TREC vectors were derived from radar reflectivity patterns in 3 km height CAPPI (constant altitude plan position indicator) mosaics through a cross-correlation technique. The background steering winds were provided by predictions of the rapid update assimilation model CHAF (cycle of hourly assimilation and forecast). A similarity index was designed to determine the vertical level at which model winds were applied in the extrapolation process, which occurs via a comparison between model winds and radar vectors. Based on a summer rainfall case study, it is found that the new algorithm provides a better forecast.  相似文献   

汶川地震触发的绵远河流域崩塌滑坡的特征   总被引：1，自引：1，他引：0  

李为乐  黄润秋  唐川  许强 《山地学报》2011,29(4)

利用地震后ALOS影像自动提取了汶川地震重灾区绵远河流域内的崩塌滑坡,结合野外调查共确定地震触发崩塌滑坡1 073处,面积48.5 km2.其中分布最广、数量最多的是浅层崩滑体;同时由于地震力作用强烈,触发了许多深层、高速、远程滑坡,并形成了大量的滑坡堰塞湖.汶川地震诱发的第二大滑坡文家沟滑坡就位于流域内,该滑坡是本次地震中滑动距离最远的滑坡.地震导致大量的碎屑物质堆积在沟道内或悬挂在斜坡上,为泥石流的发生提供了有利条件.基于GIS的统计分析表明,地震滑坡的空间分布主要受发震断层的控制,流域内的崩塌滑坡受到了映秀-北川断裂和江油-都江堰断裂的双重影响,主要分布于两断裂上盘的一定范围内;地层岩性影响着地震滑坡的类型,岩浆岩、白云岩等硬岩主要发育浅层崩滑体,而上硬下软的地层多发生大型滑坡;大部分崩塌滑坡都发生在海拔1 000～2 000 m的高程内;坡度是崩塌滑坡发生的主要控制因素之一,大部分崩塌滑坡发生在25°～55°的范围内;坡向对滑坡的分布也有一定的影响,背靠震源(发震断层)方向的斜坡比面向震源(发震断层)方向更容易发生滑坡.  相似文献   

FY-2C高时间分辨率扫描数据在强对流云团监测中的应用研究   总被引：6，自引：1，他引：5  

刘健  蒋建莹 《大气科学》2013,37(4):873-880

利用我国首次获取的静止气象卫星平均10 分钟观测间隔的高时间分辨率数据对2011 年6 月28 日～29日发生的一次强对流云团特征进行分析。Hovm?ller 分析图清晰地展示出在高时间分辨率观测条件下云团中心冷核的演变特征。高时间分辨率卫星资料与地面降水量进行联合分析,可推知对流云团中冷核的演变与地面小时降水量大值的落区间有很好的一致性;10 分钟雨量资料联合前推1 小时内7 次平均10 分钟观测间隔的卫星红外1通道亮温,分析可知地面雨量较大时,云顶像元亮温具有持续降低或维持低温状态的特点。反映出在对流性强降水中,冷且具有一定稳定性的云顶是产生大降水的主要特征。研究结果显示,静止气象卫星的高时间分辨率观测可很好地捕捉到强对流云团发展的演变特征,利用FY-2C 静止气象卫星红外1 通道亮温、红外1 通道与水汽通道亮温差在高时间分辨率观测中的时差特征变量,可实现对强对流云团初生的有效监测,为强对流云团的预测预报提供支撑。  相似文献   

海量遥感影像的存储与快速调度显示方法   总被引：2，自引：0，他引：2  

张涵斐  黄忠红  孟永军 《测绘与空间地理信息》2011,34(3):36-39,43

随着计算机技术的发展,计算机的存储和处理的功能越来越强大,但是仍然无法满足日益增加的海量信息处理的需要。因此研究如何利用有限的计算机内存,处理无限大小的数据,成为研究的重点。本文根据海量遥感影像数据的特点以及对海量遥感图像进行处理的需要,研究了实现海量图像数据快速显示的方法以及其数据库存储结构。主要包括图像重采样、影像金字塔生成技术、图像快速显示技术等。  相似文献   

