共查询到19条相似文献，搜索用时 187 毫秒
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在三维视觉系统中 ,采用数字信号处理器 ( DSP)对三维视觉信息进行实时处理 ,可以提高处理三维视觉信息的运算速度。在实时采集处理系统的实现方案中 ,信号采集子系统与 DSP之间的数据通信方式 ,实时采集处理系统与 PC机之间的数据传输方式 ,也是影响三维视觉系统信息处理速度的两个重要因素。该系统采用双端口 RAM和中断方式进行数据传输 ,实现了信号采集子系统与 DSP、实时采集处理系统与 PC机的并行处理 ,以提高整个三维视觉系统信息的处理速度 相似文献
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针对利用X波段海浪雷达回波图像反演海浪参数(波高、波向、波周期)的需要,而海浪雷达回波信号的采集和存储是利用雷达回波图像序列反演海浪参数的必要前提,提出了基于PXI-9280 A/D采集卡对X波段海浪雷达回波进行采集的方案.具体介绍了PXI-9280 A/D采集卡的功能特性,海浪雷达回波信号样式,设计并完成了基于VC 6.0的采集和存储软件,并对使用该采集卡需要注意的实际问题给予说明.此外,还搭建了实验平台,给出了基于PXI-9280 A/D采集卡在我国南海某海域中采集数据并回放得到的海浪雷达回波图像,得到较满意的结果. 相似文献
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《中国海洋大学学报(自然科学版)》2017,(4)
多体散射环境下,本文提出一种非迭代的声学反演点散射体散射系数的方法。这种方法运用非向量数学运算,从而避免测量多基地响应矩阵,与现有的方法相比更容易实现。本文对两种布设环境数值仿真验证该方法的有效性,并在噪声环境下将本文方法与现有的两种非迭代反演方法进行比较。仿真结果表明:(1)反演公式中矩阵的条件数由布设环境决定,布设环境通过条件数影响反演结果;(2)噪声对反演结果的影响程度取决于布设环境;(3)布设环境对三种方法的影响程度不同,本文方法与另外两种方法在不同布设环境中各有优劣。 相似文献
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本文基于时间分布参数设置,利用伴随同化方法,反演了Ekman模型中随时间变化的风应力拖曳系数,并在孪生实验和实际实验中对该方法进行了验证。在孪生实验中,研究了参数反演结果对不同影响因素的响应,包括:风速分布、风应力系数分布、风应力系数初始猜测值、风应力系数独立变量个数、观测数据误差和观测的深度。孪生实验结果验证了伴随同化方法反演Ekman模型中时变风应力系数的有效性,具体包括如下五个方面结论:1)不同风速分布下均能成功反演出不同风应力拖曳系数分布; 2)反演结果对初始猜测值较为敏感,风应力系数初始猜测值越接近给定值,反演结果越好;3)风应力系数独立点个数的选取会显著影响反演结果,合理的选择有利于提高反演效率及减小观测数据误差;4)观测误差能够影响反演结果,观测数据误差在20%以下时能取得合理的反演结果; 5)反演结果对观测数据的表层和次表层流速更为敏感,这是由Ekman流的物理性质决定的。实际实验,利用百慕大锚系试验平台的风速和流速数据,去除周期性潮流和地转流成分后得到Ekman流成分,并作为观测输入到该同化模型,反演出了适用于该区域和该时段的随时间变化的风应力系数。通过比较模拟流速和观测流速,证明利用伴随同化方法能从实测数据中反演出合理的时变风应力系数,对于海洋模型风应力系数的确定是一项有益的尝试。 相似文献
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QuikSCAT风矢量快速反演的后向散射系数预处理算法 总被引：1，自引：0，他引：1
根据QuikSCAT的工作特点,提出了一种通过对QuikSCAT风矢量单元后向散射系数进行预处理,从而提高反演效率的快速算法.预处理算法将每个风矢量单元对应的后向散射系数按测量几何关系分为外波束前视、内波束前视、内波束后视、外波束后视观测4组,取每组后向散射系数平均值作为对应组的测量结果,再将作分组平均处理后的后向散射系数代入反演流程中,使得求目标函数值步骤中搜索查找表的次数减少到4次.与JPL业务化运行所选用的算法相比较,快速算法仅以损失少量风向信息为代价,将风矢量反演所需计算量减少到原来的1/3,极大地提高了运算效率,缩短了风矢量反演所需的时间,可为应对突发灾难性天气等特殊情况争时间. 相似文献
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在过去的十几年中,海洋可控源电磁法的迅猛发展在油气勘探中起到了重要的作用。在浅海环境中,常见的两种可控源电磁法的数据采集系统采用海底基站式（Sea Bed Logging（SBL））,以及拖缆式（Towed Streamer electromagnetics（TSEM））两种模式。本文的研究目的是研究在不同水深条件下,两种数据采集系统的工作模式以及海水对其的影响。为了更好的比较两种数据采集方式,本文采用了三种不同的分析方法：一维敏感度模型,二维油藏敏感指数,Occam反演。一维敏感度模型能够迅速的给出结果,但是由于结果的信息量有限,不足以给定准确的结论。二维油藏敏感指数可以依据正演的结果快速的给定一个水深和油藏敏感度的关系。Occam反演方法用于对合成数据进行反演计算,估计地下介质电阻率参数。为了更好的评价反演结果,本文引入了横向电阻异常率（ATR）。通过对合成数据的反演结果的分析,本文得出以下结论：在浅水环境中,SBL和TSEM数据采集系统都可以提供较高的分辨率,对高电阻层有很好的敏感度。在深水环境中,SBL数据采集系统具有明显的优势。ATR对于反演的电阻率参数结果具有很好的评价作用。 相似文献
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由风、雨、舰船、海洋生物以及工业等因素形成的海洋环境噪声,是海洋中永恒存在的声场, 包含频段丰富。无论是在水下目标的主动探测还是被动探测过程中,海洋环境噪声都被认为是水声信道中的干扰因素。但海洋环境噪声包含诸多水体、海面、海底和海洋生物等信息,可以通过反演获取海水、海底等各种信息。概述了国内外基于海洋环境噪声声成像的发展现状,并预测了该领域技术发展趋势。基于海洋环境噪声进行的水下目标探测,在探测开发海洋资源、维护国家主权和国家海洋环境安全等方面具有重要意义。 相似文献
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林俊轩 《中国海洋大学学报(自然科学版)》1996,(4)
采用场匹配处理法反演层系介质参数，在匹配处理前先对层系模型参数进行预估。参数预估将大大地减少匹配运算时间。模拟实验的反演结果与取样实测结果相当符合 相似文献
