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1.
提出了一种改进的Bancroft算法运用于组合双系统SPP解算。为检验新算法的解算精度,选取2013年2月采集于武汉大学实验大楼楼顶的GPS/BD双频双模接收机实测数据进行解算。实验结果表明改进的Bancroft算法与传统的最小二乘算法的解算精度相当,其解算效率与最小二乘算法相比提高了22%,从而验证了改进的Bancroft算法在组合双系统SPP解算中的可行性及优越性。  相似文献   

2.
首先分析了法方程稳定性对平差解算结果的影响。为减弱法方程对平差解算结果的影响,采用矩阵分解方法直接对系数矩阵进行矩阵分解,以求解最小二乘最小范数解替代原来最小二乘的法矩阵求逆运算,从而克服法方程求逆造成的解算稳定性差和病态性问题。实验分析结果表明基于矩阵分解的平差解算精度和可靠性较优。  相似文献   

3.
新型遥感卫星传感器几何模型-有理函数模型   总被引:9,自引:0,他引:9  
介绍了一种新型的遥感卫星传感器几何模型:有理函数模型。结合目前遥感卫星传感器几何模型的研究现状,讨论了有理函数模型的建立、最小二乘解算过程,并分析了其几何特性以及在遥感中的应用前景。  相似文献   

4.
王振杰  方稚 《海洋测绘》2014,34(6):29-31,35
为了满足在复杂观测条件下GPS基线解算的精度要求,研究了一种新的随机模型。与基于卫星高度角的随机模型难以定义出观测值之间的空间相关性不同,该随机模型核心是基于最小二乘估计得到的残差序列,通过移动窗口,利用前几个历元的残差序列,对当前历元观测值的方差-协方差阵进行实时估计。通过实例分析,将其与传统的随机模型的计算结果进行对比,验证了该实时随机模型在改善基线解算精度方面的有效性。  相似文献   

5.
介绍了在航模糊度求解的模型。在航模型每个历元均需要多估计一组坐标矢量,因而降低模糊度求解的精度。用取整法、引导取整法和整数最小二乘法三种模糊度固定方法,比较了在静态模型和在航模型下整周模糊度求解的成功率和需要的初始化时间,为动态平台的糊度解算提供参考。  相似文献   

6.
基于最小二乘水位拟合模型参数的时变性及其规律,分析指出模型参数求解的最佳同步时长与潮汐类型相关,按半日潮、混合潮、全日潮类型应分别取略大于6h、10h、12h。分析了参数在一定精度下能延续使用的时长,即参数的时效性问题,统计分析表明:在保证精度的前提下,模型参数可延续使用同步时长的约一半,可显著提高运行效率。  相似文献   

7.
分别采用切比雪夫曲线和最小二乘曲线拟合HY-2(海洋二号)卫星精密轨道,并进一步解算速度场与预报轨道。结果表明:最小二乘曲线拟合结果明显优于切比雪夫曲线拟合结果,拟合轨道精度为1~2cm,拟合速度场精度为1~2cm/s,且可以进行轨道短期预报,预报轨道精度与拟合轨道精度相当。  相似文献   

8.
文章给出了定位数学模型和递推最小二乘算法,并且讨论了数据后置处理的过程和最小二乘法在数据后置处理中的应用,最后详细介绍了水池试验数据的处理结果。实验结果表明,利用递推最小二乘法能够有效地对定位结果进行平滑处理。  相似文献   

9.
工程设计Weibull分布参数拟合的改进方法   总被引:2,自引:0,他引:2  
图解法是求解Weibul分布中3个可调参数的传统方法。但参数的推求过程要图解试求,反复调整,最后结果往往不是最佳拟合参数;线性最小二乘法是最近几年提出的一种求解Weibul分布参数的方法,但其精度受位置参数初始迭代值的影响很大。文中运用麦奎尔特法推求Weibul分布的参数,实现了参数推求的一举寻优。算例表明,拟合方法可行实用,拟合精度明显提高。  相似文献   

