共查询到20条相似文献,搜索用时 531 毫秒
1.
2.
3.
《海洋测绘》2003,(6)
海洋测量机载激光测深中的深度归算技术欧阳永忠 ,黄谟涛 ,翟国君 ,等 (1— 1)多波束测深系统的归位问题研究赵建虎 ,刘经南 (1— 6 )海图深度基准面的算法研究暴景阳 ,黄辰虎 ,刘雁春 ,等 (1— 8)海洋测线网平差中拟稳测线系统误差的影响李明叁 ,刘雁春 ,黄谟涛 ,等 (1— 13)侧扫声纳和多波束测深系统在海洋调查中的综合应用罗深荣 (1— 2 2 )侧扫声纳数据库管理设计滕惠忠 ,邓雪清 ,郭思海 (1— 2 7)多波束测深系统的安装校准王闰成 (1— 34)双频测深仪在海底浅层物质分类中的应用郭发滨 ,刘忠臣 (1— 4 6 )黄河改道后河口至黄河海港海岸… 相似文献
4.
多波束测深系统的精度评估方法研究 总被引:2,自引:1,他引:2
在分析了多波束测深系统测量误差来源的基础上,讨论了多波柬测深系统静态精度、相对精度和绝对精度的系统精度评估方法。采用的静态精度评估方法就是在多波柬测深系统静止的条件下考核其对同一位置测量深度的误差;相对精度评估方法就是布设多条交叉重叠的测线,考核交叉重叠点的测深误差;绝对精度评估方法是在多波束测深的同时利用高精度的测深仪测量同一区域,用此参考地理模型来检验多波束测深的精度。根据误差理论,三种精度评估的方法分别从系统稳定性、自符合性和系统误差方面确定各误差源的综合误差,它们是检验多波束测深系统精度是否符合海道测量标准的有效方法。文中给出了系统试验数据的重要结果及设备验收的方法。 相似文献
5.
6.
以海口湾为研究区,利用Landsat资料进行可见光遥感测深方法研究。采用NDWI、MNDWI、EWI、NWI指数的阈值分割法进行水陆分离,结果表明NDWI指数更适合海口湾。选取与水深相关性比较好的反射率因子TM2、TM3、TM1/TM2、TM1/TM3,采用目前常见的可见光遥感测深方法,建立了线性、对数、幂指数、指数测深模型,与实测水深的比较结果表明TM1/TM3的指数测深模型在0-10 m水深的平均绝对误差为1.67 m,在实际应用中有参考价值。此外,建立了TM2、TM3、TM1/TM2、TM1/TM3的二次多项式测深模型以及对数二次多项式测深模型,建立了它们的二元和四元线性、对数测深模型,还建立了它们的分段函数测深模型,与实测水深的比较结果表明,二次多项式测深模型优于线性测深模型,对数二次多项式测深模型优于对数测深模型,分段函数测深模型优于非分段函数测深模型。 相似文献
7.
8.
9.
10.
根据多波束测深系统边缘波束采集的异常数据云图,判别分析多波束测深系统的各误差源对边缘波束测深的影响,从理论上探讨声线折射所引起的测深误差与边缘波束角之间的关系,通过多波束测深工程实例的精度验证,结果表明:换能器安装的牢固程度和校准精度、测船定位和姿态改正与测深的时间同步性,对边缘波束的测深精度影响较大;声线剖面误差使得中央波束和边缘波束的测深偏浅或偏深,各波束的测深误差曲线呈现"哭脸"状或"笑脸"状,但对于各波束测深的综合精度,中央波束精度相对较高,两侧边缘波束精度相对较低。 相似文献
11.
12.
在海洋磁力测量中,因受测量环境及各项改正的残余量等因素的系统性影响,不同测线间存在着不同程度的系统差,这种测线系统差会使测区磁场水平不统一,导致磁异常等值线图失真。为此,研究了基于虚拟检查线的海洋地磁测量数据调差方法,该方法尝试在不使用检查线数据情况下,沿垂直于测线方向选取一定数量的虚拟检查线,根据测线数据拟合出各条虚拟检查线上场的分布规律,并将测线方向拟合前后残差的平均值作为各条测线上的测线系统差,对各条测线数据进行改正。仿真计算与分析表明:对于磁异常变化较平缓的测区,该方法可以有效消除测线系统差;当磁异常变化剧烈时,该方法可以部分消除测线系统差。 相似文献
13.
14.
15.
Dhouha Ferjani Slim Gana 《Deep Sea Research Part I: Oceanographic Research Papers》2010,57(10):1177-1191
Seasonal hydrographic conductivity–temperature–depth surveys and moored current meter measurements have been analysed using an inverse approach in order to highlight the main features of the circulation in the western Sicily Strait during 2003. The variational inverse section model combines different types of constraints to seek for a continuous flow field satisfying data and physical assumptions within prescribed prior error bars. It is based on a finite element discretization that allows an appropriate resolution of very irregular topography. The corresponding results, consistent with data and dynamics, are providing new insight into the circulation of the surface and intermediate layers in conjunction with transport and formal error estimates during five hydrographic cruises. In the upper layer, these insights include the southward Atlantic Tunisian Current (ATC) off the Cap Bon Coasts, its high variability at short time-scales and its recirculation during October. For the Levantine Intermediate Water (LIW) regime, a detailed view of the circulation in the western Sicily Strait is given evidencing its recirculation at the western sill during the same period. Transports for both ATC and LIW are computed and found to be maximum in spring and decrease in summer and fall. 相似文献
16.
17.
18.
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
19.
Optimal interpolation method is applied to Geosat altimetry data both to remove orbit error and to separate temporal mean sea surface dynamic topography (SSDT) from temporal fluctuations around the mean. Loss of long-wavelength oceanic signals at orbit error reduction procedure is smaller in this method than that in conventional collinear methods, but the areal average height over the study domain is still removed as the orbit error. The fluctuation SSDT is quantitatively evaluated by sea level data from tide gauge stations at Japanese islands. The correlation coefficient of the two sea-level variations is 0.83 when the loss of the areal average is compensated by the seasonal variation of the areal average height determined from the climatological monthly-mean SSDT. In addition, the improvement of the geoid model by combined use of Seasat altimetry data and hydrographic data is validated through the estimated temporal mean SSDT. In a local area where hydrographic data contemporary with the Seasat mission exist, the geoid model has been significantly improved so that the absolute SSDT can be determined from combination of the altimetry data and geoid model; the absolute SSDT describes the onset event of a quasi-stationary large meander of the Kuroshio south of Japan very well. Outside this local area, however, errors of several tens of centimeters still remain in the improved geoid model. 相似文献
20.
《Deep Sea Research Part I: Oceanographic Research Papers》2001,48(6):1347-1373
The quantification of vertical motion and vertical fluxes is essential in our ability to predict and tolerate climate change. However, diagnostic estimations might be affected by the errors arising from the necessary compromise between spatio-temporal resolution and cost of hydrographic surveys. Observations of a numerical ocean model have been made in order to test the accuracy of different sampling strategies and their possible a-posteriori corrections. A simple first-order correction method, computing a pseudo-synoptic data set from a non-synoptic data set and involving a geostrophic relocation of the stations is shown to correct significantly the synopticity error in hydrographic data, derived QG vertical motion and vertical temperature fluxes. Sensitivity analyses also show that the lack of synopticity is more critical than other factors, including the sampling resolution, the level of no-motion and the analysis. 相似文献