排序方式: 共有40条查询结果,搜索用时 15 毫秒
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DS证据理论在SAR图像边缘检测中的应用 总被引:2,自引:0,他引:2
提出了一种新的基于DS证据理论的SAR图像多尺度边缘检测方法.该方法利用DS证据理论融合多级尺度ROA算子输出响应,在融合过程中引入检测不确定性.并通过分析ROA算子检测门限与虚警率的关系设计基本可信度分配函数(BPAF),使得检测不确定性在门限处达到最大值.实验通过检测结果比较以及列表分析,表明本文算法能够有效降低边缘检测不确定性. 相似文献
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Luciano Nicastro & Simon Johnston 《Monthly notices of the Royal Astronomical Society》1998,293(3):L65-L67
We report the discovery of a pulsar with a Galactic longitude of 304° and a dispersion measure (DM) of 875 cm−3 pc. PSR J1302−63 has the second largest DM of any known pulsar. It is also relatively weak, with a flux density of only 0.2 mJy at 1500 MHz. This is the 13th pulsar with a DM greater than 400 cm−3 pc located more than 50° from the Galactic Centre. It provides further evidence for a significant pulsar population and enhanced electron densities within the major spiral arms. 相似文献
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由于自然地表像元在长期观测中容易发生时空失相干,利用时序InSAR(Synthetic Aperture Radar Interferometry)技术对其开展形变监测会面临可用形变测量点不足的挑战。针对这一问题,提出一种改进的小基线(Small Baseline Subset,SBAS)方法。该方法改进了传统SBAS中初始高相干像元筛选及相位滤波过程:首先利用拟合优度检验,并结合相干性阈值条件来识别同质像元;然后根据同质像元数量将所有像元分成2部分,即PS(Persistent Scatterers)候选点和DS(Distributed Scatterers)候选点;其次分别在这两部分像元中开展初始高相干PS点及DS点筛选;最后对选出的高相干PS点及DS点进行加权相位滤波。利用覆盖北京平原区西北部(含城区及山区)的27景ENVISAT ASAR影像开展的形变监测实验表明:与2个参考方法相比,该方法能够有效扩展形变结果上的测量点数量和覆盖范围,测量点数量分别提高了22.6%及27.6%,且自然地表的形变测量点密度得到了明显提升。同时,研究区形变结果与4个连续GPS站的位移数据有很好的一致性,证明了该方法在地表形变反演中的有效性及优越性。 相似文献
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本系统通过多种方法采集并分析数据,采用3DS Max进行建筑三维建模,结合并利用Skyline组件进行系统开发,实现对某房地产小区的三维虚拟场景开发。该系统不但提供三维游览服务,同时也实现了地理信息系统的多种三维分析功能。 相似文献
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依据3DS MAX软件制作三维图的原理和方法,制作了东华理工学院三维校园图。文中详细介绍了利用3DS MAX技术制作三维图的过程.包括:从资料的收集、底图的生成、立体模型的制作、三维贴图到校园立体图的渲染输出等。对在3DS MAX环境下建筑物的建模,材质贴图,灯光设置等关键技术作了重点阐述。并就三维场景的虚拟漫游的图像文件格式、渲染的时间等技术因素的设置作了必要的论述。制作的校园立体图既具有传统鸟瞰图的特点又具有普通地图特点,所包含的信息量远比两者多,并且可利用它作地理信息系统底层数据,用于实现三维仿真及属性查询等多种用途。 相似文献
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合成孔径雷达干涉测量(Interferometric Synthetic Aperture Radar,InSAR)时序分析技术,利用时域上多幅SAR图像选择时间基线、空间基线满足一定条件的干涉对进行干涉,通过建立干涉相位形变模型获取地表形变信息。InSAR时序分析技术改善了差分干涉测量中时空失相干、大气延迟等问题,广泛应用于有关形变监测的多个领域,并逐渐成为获取长期地表形变趋势的重要手段。在InSAR时序分析中,针对不同应用选取合适的高相干目标选取方法,获得可靠的高相干目标,是获取精确可靠的地表形变信息的基础。本文通过分析永久散射体(Permanent Scatterers,PS)、分布式散射体(Distributed Scatterers,DS)选取方法的理论模型及其算法,研究其适用地物目标类型的异同,并分析、归纳总结了幅度相关法、相位分析法、信号杂波比法、相干性统计法等不同的高相干目标选取方法的优缺点。最后,以阿尔金断裂带西段部分区域为研究区,分别采用具有代表性的PS、DS选取方法开展该研究区域的选点实验,结果表明该研究区域DS选取方法比PS选取方法适用。本文方法为解决在不同地理区域进行应用研究时选取合适的选点方法提供参考。 相似文献
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The equilibrium form of the fluvial long profile has been used to elucidate a wide range of aspects of landscape history including tectonic activity in tectonic collision zones, and in continental margin and other intraplate settings, as well as other base‐level changes such as due to sealevel fluctuations. The Hack SL form of the long profile, which describes a straight line on a log–normal plot of elevation (normal) versus distance (logarithmic), is the equilibrium long profile form that has been most widely used in such studies; slope–area analysis has also been used in recent years. We show that the SL form is a special case of a more general form of the equilibrium long profile (here called the DS form) that can be derived from the power relationship between stream discharge and downstream distance, and the dependence of stream incision on stream power. The DS form provides a better fit than the SL form to river long profiles in an intraplate setting in southeastern Australia experiencing low rates of denudation and mild surface uplift. We conclude that, if an a priori form of the long profile is to be used for investigations of regional landscape history, the DS form is preferable. In particular, the DS form in principle enables equilibrium steepening due to an increase in channel substrate lithological resistance (parallel shift in the DS plot) to be distinguished from disequilibrium steepening due to long profile rejuvenation (disordered outliers on the DS plot). Slope–area analysis and the slope–distance (DS) approach outlined here are complementary approaches, reflecting the close relationship between downstream distance and downstream catchment area. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献