10.
侧扫声纳系统姿态参数平滑方法研究   总被引:1,自引:0,他引:1  
针对侧扫声纳系统姿态参数采样率低于声纳Ping值采样率的问题,采用窗口移动多项式最小二乘平滑方法(Savitzky—Golay平滑法),对阶梯状姿态数据进行平滑。结果证明了该法的可行性。在选取窗口宽度和多项式阶数时,通过实测数据比较表明,采用窗口为11的二阶多项式平滑后结果与原数据符合程度高。  相似文献   

11.
将抗差估计的思想融入到粗差探测的算法中,设计出对模型误差特别是粗差具有抵抗能力的粗差探测算法。应用最小二乘法来计算观测值的参数、残差、协因数阵及单位权的初值,再根据残差和有关的参数,按所选择的权函数,计算每个观测值的权,经过迭代计算求得观测值的残差,按照统计检验的方法剔除粗差。通过实验证明,基于验后方差估计原理导出的选权迭代具有很强的粗差探测能力。  相似文献   

12.
A new standardization method for glass electrodes is proposed for pH measurements on the NBS scale. An expression is obtained to evaluate the apparent activity coefficient of hydrogen ions as a function of salinity and temperature, from determinations obtained by Mehrbach et al., 1973 (Limnol. Oceanogr., 18: 897–907). This expression must be used to estimate systematic errors produced by variations of residual liquid-junction potential by estimating the apparent activity coefficient of hydrogen ions. In this way, values of pH obtained in oceanographical cruises can be standardized in order to determine and compare different parameters of the CO2 system.Some experiments to study the variation of pH with temperature are carried out to compare the different series of acid constants used at present. A simple and precise polynomial equation is also obtained to determine the variation of pH with temperature.  相似文献   

13.
Nearshore wave and flow model results are shown to exhibit a strong sensitivity to the resolution of the input bathymetry. In this analysis, bathymetric resolution was varied by applying smoothing filters to high-resolution survey data to produce a number of bathymetric grid surfaces. We demonstrate that the sensitivity of model-predicted wave height and flow to variations in bathymetric resolution had different characteristics. Wave height predictions were most sensitive to resolution of cross-shore variability associated with the structure of nearshore sandbars. Flow predictions were most sensitive to the resolution of intermediate scale alongshore variability associated with the prominent sandbar rhythmicity. Flow sensitivity increased in cases where a sandbar was closer to shore and shallower. Perhaps the most surprising implication of these results is that the interpolation and smoothing of bathymetric data could be optimized differently for the wave and flow models. We show that errors between observed and modeled flow and wave heights are well predicted by comparing model simulation results using progressively filtered bathymetry to results from the highest resolution simulation. The damage done by over smoothing or inadequate sampling can therefore be estimated using model simulations. We conclude that the ability to quantify prediction errors will be useful for supporting future data assimilation efforts that require this information.  相似文献   

14.
多波束声呐图像是进行海底底质分类的主要数据源之一,由于受海洋噪声、声波散射和混响、仪器设备等因素影响,其经各项常规改正后仍存在明显残差,突出表现在中央波束区和条带重叠区,难以形成高质量的声呐图像。文中分析了多波束声呐图像残差的成因及影响,提出了一种基于多条带最小二乘拟合的多波束声呐图像残差处理方法。首先,得到相邻声脉冲(ping)信号中央区域、重叠区域以及整体趋势的拟合函数;然后,通过拟合函数计算得到中央和重叠区域的残差改正系数;最后,通过改正系数进行残差改正。实验分析表明,该方法在保留原始细节的基础上,有效削弱了残差对声呐图像的影响,对多波束声呐图像处理具有参考和应用价值。  相似文献   

15.
长江口浑浊带核心区北槽水动力特征研究   总被引:4,自引:2,他引:2  
蒋杰  何青  朱磊  林建良 《海洋学报》2019,41(1):11-20
本文根据2015年长江口洪季浑浊带水域座底三脚架全水深范围观测数据,对北槽中下段纵横向流、余流结构、边界层特征等进行了深入研究,结果显示:(1)大潮潮流矢量特征在垂向上的变化差异最为显著;北槽中下段水流出现明显的横向输移,指向航槽北面;(2)横向流速在大潮期间的变化(垂线平均)为-0.10~0.39 m/s,小潮期间的变化为-0.13~0.25 m/s;横向平流对于北槽纵向物质输运有显著调整作用;(3)余流垂向差异大,底部几乎为0,小潮期间余流更强;周期性再悬浮的细颗粒泥沙可作为北槽最大浑浊带的重要物质来源;(4)传统六点对数流速拟合法获得摩阻流速误差较大,近底1 m区域高分辨流速剖面是准确获取底边界层参数的有效途径。  相似文献   

