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基于MTF的潜航体尾迹SAR成像仿真 被引量:5
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作者 周强 杨俭 +1 位作者 曲长文 骆卉子 《海军航空工程学院学报》 2013年第3期231-236,共6页
基于水动力学理论和波流弱相互作用理论,运用波作用量谱平衡方程研究了潜航体的尾流场与表面波作用后的表面尾迹,探讨了采用传递变换函数实现表面尾迹SAR成像的可行性。研究表明,波作用量谱平衡方程能够较准确地计算出潜航体尾流场与表... 基于水动力学理论和波流弱相互作用理论,运用波作用量谱平衡方程研究了潜航体的尾流场与表面波作用后的表面尾迹,探讨了采用传递变换函数实现表面尾迹SAR成像的可行性。研究表明,波作用量谱平衡方程能够较准确地计算出潜航体尾流场与表面波之间的非线性相互作用;传递变换函数能够快速有效实现海面后向散射系数到SAR图像的转换,且保证了较高的精度。 展开更多
关键词 潜航体 波流相互作用 多尺度散射模型 传递变换函数 尾迹仿真
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Experimental study on the multiscale scattering of high-velocity heterogeneous bodies
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作者 Qin Zhen-Chao Wei Jian-Xin +1 位作者 Di Bang-Rang Wang Di 《Applied Geophysics》 SCIE CSCD 2022年第1期1-10,143,共11页
There are complex heterogeneous entities in the underground medium,and the heterogeneous scale has a substantial impact on wave propagation.In this study,we used a set of 11 samples of glass beads as high-velocity het... There are complex heterogeneous entities in the underground medium,and the heterogeneous scale has a substantial impact on wave propagation.In this study,we used a set of 11 samples of glass beads as high-velocity heterogeneous bodies to evaluate the impact of such heterogeneous bodies on the propagation of P-wave.We vary the heterogeneous scale by changing the diameter of the glass beads from 0.18 to 11 mm while keeping the same volume proportion(10%)of the beads for the set of 11 samples.The pulse transmission method was used to record measurements at the ultrasonic frequencies of 0.34,0.61,and 0.84 MHz in the homogeneous matrix.The relationship between P-wave fi eld features and heterogeneity scale,P-wave velocity,and the multiple of the wave number and heterogeneous scale(ka)was observed in the laboratory,which has sparked widespread interest and research.Heterogeneous scale affects P-wave propagation,and its wave field changes are complex.The waveform,amplitude,and velocity of the recorded P-waves correlate with the heterogeneous scale.For the forward scattering while large-scale heterogeneities,noticeable direct and diff racted waves are observed in the laboratory,which indicates that the infl uence of direct and diff racted waves cannot be ignored for large-scale heterogeneities.The relationship between velocity and ka shows frequency dependence;the reason is that the magnitude of change in velocity caused by wave number is diff erent from that caused by heterogeneous scale.According to the change in the recorded waveform,amplitude variation,or the relationship between the velocity measured at diff erent frequencies and the heterogeneous scale,the identifi ed turning points of the ray approximation are all around ka=10.When ka is less than 1,the velocity changes slowly and gradually approaches the eff ective medium velocity.The ray velocity measured for heterogeneous media with large velocity perturbations in the laboratory is signifi cantly smaller than the velocity predicted by the perturbation theory. 展开更多
关键词 heterogeneous bodies multiscale scattering velocity dispersion pulse transmission method
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Development of RAMS-CMAQ to Simulate Aerosol Optical Depth and Aerosol Direct Radiative Forcing and Its Application to East Asia
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作者 HAN Xiao ZHANG Mei-Gen +3 位作者 LIU Xiao-Hong Steven GHAN XIN Jin-Yuan WANG Li-Li 《Atmospheric and Oceanic Science Letters》 2009年第6期368-375,共8页
The air quality modeling system RAMS (Regional Atmospheric Modeling System)-CMAQ (Models-3 Community Multi-scale Air Quality) is developed to simulate the aerosol optical depth (AOD) and aerosol direct forcing (DF). T... The air quality modeling system RAMS (Regional Atmospheric Modeling System)-CMAQ (Models-3 Community Multi-scale Air Quality) is developed to simulate the aerosol optical depth (AOD) and aerosol direct forcing (DF). The aerosol-specific extinction, single scattering albedo, and asymmetry factor are parameterized based on Mie theory taking into account the aerosol size distribution, composition, refractive index, and water uptake of solution particles. A two-stream solar radiative model considers all gaseous molecular absorption, Rayleigh scattering, and aerosols and clouds. RAMSCMAQ is applied to simulate all major aerosol concentrations (e.g., sulfate, nitrate, ammonium, organic carbon, black carbon, fine soil, and sea salt) and AOD and DF over East Asia in 2005. To evaluate its performance, the simulated AOD values were compared with ground-based in situ measurements. The comparison shows that RAMSCMAQ performed well in most of the model domain and generally captured the observed variations. High AOD values (0.2 1.0) mainly appear in the Sichuan Basin as well as in central and southeastern China. The geographic distribution of DF generally follows the AOD distribution patterns, and the DF at the top-of-the-atmosphere is less than 25 and 20 W m 2 in clear-sky and all-sky over the Sichuan Basin. Both AOD and DF exhibit seasonal variations with lower values in July and higher ones in January The DF could obviously be impacted by high cloud fractions. 展开更多
关键词 CMAQ AOD aerosol direct forcing model development
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