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基于GPU和分块技术的巨幅影像快速傅里叶变换算法研究(英文) 总被引:1,自引:0,他引:1
快速傅里叶变换(FFT)是遥感影像处理的基础方法,随着高光谱、高空间和高时间分辨率遥感影像获取能力的提升,如何利用快速傅里叶变换技术快速有效地处理巨幅遥感影像是当前遥感影像处理技术中的重要环节和研究热点。傅里叶变换算法FFT是基本的图像处理算法之一,该算法可进行遥感影像的条带噪声去除、影像压缩和影像配准处理等多种用途。CUFFT函数库是NVIDIA公司提供的基于GPU的FFT算法库,FFTW是由MIT科学实验室计算机组在PC平台上开发的基于CPU的FFT算法,是目前在基于CPU的运行速度最快的FFT算法函数库,这两种实现共有的问题是当可用内存或显存的容量小于图像容量时,就会出现内存或显存溢出。针对这种问题,提出了一种基于GPU和分块技术的巨幅遥感影像快速傅里叶变换(huge remote fast Fourier transform,HRFFT)算法。通过对CUDA的CUFFT函数库中的FFT算法进行改进,解决了巨幅图像内存或显存溢出的问题,并结合HJ-1A卫星的CCD影像,通过实验与其他算法进行了对比,证明了该方法的合理性。在实际应用中,利用本文提出的HRFFT算法,改善了影像处理的效果,提高了遥感影像的质量,同时加快了影像处理的速度,节省了计算时间,取得了较好的效果。 相似文献
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根据菲涅耳衍射公式,导出了含介质的单透镜与双透镜系统输出面的光场复振幅分布,并与分数傅里叶变换定义式比较,得到了实现分数傅里叶变换的系统结构参量.运用矩阵光学方法,导出上述系统的ABCD矩阵,并与分数傅里叶变换矩阵比较,研究发现两种方法所得结果一致. 相似文献
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针对光学图像加密的轮廓显现问题,提出了一种基于稀疏相位和可调傅里叶变换的图像加密方法。将可调傅里叶变换引入光学图像加密程序中,运用二维可调傅里叶变换实现像素混淆处理,相比基于复数或实数的变换域方案,计算复杂度较低;从加密函数提取相位值并获得加密数据的相位函数,再提取相位加密函数的稀疏数据,从而避免将密文相位信息主要集中在纯相位掩码内,以解决轮廓显现问题;完成了单图像加密实验和双图像加密实验,结果表明实现了较好的安全性,解决了光学图像加密的轮廓显现问题。 相似文献
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We have examined the validity of the time-dependent variational approximation (TDVA) to the Gaussian wavepacket method (GWM) for quantum double-well (DW) systems, by using the quasi-exact spectral method (SM). Comparisons between results of wavefunctions, averages of position and momentum, the auto-correlation function, and an uncertainty product calculated by SM and TDVA have been made. It has been shown that a given initial Gaussian wavepacket in SM is quickly deformed at t>0 where a wavepacket cannot be expressed by a single Gaussian, and that assumptions on averages of higher-order fluctuations in TDVA are not justified. These results cast some doubt on an application of TDVA to DW systems. Gaussian wavepacket dynamics in anharmonic potential systems is studied also. 相似文献
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The quality of wavefunctions obtained by the Fourier grid Hamiltonian (FGH) method is analyzed. The criteria used for judging
the quality are the extent to which virial, hypervirial and Hellmann-Feynman theorems are satisfied by the numerically computed
FGH-wavefunction. The quality of the FGH-wavefunction is also examined from the point of view of local error in the wavefunction.
It is shown that high quality wavefunctions can be obtained from the FGH recipe if the grid length (L) and grid spacings are chosen after properly examining the range of the potential and its nature. 相似文献
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采用劈裂-伪谱方法求解激光场中的含时薛定谔方程,探讨飞秒激光脉冲中氢原子波包的演化过程.研究了氢原子激发态的径向分布,角向分布、各态布居和电子云密度随时间的变化关系.在用共振激光脉冲控制氢原子波包演化的过程中径向分布、角向分布、各态布居和电子云密度随时间发生变化,但发现径向分布和角向分布在变化的过程中始终经过一些特殊点,并从理论上分析了存在这些特殊点的原因. 相似文献
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Dirac‘s method which itself is for constrained Boson fields and particle systems is followed and developed to treat Dirac fields in light-front coordinates. 相似文献
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在波恩-奥本海默近似中,分子中原子核的运动通常采用绝热表象的基态势能面来描述,一般情况下这样是比较好的近似. 然而当势能面上存在锥形交叉时,即使体系的能量远远低于锥形交叉点,绝热基态势能面近似将不再有效. 锥形交叉的出现,使得绝热表象下描述核运动的哈密顿中出现了两个额外的附加项:对角波恩-奥本海默近似校正(DBOC)项和几何相位(GP)项. 尤其GP项,使得基态绝热势能面近似失效. 这两项在锥形交叉点处的数值是发散的,因此在绝热表象中来严格描述核运动,会使量子动力学的计算存在数值收敛的困难. 在量子分子动力学计算中,最常用的数值方法是分离变量表象方法(DVR). 本文通过在绝热表象和透热表象下求解涉及两个电子态且包含锥形交叉的二维的薛定谔方程来验证Sinc-DVR的数值收敛性. 计算结果显示,在绝热表象中采用通常格点密度分布的Sinc-DVR方法,即使在没有特别的处理DBOC和GP项时,也可以得到比较可靠的结果. 此时的数值不确定性并没有比引入任意的向量势来纠正GP效应的不确定性更差. 需要特别注意的是,纠正GP效应的任意向量势的精确形式,通常是不易得到其精确形式的. 相似文献
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Estimating leaf chlorophyll and nitrogen content of wetland emergent plants using hyperspectral data in the visible domain 总被引:2,自引:0,他引:2
Chaofan Guo 《光谱学快报》2013,46(3):180-187
Increasing amounts of recycled water have been used in wetlands; as such, monitoring the growth status of wetland plants with remote sensing technology is of great significance to restore and reconstruct wetland added by recycled water. In this paper, Phragmites australis and Typha angustifolia were selected. Spectral reflectance was determined in the visible domain to avoid the influence of leaf water on the established model; chlorophyll and nitrogen contents were measured as data sources. Statistical analysis, including correlation analysis and stepwise regression analysis, was conducted to estimate chlorophyll and nitrogen contents with different derivative transform spectra, namely, first derivative reflectance spectrum (FDS), band