共查询到18条相似文献,搜索用时 859 毫秒
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在水声正交频分复用(OFDM)通信系统中,水声信道中的多径时延扩展会带来频域选择性衰落,多普勒效应会带来子载波间干扰(ICI)。传统接收算法需要开展复杂的二维(时延/多普勒)信道估计,再进行复杂的信道均衡和符号检测。针对有限多普勒扩展的信道条件下多普勒矩阵元素变化缓慢、ICI干扰范围有限的特点,借鉴多项式拟合思想,提出了一种创新的接收算法。该算法将多普勒矩阵元素近似为多项式函数,迭代进行多项式拟合和数据符号频域均衡。和传统方法相比,该算法无需进行信道多普勒估计,仅需信道的一维(时延)估计即可实现较好的性能。利用Bellhop产生的水声信道仿真结果验证了该算法的可行性。 相似文献
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振幅随偏移距变化(AVO)的分析对时左校正非常敏感。用时间穿估计AV涌减少时差校正的误差,在每个时窗内,在每个时窗内,使用块NMO能避免NMO拉伸,剩余NMO校正通过迭代互相关技术实现,时关 正后,时窗内的数据用偏移距坐标为变量表示的多项式乘常数脉冲来模拟。从而避免了数据从偏移琶角度呈慢度域的转换。用最小平方法求解地震脉冲和多项式系数。这种可分离最小平方问题的多项式系数和脉冲能力分别估计。简化的非 相似文献
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高抒 《中国海洋大学学报(自然科学版)》1997,(3)
地学研究经常涉及两变量间的线性回归分析。此类线性关系可有三种情形:(1)x数据的观测误差很小,数据点的离散只与y数据有关;(2)x和y数据都有观测误差,且数据点的离散仅由观测误差所引起;(3)数据点的离散不仅与观测误差有关,而且还受到其它因素的影响(但两变量仍存在显著的线性关系)。其中第三种情形在地学中最为常见,但已有的回归分析方法只是针对前两种情形。本文对LNS方法进行了改进,使之适用于第三型的回归分析。改进的方法在逻辑上具有一致性,在应用上适合线性关系第三型线性关系的特点,因而优于传统的OLS方法 相似文献
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《中国海洋大学学报(自然科学版)》1996,(4)
1996年《青岛海洋大学学报》总目次(括号内数字依次为卷数、期数、页数)分析海浪方向谱的EEV方法的一种迭代形式管长龙(26,1,1)……………………………………………分潮波模型多资料数值计算方法研究Ⅰ.岸边资料运动学外推的第一边值方法潘文波等(26... 相似文献
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海浪方向谱的现场观测与分析 总被引:3,自引:0,他引:3
方向谱是海浪的基本性质之一。本文在国内首次采用测波仪阵列法在渤海采油平台上成功地观测到海浪方向谱,给出了当地随波浪成长而变化的方向谱表达式。观测前采用数模和模型试验方法,对阵列的布置型式、测波仪间距和平台等对观测结果的影响,以及现有各种方向谱分析方法的精度等进行了对比分析,为提高观测精度,保证方向谱分析的质量提供了依据。 相似文献
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Okey Nwogu 《Applied Ocean Research》1989,11(4):176-182
A procedure for estimating directional wave spectra from an array of wave probes based on the Maximum Entropy Method (MEM) is developed in the present paper. The MEM approach yields an angular spreading function at each frequency band consistent with the input cross-spectral density matrix. The method is evaluated using numerical simulations of directional sea states. The MEM is also used to analyze data obtained from the three-dimensional wave basin of the Hydraulics Laboratory, National Research Council of Canada. Finally, the MEM is compared with the Maximum Likelihood Method (MLM) and is shown to be a powerful tool for directional wave analysis. 相似文献
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Liu Shuxue Yu Yuxiu
Assistant Researcher State Key Laboratory of Coastal Offshore Engineering Dalian University of Technology 《中国海洋工程》1995,(1)
The directional spectrum is one of the basic characteristics of sea waves. The observations of directional spectrum of sea waves were successfully conducted at platform Bohai 8 during 1991 and 1992 using a wave gage array for the first time in China. Based on the field data, the directional spectrum which depends on the wave growth is given in this paper. Before observations, the effects of the type of gage array, the distance between the gages and the platform itself on the measured results and the precision of some methods for estimating the directional spectrum were investigated and compared with the methods of numerical simulations and model tests of multi-direcitonal irregular waves. This ensures the quality of the observations and estimations of the directional spectrum. 相似文献
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In the nearshore,the wave field contains reflected and incident waves in which there iscorrelation between their phases due to the effect of reflection by some obstacles.Based on the extendedeigenvector method(EEV)derived by Guan et al.,a modified method(MEEV)is proposed as a generaland practical approach to estimating directional spectra for the co-existent field of incident and reflectedwaves and a formula is given for direct calculation of the reflection coefficient.The results of numericalsimulations show that MEEV is superior to EEV in resolution power,and the computed reflectioncoefficient agrees well with the real value within a certain range of incident angle. 相似文献
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This is a Part II of a paper of nonlinearities of wind waves in the deep open ocean. As shown in Part I, bound waves in deep sea are detectable by extracting secondorder Doppler spectra from the Doppler spectra of HF (high-frequency) radio waves scattered from the sea surface. There is a remarkable agreement between the calculated and measured Doppler spectra, considering the noise levels in measured Doppler spectra and the uncertainties in directional properties. The theoretical expression for bound waves is thus verified. Furthermore, the upper limit in calculating the Doppler spectra for the second-order approximation is presented from field observations, although we cannot conclude that it is equivalent to the limitation of the second-order bound wave theory. It is shown that analysis of radio wave scattering by the sea surface is one useful means of understanding the nonlinear properties of ocean waves. 相似文献
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海浪双峰方向分布的一种物理解释 总被引:3,自引:0,他引:3
用 18个波高计组成的直径为 40cm的圆形阵列在大型风浪槽内系统地测量了风浪和涌浪方向谱。用两种分辨力较高的方向谱估计方法最大似然法(MLM)和贝叶斯方法(BDM)分析的结果表明:风浪高频域出现的依赖于估计方法的双峰方向分布是一种物理假象;在较成长的涌浪低频域,得到跟传播方向对称、两峰间隔大约60°-90°非常规则的双峰方向分布,它跟频率和涌浪的成长状态有关,而跟估计方法无关,这种现象可以用非线性波-波相互作用过弱,在不同方向之间不能有效传递能量来解释。 相似文献
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不规则波作用下的船舶撞击作用 总被引:2,自引:1,他引:2
随着波谱理论研究的发展,各种海工结构及船舶的荷载及其内力分析也日趋应用不规则波的计算方法。目前对于外海码头在波浪作用下的船舶撞击荷载还应用规则波的研究方法,对其应用不规则波分析方法的途径以及在考虑波谱作用后会有怎样的结果等问题目前还较少研究。本文试图对此问题进行初步的分析。 相似文献
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The observation and estimation of directional spectra of sea waves is one of the essential subjects of study of oceanic dynamics. On the basis of the irregular linear wave theory, estimation methods for i/UV, PUV and VV directional wave spectra are derived. By using ij and PUV data measured in-situ, directional wave spectra are estimated, meanwhile the virtues and defects of various spectra are comparied. This method provide a basis for the observations of sea waves. 相似文献