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在三维地震资料采集中,由于观测系统本身的原因及采集条件等因素在地震数据体上形成了采集脚印,在海域资料中表现为条带状的振幅异常。采集脚印的存在,影响着地震资料的成像质量以及后续的地震反演、属性分析和AVO研究。尤其在水合物地震资料分析中,精确的成像以及可靠的地震反演、地震属性分析关乎精确识别水合物分布。因此本文详细分析了神狐海域地震资料的采集脚印现象并采取了有效的压制技术,为后续通过地震反演、属性分析和AVO反演研究精细刻画、描述构造形态、预测天然气水合物储层分布和预测天然气水合物有利富集区带提供了可靠的地震资料。 相似文献
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As for the satellite remote sensing data obtained by the visible and infrared bands inversion, the clouds coverage in the sky over the ocean often results in missing data of inversion products on a large scale, and thin clouds di?cult to be detected would cause the data of the inversion products to be abnormal. Alvera et al.(2005) proposed a method for the reconstruction of missing data based on an Empirical Orthogonal Functions (EOF) decomposition, but his method couldn’t process these images presenting ex... 相似文献
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为了研究频率域2.5维非线性共轭梯度反演在海洋天然气水合物探测中的实际应用效果,利用美国Scripps研究所在South Hydrate海域采集的可控源电磁探测数据进行2.5维非线性共轭梯度反演计算,结合其他地球物理方法在同一海区的研究结果,综合分析2.5维反演计算的准确性和有效性。结果表明,非线性共轭梯度反演能够清晰地反映出该区域海底面以下1~2 km地层的电导率结构分布,其局部反演结果与地震反射、地震层序、测井分析结果基本一致,且对小尺寸异常、浅层高阻体分辨力较强,尤其在海洋天然气水合物探测方面具有较大潜力。 相似文献
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This study concerns the determination of a regional geoid model in the North Atlantic area surrounding the Azores islands by combining multi-mission altimetry from the ERS (European Remote Sensing) satellites and surface gravity data. A high resolution mean sea surface, named AZOMSS99, has been derived using altimeter data from ERS-1 and ERS-2 35-day cycles, spanning a period of about four years, and from ERS-1 geodetic mission. Special attention has been paid to data processing of points around the islands due to land contamination on some of the geophysical corrections. A gravimetric geoid has been computed from all available surface gravity, including land and sea observations acquired during an observation campaign that took place in the Azores in October 1997 in the scope of a European and a Portuguese project. Free air gravity anomalies were derived by altimetric inversion of the mean sea surface heights. These were used to fill the large gaps in the surface gravity and combined solutions were computed using both types of data. The gravimetric and combined solutions have been compared with the mean sea surface and GPS (Global Positioning System)-levelling derived geoid undulations in five islands. It is shown that the inclusion of altimeter data improves geoid accuracy by about one order of magnitude. Combined geoid solutions have been obtained with an accuracy of better than one decimetre. 相似文献
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This study concerns the determination of a regional geoid model in the North Atlantic area surrounding the Azores islands by combining multi-mission altimetry from the ERS (European Remote Sensing) satellites and surface gravity data. A high resolution mean sea surface, named AZOMSS99, has been derived using altimeter data from ERS-1 and ERS-2 35-day cycles, spanning a period of about four years, and from ERS-1 geodetic mission. Special attention has been paid to data processing of points around