16.
Multibeam bathymetric system (MBS) has been widely applied in the marine surveying for providing high-resolution seabed topography. However, some factors degrade the precision of bathymetry, including the sound velocity, the vessel attitude, the misalignment angle of the transducer and so on. Although these factors have been corrected strictly in bathymetric data processing, the final bathymetric result is still affected by their residual errors. In deep water, the result usually cannot meet the requirements of high-precision seabed topography. The combined effect of these residual errors is systematic, and it’s difficult to separate and weaken the effect using traditional single-error correction methods. Therefore, the paper puts forward a new method for weakening the effect of residual errors based on the frequency-spectrum characteristics of seabed topography and multibeam bathymetric data. Four steps, namely the separation of the low-frequency and the high-frequency part of bathymetric data, the reconstruction of the trend of actual seabed topography, the merging of the actual trend and the extracted microtopography, and the accuracy evaluation, are involved in the method. Experiment results prove that the proposed method could weaken the combined effect of residual errors on multibeam bathymetric data and efficiently improve the accuracy of the final post-processing results. We suggest that the method should be widely applied to MBS data processing in deep water.  相似文献   

17.
对顾及系统误差的地球静止轨道(GEO)卫星几何法定轨做了初步探讨,给出顾及系统误差的GEO卫星几何法定轨数学模型,推导了参数解算公式,提出PDOP值加权的几何法定轨方法,并讨论了权函数的选取。最后以卫星钟差为例进行模拟计算。结果表明:顾及系统误差的GEO卫星几何法定轨,可大大减弱系统误差对定轨结果的影响;基于PDOP值加权的几何法定轨,可进一步提高系统参数解算精度和定轨精度。  相似文献   

18.
研究带乘性噪声广义系统的观测噪声最优估计问题。在假设系统正则的情况下,针对乘性噪声为一般随机矩阵即各观测通道乘性噪声同时刻相关的情况,通过受限等价变换和状态扩维的方法,给出了线性最小方差意义下的观测噪声最优滤波算法和最优平滑估计算法。数字仿真结果表明了算法的有效性。  相似文献   

19.
A model-based approach is proposed to solve the oceanic internal wave signal processing problem that is based on state-space representations of the normal-mode vertical velocity and plane wave horizontal velocity propagation models. It is shown that these representations can be utilized to spatially propagate the modal (depth) vertical velocity functions given the basic parameters (wave numbers, Brunt-Vaisala frequency profile, etc.) developed from the solution of the associated boundary value problem as well as the horizontal velocity components. These models are then generalized to the stochastic case where an approximate Gauss-Markov theory applies. The resulting Gauss-Markov representation, in principle, allows the inclusion of stochastic phenomena such as noise and modeling errors in a consistent manner. Based on this framework, investigations are made of model-based solutions to the signal enhancement problem for internal waves. In particular, a processor is designed that allows in situ recursive estimation of the required velocity functions. Finally, it is shown that the associated residual or so-called innovation sequence that ensues from the recursive nature of this formulation can be employed to monitor the model's fit to the data  相似文献   

20.
The feasibility of adding an interferometric swath bathymetric system to GLORIA, a 6.6 kHz long-range sidescan sonar, is discussed. The size of GLORIA's low-frequency transducer arrays and towfish precludes significant modifications, but even without such changes bathymetric errors could be several tens of metres over a usable swath somewhat smaller than the normal GLORIA swath. A swath bathymetry based on GLORIA will have random errors depending strongly on wind speed, water depth, and swath width. Within the range of these parameters, root-mean-square bathymetry errors in the range of 1-100 m can be expected  相似文献   

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