The simulation of ice anisotropy feature based on 3-D FDTD method
The application of RES technology is the most important method for the study of inner structure on Antarctic ice sheet.But the study on the electro-magnetic response to the anisotropy ice is still in the early stages.This paper deduced the 3-D FDTD equations which was derived from Maxwell equation and adapted to permittivity anisotropy media.Then we simulated the radar response and spatio-temporal distributing feature.The results would develop and promote the research of inner structure on ice sheet by using multi-polarization radar.
anisotropy FDTD crystal-orientation-fabric (COF)
Bangbing Wang Gang Tian Bo Sun
Department of Earth Science,Zhejiang University,Hangzhou 310027,China Polar Research Institute of China,Shanghai 200129,China
国际会议
The 3rd International Conference on Environmental and Engineering Geophysics(第三届环境与工程地球物理国际会议)
武汉
英文
473-476
2008-06-15(万方平台首次上网日期,不代表论文的发表时间)