the islands due to land contamination on some of the geophysical corrections. A gravimetric geoid has been computed from all available surface gravity, including land and sea observations acquired during an observation campaign that took place in the Azores in October 1997 in the scope of a European and a Portuguese project. Free air gravity anomalies were derived by altimetric inversion of the mean sea surface heights. These were used to fill the large gaps in the surface gravity and combined solutions were computed using both types of data. The gravimetric and combined solutions have been compared with the mean sea surface and GPS (Global Positioning System)-levelling derived geoid undulations in five islands. It is shown that the inclusion of altimeter data improves geoid accuracy by about one order of magnitude. Combined geoid solutions have been obtained with an accuracy of better than one decimetre. 相似文献
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Pan Jiayi Wang Junqin Wang Yanfeng Zhang Xinmei Yuan Yeli Zheng Quan''an 《海洋学报(英文版)》1999,18(4):523-533
INTRODUCTIONThegeoidistheiargeopotentials~econfidingmostlywiththemeanseasurfaceandisdenotedastheheightrelativetotheidealelliPSes~eoftheearth.Thegeoidundulationsinglobalaceareupto100m.TheunevenstructureOftheearthgivesrisetotheunevenfeatureofthecitysot... 相似文献
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海底浅层地质灾害的高分辨率地震识别技术 总被引：1，自引：0，他引：1
将渤海某油田最新采集的二维高分辨率资料处理解释后,结合区域地球物理及地质概况,利用地震相分析、波阻抗反演、井(孔)震标定等深层油气勘探的成熟技术,系统研究了各类海底浅层地质灾害因素的成因、特征、危害及展布规律,总结了一套完整的利用高分辨率地震识别海底浅层地质灾害的技术方法。结果表明,浅层断裂、浅层气和埋藏古河道是研究区海底浅层发育的主要地质灾害因素,通过刻画不同期次地质灾害因素的类型及其分布范围,为今后该油田海上施工提供了可靠的工程地质调查成果。因此,高分辨率地震技术能够很好地应用于海底浅层地质灾害的识别。 相似文献
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The techniques of linearized least squares inversion (LLSI) and simulated annealing (SA) are both used to invert a series of synthetic and real normal-incidence, geo-acoustic sonar returns for estimates of impedance versus two-way travel time in the top several meters of ocean floor sediment. The objective is to determine the better (faster, more accurate) method for inverting this class of data. LLSI uses an over parameterized earth, i.e., one composed of layers whose thickness corresponds to a travel time equal to the sample interval. This makes the inverse problem quite large, but also makes it nearly linear. SA uses a more efficient parameterization, one whose layers have variable thickness as well as variable impedance. Because of the relatively narrow frequency band (~1 octave at 20 dB down from the peak) the time domain signal is oscillatory and inversion for layer thickness is nonlinear. Results show greater time efficiency in solving the large linear problem (LLSI) than in solving the small nonlinear problem (SA). However, in both cases almost all of the waveform energy was modeled, indicating that essentially all the information in the data had been successfully recovered. The inversions are applied to 10-20 kHz field data acquired offshore Florida, and several techniques are employed to enhance the effectiveness of each inversion method 相似文献