理论模型反演计算表明，该方法实际可行。
The inversion result of theoretical model shows that this inversion method is practically reliable.
因此选择该模型反演全球的月平均风速，并将反演结果与NOAA产品风速比较。
Therefore, this model is chosen to retrieve the global monthly-average wind speed, and the retrieval results are compared with the NOAA products.
在软件中提供了多种反演方法如基于模型反演，稀疏脉冲反演和人工智能神经网络反演。
Multi inversion methods are provided in the software, such as inversion based on models, sparse pulses inversion and artificial intelligence neural network inversion.
利用速度模型反演技术，准确地描述了表层速度和厚度的纵横向变化细节，弥补了微测井单点调查的不足。
Inversion of surface model can depict the details of surface velocity and thickness, and makes up the shortcomings of uphole data.
现有基于声波时差的孔隙度及岩石强度计算模型反演出的地层孔隙度及岩石强度信息与实际地层偏差较大。
Porosity and rock strength of formation had got by utilizing mathematics model of porosity and rock strength which base on acoustic time have big derivation with actual situation.
目前常规的叠后地震反演主要包括道积分，递推反演，基于模型反演，但这些反演都是反演波阻抗具有局限性。
At present regular post-stack seismic inversion include recursive inversion, model inversion seismic which are impedance inversion and have their limitations.
实验结果表明，我们通过听觉模型反演从信号的自相关图谱中恢复出的语音信号，具有较好的自然度和良好的噪声鲁棒性。
The result of experiments show that resynthesized speech signals form the its correlogram by auditory model inversion is nature and robust in noisy environment.
反演使用的模拟数据是用IEM模型得到的，并用来训练神经网络。
Simulated data sets based on the Integration Equation Model (IEM) are used to train the neural network.
理论模型和实际资料的反演结果表明，本方法是求解地球物理反问题的一种有效手段。
Theoretical model and real data inversion results show that the method is an effective means to solve geophysical inverse problem.
映射反演模型方法是分析复杂问题的经典方法。
The method of mapping inversion model is a classical method of analyzing complicate problems.
实际地震资料的波阻抗反演结果，说明了这种反演方法不依赖于初始模型，并且具有极高的分辨能力。
The results of real seismic data have shown that this inverse method does not depend on the initial model and has high resolution.
理论模型和实际资料的反演结果表明，此方法是稳健的，反演结果是可靠的，具有良好的应用前景。
Theoretical model and real data inversion shows that the method is robust with which we can obtain reliable results.
盐度的被动微波辐射遥感虽然在L波段灵敏度最高，但是其在L波段的灵敏度低于其它许多变量，因此对盐度反演模型精度要求很高。
Even though the window at L-band is the best choice for salinity remote sensing, the sensitivity of brightness temperature to SSS is lower than that of the other variables.
计算中采用考虑围岩松动圈的双介质模型，反演松动圈的弹性模量。
Taking into account rock loosing zone, the two-medium model is adopted in the computation.
因此建立合适的目标函数和反演模型是非常重要的。
So it is very important to establish an appropriate objective function and the inversion model.
提出了一种基于岩石物理模型与混合优化算法同时反演孔隙度和饱和度的新方法。
A new method for simultaneous inversion of porosity and saturation based on rock-physics model and hybrid optimization method was presented.
分析了在理论模型、反演技术、综合解释上的成果与问题；指出了固体地球物理的复杂性。
The paper analyzes the results and problems in theoretical model, inverse technology and comprehensive interpretation, and points out the complexity of solid geophysics.
传统的实测曲线拟合法对土模型参数的反演采用人工试凑的方法，效率低，且需要有一定工程经验的专业人员来操作。
Traditional signal matching analysis adjusting parameters of soil model uses manual way which has a fault of low efficiency and need the professional who processes engineering experience.
经过模型检验、参数反演，确定了水力参数和入渗补给系数。
The hydraulic parameters and infiltration supplement coefficient are ascertained by model testing and parameter inversion.
在这些地表通量定量遥感模型中，以遥感信息反演地表参数是其主要的内涵。
Surface parameters is retrieved from Remote Sensing, which is the main connotation of the surface flux retrieved from quantitative Remote Sensing model.
通过常密度模型、变密度模型及地震反演得到的莫霍面的比较，证实变密度模型更适合于莫霍面结构的反演。
The variable density model is more suitable for inversion of Moho depths structures than constant density model by comparison of Moho depth from seismic inversion.
与统计模型相比，反演的精度有明显提高。
In contrast to statistical model, the accuracy of the inversion is greatly improved.
基于生物光学模型的水质参数反演分析方法是水质遥感监测算法的发展趋势。
Analytical algorithm, which is based on bio-optical model, represents the trends of algorithms in retrieving water quality parameters from remote sensing data.
并从椭球模型的衍射图像反演得到微粒的形体因子。
Finally, the body factors of the particles are achined from the inversion to the diffraction pattern of ellipsoid model.
利用全球和近海海潮模型以及岛屿验潮站数据较系统地研究了海潮负荷特征，反演了全球海潮模型的适定性。
The ocean loading characteristics are studied systematically by using global and local ocean models as well as tidal gauge data, the suitability of global ocean models is also studied.
利用全球和近海海潮模型以及岛屿验潮站数据较系统地研究了海潮负荷特征，反演了全球海潮模型的适定性。
The ocean loading characteristics are studied systematically by using global and local ocean models as well as tidal gauge data, the suitability of global ocean models is also studied.
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