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121.
基于反馈环的多次波压制方法研究   总被引:1,自引:0,他引:1       下载免费PDF全文
基于波动方程理论压制多次波,综合考虑了多次波传播的运动学特性和动力学特性,避免了非波动法解决问题所带来的局限性,已成为多次波去噪的发展趋势.首先对多次波压制国内外研究现状做了简单的阐述.在此基础上,给出了反馈环波动方程预测减去法的方法原理.介绍了抛物线拉东(Radon)变换外推近道数据、谱模拟法提取震源子波、均衡伪多道匹配和多次波减去法效果评价等四大关键技术的思路及主要计算公式.用JAVA语言自行开发了相应的模块,并应用射线法多次波模型和SEG/EAGEPluto模型,对以上方法技术进行了检验,去噪效果良好.对海上某多次波特发育实际资料进行了处理,取得了满意的效果.  相似文献   
122.
Extrapolating wavefields and imaging at each depth during three‐dimensional recursive wave‐equation migration is a time‐consuming endeavor. For efficiency, most commercial techniques extrapolate wavefields through thick slabs followed by wavefield interpolation within each thick slab. In this article, we develop this strategy by associating more efficient interpolators with a Fourier‐transform‐related wavefield extrapolation method. First, we formulate a three‐dimensional first‐order separation‐of‐variables screen propagator for large‐step wavefield extrapolation, which allows for wide‐angle propagations in highly contrasting media. This propagator significantly improves the performance of the split‐step Fourier method in dealing with significant lateral heterogeneities at the cost of only one more fast Fourier transform in each thick slab. We then extend the two‐dimensional Kirchhoff and Born–Kirchhoff local wavefield interpolators to three‐dimensional cases for each slab. The three‐dimensional Kirchhoff interpolator is based on the traditional Kirchhoff formula and applies to moderate lateral velocity variations, whereas the three‐dimensional Born–Kirchhoff interpolator is derived from the Lippmann–Schwinger integral equation under the Born approximation and is adapted to highly laterally varying media. Numerical examples on the three‐dimensional salt model of the Society of Exploration Geophysicists/European Association of Geoscientists demonstrate that three‐dimensional first‐order separation‐of‐variables screen propagator Born–Kirchhoff depth migration using thick‐slab wavefield extrapolation plus thin‐slab interpolation tolerates a considerable depth‐step size of up to 72 ms, eventually resulting in an efficiency improvement of nearly 80% without obvious loss of imaging accuracy. Although the proposed three‐dimensional interpolators are presented with one‐way Fourier extrapolation methods, they can be extended for applications to general migration methods.  相似文献   
123.
基于最大互相关的对流云预测   总被引:2,自引:0,他引:2  
黄勇  孔庆欣  郑兰芝 《气象科学》2005,25(4):399-404
传统上利用卫星云图做降水都是根据已知的卫星云图中的通道信息来进行降水量的估算。因此,利用卫星云图仅仅做到了降水量的估算。本文利用图像的最大互相关以及线性外推对未来的卫星云图进行预测,并取得较好的结果,从而能够利用云图进行降水量的预报。  相似文献   
124.
Measurements of photosynthetically active radiation(PAR),which are indispensable for simulating plant growth and productivity,are generally very scarce.This study aimed to compare two extrapolation and one interpolation methods for estimating daily PAR reaching the earth surface within the Poyang Lake national nature reserve,China.The daily global solar radiation records at Nanchang meteorological station and daily sunshine duration measurements at nine meteorological stations around Poyang Lake were obtain...  相似文献   
125.
合成孔径雷达空间变迹带宽外推超分辨算法   总被引:1,自引:0,他引:1  
张平  杨汝良 《测绘学报》2010,39(1):71-75
提出一种变迹法带宽外推合成孔径雷达(SAR)超分辨率成像算法,可以提高合成孔径雷达成像分辨率并抑制旁瓣。利用空间变迹法(SVA)处理后的带宽扩展效应,对频谱进行幅度均衡使有效带宽扩展,并利用非整数倍Nyquist采样率空间变迹法对外推后的旁瓣抑制,得到输出的高分辨率图像。仿真实验和定量分析验证了本文方法的有效性。  相似文献   
126.
