基于地面三维激光扫描数据的快速建模

三维激光扫描技术具有速度快、精度高、自动化程度高并且不与物体直接接触等诸多优点,现已应用于古建筑保护、数字城市、工业生产、地形测绘等不同领域。本文利用地面三维激光扫描仪对校内樱花园手形建筑物进行扫描,获取该目标物的点云数据,并对获取的点云数据进行拼接、去噪处理。同时,利用点云数据处理软件Geomagic对目标物进行快速的三维模型重建并达到了预期的效果。     

基于法向量密度聚类的LiDAR点云屋顶面提取

针对现有算法从LiDAR点云中提取复杂建筑物屋顶面不完整、阈值难以设置的问题,提出一种结合点云空间分布的法向量密度聚类提取屋顶面点云方法。通过构建Delaunay三角网,计算建筑物LiDAR点云的法向量;在分析建筑物点云空间和法向量分布特点的基础上,定义一种邻域关系度量屋顶面点云之间的相似性,并利用提出的算法聚类建筑物点云,得到屋顶面片点云粗提取结果;通过构建屋顶面片缓冲区,经面片处理得到建筑物各屋顶面的完整点云。选取不同复杂程度的建筑物进行实验,结果表明,算法能有效提取复杂建筑物屋顶面点云,具有较好的适应性,并能为建筑物三维重建提供可靠的屋顶面信息。     

隧道三维点云孔洞修复方法

针对隧道三维激光扫描点云中的孔洞,设计一种基于断面轮廓的孔洞修复方法。隧道具有深长性与截面恒定性两大特征,文中基于这两大特征,利用间邻稳定轮廓拟合完整隧道修复孔洞。该方法能够对三维激光扫描点云进行圆柱投影,利用Delaunay三角构网,提出基于隧道表面三角网的孔洞识别方法,最后根据相邻隧道轮廓相似的特点,利用相邻的轮廓对孔洞进行修复。该方法能很好的修复孔洞并保留隧道结构细节,并以真实的隧道扫描数据验证算法的有效性和可靠性。     

地理国情监测技术路线研究

针对目前地理国情监测过程中遇到的信息采集涉及行业广、种类多、工作繁琐等问题,该文提出了一种新的技术路线,并详细探讨了不同部门、不同行业信息的获取方式。对于基础地理信息采集时地理国情及地表覆盖分类中存在的特殊道路、特殊河流、特殊房屋信息难以采集的情况,给出具体采集办法,提高了采集效率和采集精度;规范地理国情监测框架要求的其他部门、行业信息采集标准,并针对数据量大、类型复杂、调用部门多等问题,提出以云数据库存储数据,解决了后期数据库需多次扩展问题。通过分析与研究表明:此技术路线具有良好的可行性,采用此技术路线可有效采集地理信息并进行数据整合。     

谈大数据时代的“云控制”摄影测量

在当今大数据时代,影像数据采集方式的多样化、高效化、便捷化产生的摄影测量影像大数据需要高效、自动与智能的处理。然而,作为传统摄影测量几何定位主要控制数据的外业控制点,其获取的复杂性与低效性仍然是制约摄影测量处理效率的关键因素。针对该问题,本文提出了"云控制"摄影测量的概念,以带有地理空间信息的数据作为几何控制替代外业控制点,通过自动匹配(或配准)获取大量密集的控制信息;并介绍了基于影像、矢量和LiDAR点云的3种"云控制"摄影测量技术;最后对"云控制"摄影测量的应用前景进行了展望并对其问题进行了讨论。     

一种利用点云邻域信息的建筑物屋顶面高精度自动提取方法

从LiDAR数据中高精度地提取建筑物屋顶面是构建屋顶面拓扑关系、实现建筑物三维模型重建的关键。本文针对现有算法提取复杂建筑物屋顶面适应性较差、精度较低等问题,提出了一种利用点云邻域信息的建筑物屋顶面高精度自动提取方法。通过主成分分析计算点云特征,构建特征直方图,选取可靠种子点;利用提出的局部点云法向量分布密度聚类算法聚类种子点,快速准确地提取初始屋顶面片;构建基于邻域信息的投票模型,有效地解决屋顶面竞争现象。试验结果表明,本文方法可自动、高精度地提取屋顶面,对不同复杂程度的建筑物具有较好的适应性,能为建筑物三维模型重建提供可靠的屋顶面信息。     

