共查询到19条相似文献，搜索用时 109 毫秒
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海道测量定位与测深的延时效应 总被引：8，自引：5，他引：3
本文对海道测量中定位与测深的延时效应进行了分析,给出了对系统性延时效应的探测改正方法。香港海域的试验数据证实了该方法的有效性,该方法可编制为一个附加软件用于高精度海道测量的数据处理。 相似文献
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为了对海道测量中测线定位精度进行评估,以及为补偿测线系统误差的需要,提出了实测定位折线模型,同时在利用小波降噪算法求得拟合航迹线的基础上,提出了拟合定位测线的概念,针对测线的不同形态给出了拟合测线的另外两种模型,即拟合直线和拟合折线。仿真实验表明:提出的三种测线模型均满足1:2 000以下比例尺测图要求;在满足定位精度和测线正横水深梯度不超限的约束条件下,可以用拟合测线代替原始测线进行数据的后处理;三种测线模型对系统误差不存在"淹没效应";拟合折线可以方便地减弱测线内受方向、船速等系统误差的影响。 相似文献
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DGPS（DifferentialGlobalPositioningSystem）测量技术即差分定位技术,包括实时差分和后处理差分定位技术,正在远海和近海测量中得到广泛应用。后处理差分定位与微波定位及GPS实时差分定位相比,具有作用距离远,不受基准台与船台之问的障碍物影响以及减少基准台等优点。对于近海大比例尺（大于1：1万）测量,可采用实时差分定位的方法,而小于1：1万中小比例尺海底地形图测绘及海上其他工程测量,采用后处理差分定位,既能满足精度要求,又能提高工作效率。本文主要介绍利用DGPS后处理定位方法,在测绘广西沿海1：5万海底地形图中的应用情况。 相似文献
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对海洋二维地震勘探导航定位数据的后处理方法进行了分析研究。在Sprint后处理软件中,根据不同观测值的特点采取不同的处理方法,对某些参数的选择提出建议,并总结了一些后处理经验。通过举例比较,体现了合理的后处理在纠正错误、提高定位质量上的作用。 相似文献
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水尺与压力式水位计数据关系的算法研究 总被引：1，自引：0，他引：1
针对海道测量中在同一验潮点人工水尺与压力式水位计同步水位观测所得不同的潮位数据,分别绘制潮位曲线,从两条相关的曲线数据中应用三次样条和拟合数学函数模型,利用计算机程序确定曲线间的线性关系,从而根据压力式水位计测得的数据确定的关系得出真实的潮位数据。 相似文献
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H／HCZ-02型水深测量自动化系统集测量定位、数据采集、实时控制和处理于一体，其工作模式适合新时期海道测量的需要。立足发掘现有设备的潜力，介绍了该型设备的主要特点及在海洋重力、磁力等海洋综合测量中的应用。 相似文献
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针对多波束测深系统换能器横向安装偏差校正不完善的问题,提出了一种以近似平面估算换能器横向安装偏差的方法。分析了横向安装偏差对海底地形测量的影响,采用选权迭代的方式对子区平坦海底进行平面拟合,以平面拟合系数求解模型作为计算平面方程的推值模型,利用两近似平面夹角确定换能器横向安装偏差,将计算结果带入CARIS软件船配置文件中,完成对换能器横向安装偏差的二次校正。实验结果表明,该法能有效探测换能器横向安装偏差,且经二次校正后的主检测线交叉区域水深值具有较好一致性,满足海道测量规范要求。 相似文献
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Shallow-water imaging multibeam sonars: A new tool for investigating seafloor processes in the coastal zone and on the continental shelf 总被引：8，自引：1，他引：8
John E. Hughes Clarke Larry A. Mayer David E. Wells 《Marine Geophysical Researches》1996,18(6):607-629
Hydrographic quality bathymetry and quantitative acoustic backscatter data are now being acquired in shallow water on a routine basis using high frequency multibeam sonars. The data provided by these systems produce hitherto unobtainable information about geomorphology and seafloor geologic processes in the coastal zone and on the continental shelf.Before one can use the multibeam data for hydrography or quantitative acoustic backscatter studies, however, it is essential to be able to correct for systematic errors in the data. For bathymetric data, artifacts common to deep-water systems (roll, refraction, positioning) need to be corrected. In addition, the potentially far greater effects of tides, heave, vessel lift/squat, antenna motion and internal time delays become of increasing importance in shallower water. Such artifacts now cause greater errors in hydrographic data quality than bottom detection. Many of these artifacts are a result of imperfect motion sensing, however, new methods such as differential GPS hold great potential for resolving such limitations. For backscatter data, while the system response is well characterised, significant post processing is required to remove residual effects of imaging geometry, gain adjustments and water column effects. With the removal of these system artifacts and the establishment of a calibrated test site in intertidal regions (where the seabed may be intimately examined by eye) one can build up a sediment classification scheme for routine regional seafloor identification.When properly processed, high frequency multibeam sonar data can provide a view of seafloor geology and geomorphology at resolutions of as little as a few decimetres. Specific applications include quantitative estimation of sediment transport rates in large-scale sediment waves, volume effects of iceberg scouring, extent and style of seafloor mass-wasting and delineation of structural trends in bedrock. In addition, the imagery potentially provides a means of quantitative classification of seafloor lithology, allowing sedimentologists the ability to examine spatial distributions of seabed sediment type without resorting to subjective estimation or prohibitively expensive bottom-sampling programs. Using Simrad EM100 and EM1000 sonars as an example, this paper illustrates the nature and scale of possible artifacts, the necessary post-processing steps and shows specific applications of these sonars. 相似文献