Designed for grid point systems, the traditional semi-Lagrangian semi-implicit scheme is not mass-conserving and can lead to significant solution errors. In the present study, a finite-volume semi-Lagrangian semi-implicit scheme (hereafter “FVSLSI”) is designed for the Yin-Yang mesh and tested in a barotropic shallow water model in the spherical coordinate system. Three test cases, i.e. the advection of a solid body, a steady state nonlinear zonal geostrophic flow and the deformation flow, are simulated to compare the performance of the FVSLSI with that of the traditional semi-Lagrangian scheme (hereafter “SL”) from perspectives of shape preservation, mass conservation, normalized bias, and convergence rate. Results indicate that the FVSLSI performs better than the SL in mass conservation and shape preservation. The bias by the FVSLSI is smaller than that by the SL, while the rate of convergence by the FVSLSI is larger than that by the SL. The FVSLSI also allows large time step. Therefore, the FVSLSI is suggested to be distributed to communities that are developing atmospheric/oceanic models.  相似文献   
127.
这里研究了VTI(Vertical Transverse Isotropy)介质隐式有限差分(IFD)波场外推算子和VTI介质平面波偏移。在文中设计了VTI介质IFD波场外推算子,将Taylor分析法求得的差分系数,作为初始解,用非线性优化方法迭代求得算子系数。将设计的外推算子频散曲线和偏移脉冲响应与理论解进行了对比分析,验证出外推算子有较高的精度。从各向同性介质平面波偏移理论出发,结合VTI介质IFD波场外推算子,将平面波偏移推广到VTI介质中。对Hess VTI标准模型拟合数据进行偏移,偏移结果验证了平面波偏移在VTI介质中的有效性,以及在加强特定陡倾界面成像方面的优势。并且,与常规VTI介质叠前深度偏移相比,VTI介质平面波偏移在保证成像质量的前提下,大大减少了计算量,为各向异性偏移成像研究提供了新的技术思路。  相似文献   
128.
The purpose of this paper is to study the possibility of performing practically stable and efficient frequency‐space (f?x) wavefield extrapolation for the application of seismic imaging and datuming via infinite impulse response (IIR) filters. The model reduction control theory was adopted to design such IIR f?x extrapolation filters. The model reduction theory reduces the order of a given order system which, in this case, involves reducing a finite impulse response (FIR) f?x extrapolation filter system into an IIR f?x extrapolation filter system. This theory relies on decomposing the states of the given filter system into strong and weakly coupled sub‐systems, and then eliminating the weakly coupled states via singular value decomposition of the Hankel and the impulse response Gramian matrices. Simulation results indicate that IIR f?x filters can be obtained, which are stable from an IIR filter design point of view. Simulations also indicate that stable seismic impulse responses and synthetics can be obtained with a reduced system model order and, hence, less computational efforts with respect to the number of complex multiplications and additions per output sample. It is hoped that this study will open new possibilities for researchers to reconsider designing IIR f?x explicit depth extrapolation filters due to their expected computational savings and wavenumber response accuracy, when compared to the FIR f?x explicit depth extrapolation filters.  相似文献   
129.
A unified method of approximation, extrapolation, and objective layering is offered for processing vertical oceanographic profiles. The method is demonstrated using seawater density and consists of adjustable splitting of each individual profile into N vertical layers based on tentative, piecewise linear homogeneous approximation with specified accuracy and a final fitting of an N-layered analytical model to data. A set of 3N coefficients of the model includes one density value at the sea surface; N−1 depths of layer interfaces; and N pairs of coefficients that describe a profile shape within the n-th layer—an asymptotic density value (a key parameter for extrapolation) and a vertical scale of maximum density variability (related to vertical gradient). Several distinctive characteristics of the technique are: (1) It can be used for the analysis of the vertical structure of individual profiles when N is an unknown parameter, and spatial interpolation when N should be equal for all profiles. (2) A justified downward extrapolation of incomplete data is possible with the model, especially if historical deepwater profiles are available. (3) Layer interfaces, as well as other coefficients, are derived with only one fitting to the entire profile. (4) The technique, using its general formulation, can serve as a parent for developing various types of models. The simpler step-like (with hyperbolic or exponential approximation) and more complicated smooth (continuous in gradient space) models were designed and tested against a large number of density profiles from the Sea of Okhotsk and the Gulf of California. Comparison of parametric, z-levels and isopycnal averaging was done for the region off the northeastern coast of Sakhalin.  相似文献   
130.
薛峰  王兴  吴双  苗春生  张琳焓 《气象科技》2017,45(6):1036-1042
提出一种基于动态权重的降水概率融合预报方法。首先建立一个适用于权重分配的评分模型,对基于雷达光流外推的降水概率预报和基于数值模式经反射率换算后的降水概率预报的预报准确率分别加以评估;提出一种改进的Brier评分法,该方法兼顾了降水落区的大小和降水量,降低评分对样本数据数量多少的敏感性;根据两种在不同预报时效的评分,动态地分配两种预报方法在不同预报时效的权重。试验部分通过Brier等评分验证表明,融合后各个预报时效的预报都表现出与雷达外推或数值模式相近甚至更高的技术评分。  相似文献   
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