depth (BD), continuum-removed derivative reflectance (CRDR), band depth ratio (BDR), and normalized band depth index (NBDI). After the selected bands were statistically analyzed, we found that the range of 550–750 nm, particularly 700–750 nm (red edge range), was the key range to estimate biochemical parameters. Single removal cross-validation results showed that the optimum models of chlorophyll content inversion in reeds, cattails, and combined samples were BD, CRDR, and NBDI, respectively; the corresponding R2 were 0.87, 0.83, and 0.81. The respective RMSE values were 0.16, 0.15, and 0.33; the optimal models of nitrogen content inversion in reeds, cattails, and combined samples were BD, CRDR, and BD, respectively; the corresponding R2 were 0.69, 0.72, and 0.79. The respective RMSE values were 0.15, 0.11, and 0.17. Kruskal–Wallis non-parametric test and multi-way ANOVA were then performed; results revealed that data types and biological differences greatly influence the inversion model; by contrast, spectral derivative transform and vegetation type difference did not significantly affect the inversion model. Our results could be used as a scientific basis of the non-destructive growth status monitoring of wetland plants. It also provided a reference for restoration and management of wetlands supplied with recycled water. 相似文献
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Yoshifumi Ota Akiko Higurashi Tatsuya Yokota 《Journal of Quantitative Spectroscopy & Radiative Transfer》2010,111(6):878-894
A vector radiative transfer model has been developed for a coupled atmosphere-ocean system. The radiative transfer scheme is based on the discrete ordinate and matrix operator methods. The reflection/transmission matrices and source vectors are obtained for each atmospheric or oceanic layer through the discrete ordinate solution. The vertically inhomogeneous system is constructed using the matrix operator method, which combines the radiative interaction between the layers. This radiative transfer scheme is flexible for a vertically inhomogeneous system including the oceanic layers as well as the ocean surface. Compared with the benchmark results, the computational error attributable to the radiative transfer scheme has been less than 0.1% in the case of eight discrete ordinate directions. Furthermore, increasing the number of discrete ordinate directions has produced computations with higher accuracy. Based on our radiative transfer scheme, simulations of sun glint radiation have been presented for wavelengths of 670 nm and 1.6 μm. Results of simulations have shown reasonable characteristics of the sun glint radiation such as the strongly peaked, but slightly smoothed radiation by the rough ocean surface and depolarization through multiple scattering by the aerosol-loaded atmosphere. The radiative transfer scheme of this paper has been implemented to the numerical model named Pstar as one of the OpenCLASTR/STAR radiative transfer code systems, which are widely applied to many radiative transfer problems, including the polarization effect. 相似文献
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Jie Lian Qingpu Wang Aijian Wei Yurong Wang Ruifeng Zhang Xingkui Cheng 《Optics & Laser Technology》2005,37(5):622-419
Cerium-doped Sr0.60Ba0.40Nb2O6 (SBN:60) crystals were obtained by Czochralski method. Optical transmission spectra were measured and the absorption coefficients were calculated in the visible range. The results showed that Ce-doped crystals were transparent for wavelengths more than and the fundamental absorption edge shifted towards the longer wavelength direction with increasing Ce concentrations. In addition, the birefringence of crystals were investigated based on the theory of interference between extraordinarily and ordinarily polarized light, and the birefringence values were determined in the long wavelength region. As a result, the birefringence becomes larger by doping of SBN crystals with cerium. 相似文献
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Nazakat Ullah 《Pramana》1986,26(1):9-14
A determinantal identity is used to calculate the ensemble-averaged traces of the Hamiltonian. Using these averages a general
expression is obtained for the Fourier transform of the single eigenvalue probability density function for all the three Gaussian
ensembles for the two-dimensional case. It is shown how one can use the familiar step-up operators for the representation
of a determinant. The ensemble-averaged traces are also used to derive the Fourier transform of the non-zero mean ensemble. 相似文献