基于AgisoftPhotoscan的图像三维重建及精度研究

通过普通相机获取图像信息,计算三维空间物体的几何信息,重建和分析物体的基本原理;了解图像处理软件Agisoft Photoscan的工作流程,并设计实验;通过未检校的普通数码相机对某雕塑头像和亭子进行拍摄,使用Agisoft Photoscan软件对图像进行处理,得到三维点云数据,进行物体三维重建,验证三维重建的有效性;通过提取和实测预设对比点的三维坐标值,求取误差,验证在百幅以内的图像建模误差在1cm以内。此方法可应用到表面复杂的异形物体建模中。     

基于三维激光扫描的校园建筑物三维建模研究

"数字校园"建设是科技发展的必然趋势,为加快这一进程,本次研究将地面三维激光扫描技术应用到大学校园。本文以Z+F IM AGER 5010c地面三维激光扫描仪采集到的吉林建筑大学基础实验楼数据为基础,运用3ds max、Auto CAD、Point Cloud等建模软件建立三维模型。同时将依据点云数据建立的实体模型与实际测量数据进行对比和精度分析,验证了地面三维激光扫描仪在建筑物三维模型建立中的精度和可靠性。     

THE CONTRASTS BETWEEN STRONG AND WEAK MJO ACTIVITY OVER THE EQUATORIAL WESTERN PACIFIC IN WINTER

This paper investigates the contrasts between strong and weak Madden-Julian Oscillation (MJO) activity over the equatorial western Pacific during winter using the NCEP reanalysis data. It is shown that the MJO over the equatorial western Pacific in winter shows significant interannual and interdecadal variabilities. During the winters with strong MJO activity, an anomalous cyclonic circulation lies east of the Philippines, strong anomalous easterlies control the equatorial eastern Pacific, and anomalous westerlies extend from the Indian Ocean to the western Pacific in the lower troposphere, which strengthens the convergence and convection over the equatorial western Pacific. The moisture convergence in the lower troposphere is also enhanced over the western Pacific, which is favorable to the activity of MJO. Eastward propagation is a significant feature of the MJO, though there is some westward propagation. The space-time spectral power and center period of the MJO are higher during strong MJO activity winters. The anomalous activity of MJO is closely related to the sea surface temperature (SST) and East Asian winter monsoon (EAWM). During strong MJO activity winters, there are positive/negative anomalies at high/low latitudes in both sea level pressure and 500 hPa geopotential height, and the temperature is lower over the central part of the Chinese mainland, which indicates a strong EAWM. China experiences more rainfall between the Yellow and Yangtze Rivers, but less rainfall south of the Yangtze River. The SSTA is negative near the Taiwan Island due to the impact of strong EAWM and shows a La Ni?a pattern anomaly over the eastern Pacific. During the weak MJO activity winters, the situation is reversed.     

THE EFFECT OF EQUATORIAL CENTRAL PACIFIC SSTAS ON THE INTERANNUAL VARIATION OF PRECIPITATION OVER SOUTHWEST CHINA DURING SPRING

The interannual variations of rainfall over southwest China (SWC) during spring and its relationship with sea surface temperature anomalies (SSTAs) in the Pacific are analyzed, based on monthly mean precipitation data from 26 stations in SWC between 1961 and 2010, NCEP/NCAR re-analysis data, and Hadley global SST data. Sensitivity tests are conducted to assess the response of precipitation in SWC to SSTAs over two key oceanic domains, using the global atmospheric circulation model ECHAM5. The interannual variation of rainfall over SWC in spring is very significant. There are strong negative (positive) correlation coefficients between the anomalous precipitation over SWC and SSTAs over the equatorial central Pacific (the mid-latitude Pacific) during spring. Numerical simulations show that local rainfall in the northwest of the equatorial central Pacific is suppressed, and a subtropical anticyclone circulation anomaly is produced, while a cyclonic circulation anomaly in the mid-latitude western Pacific occurs, when the equatorial Pacific SSTAs are in a cold phase in spring. Anomalous northerly winds appear in the northeastern part of SWC in the lower troposphere. Precipitation increases over the Maritime Continent of the western equatorial Pacific, while a cyclonic circulation anomaly appears in the northwest of the western equatorial Pacific. A trough over the Bay of Bengal enhances the southerly flow in the south of SWC. The trough also enhances the transport of moisture to SWC. The warm moisture intersects with anomalous cold air over the northeast of SWC, and so precipitation increases during spring. On the interannual time scale, the impacts of the mid-latitude Pacific SSTAs on rainfall in SWC during spring are not significant, because the mid-latitude Pacific SSTAs are affected by the equatorial central Pacific SSTAs; that is, the mid-latitude Pacific SSTAs are a feedback to the circulation anomaly caused by the equatorial central Pacific SSTAs.