Rapid repair of severely earthquake-damaged bridge piers with flexural-shear failure mode   总被引：1，自引：1，他引：0  

Zhiguo Sun  Dongsheng Wang  Xiuli Du  Bingjun Si 《地震工程与工程振动(英文版)》2011,10(4):553-567

An experimental study was conducted to investigate the feasibility of a proposed rapid repair technique for severely earthquake-damaged bridge piers with flexural-shear failure mode. Six circular pier specimens were first tested to severe damage in flexural-shear mode and repaired using early-strength concrete with high-fluidity and carbon fiber reinforced polymers (CFRP). After about four days, the repaired specimens were tested to failure again. The seismic behavior of the repaired specimens was evaluated and compared to the original specimens. Test results indicate that the proposed repair technique is highly effective. Both shear strength and lateral displacement of the repaired piers increased when compared to the original specimens, and the failure mechanism of the piers shifted from flexural-shear failure to ductile flexural failure. Finally, a simple design model based on the Seible formulation for post-earthquake repair design was compared to the experimental results. It is concluded that the design equation for bridge pier strengthening before an earthquake could be applicable to seismic repairs after an earthquake if the shear strength contribution of the spiral bars in the repaired piers is disregarded and 1.5 times more FRP sheets is provided.  相似文献   

利用余震法快速判定宏观震中的研究   总被引：2，自引：1，他引：1  

王伟锞  李志强  李晓丽 《震灾防御技术》2011,6(1):36-48

当前在震后快速响应阶段的盲场快速评估过程中,震中位置普遍采用速报震中,而速报震中与实际宏观震中之间存在客观的不一致性,会给震灾评估结果带来较大的误差。而在震后短时间内可用信息量极少的情况下,判断宏观震中的位置存在较大的困难,本文通过引入余震法,为震后快速判定宏观震中提出了新的思路。通过对1970年以来近40组破坏性地震的研究,利用余震法可在震后6h根据地震破裂性质推断宏观震中,其准确度、时效性都能为震后快速评估提供较为可靠的依据。  相似文献   

Physical modelling of rainfall‐ and snowmelt‐induced erosion of stony slope underlain by permafrost     

E. Vedie  J.‐L. Lagarde  M. Font 《地球表面变化过程与地形》2011,36(3):395-407

Physical modelling experiments have been carried out in a cold room to test on a small scale, the effects of water supply during the thaw of an experimental slope with permafrost. Permafrost was maintained at depth and a thin active layer was frozen and thawed from the surface. Data from the experiments relate to two different conditions, first with moderate rainfall, and second with heavy rainfall during the thaw period. When moderate rainfall is applied during thaw phases, the experimental slope is slightly degraded. At the scale of the experiment, erosion processes involve frost jacking of the coarse blocks, frost creep and gelifluction that induce slow and gradual down slope displacements of the active layer, but also small landslides leading to large but slow mass movements with short displacements. Changes in experimental slope morphology are marked by the initiation of a small‐scale drainage network and the development of a little crest line which shows a progressive upslope migration. With such boundary conditions, there is not enough water supply to evacuate downslope the whole of the eroded material and a topographic smoothing is observed. When heavy rainfall is applied during thaw periods, rapid mass wasting (small mud‐flows and debris flows) become prominent. Slope failures are largely controlled by the water saturation of the active layer and by the occurrence of steeper slopes. At the scale of the experiment, rates of erosion and maximum incision increase by about 100% leading to significant slope degradation with marked and specific scars comparable to gullying. These morphological changes are dependant on both the size and the frequency of catastrophic events. These experiments provide detailed data that could improve the knowledge of the physical parameters that control the initiation, at a small‐scale, of erosion processes on periglacial slopes with a thin active layer and/or with thin cover of mobilizable slope deposits. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献