用户名: 密码: 验证码:
Stokes Parameters in Polarimetric Passive Remote Sensing from Two-layer Rough Surfaces
详细信息    查看全文 | 下载全文 | 推荐本文 |
  • 作者:Peng XULeung TSANGKun-Shan CHEN
  • 会议时间:2011-08-01
  • 关键词:polarimetric passive remote sensing ; layered rough surface ; emissivity
  • 作者单位:Peng XU(School of Electronic Information, Wuhan University, Wuhan 430079, China)Leung TSANG(Department of Electrical Engineering, University of Washington, Seattle, WA 98195, USA)Kun-Shan CHEN(Center for Space and Remote Sensing, National Central University, Chung-Li 32054, Taiwan)
  • 母体文献:第五届海峡两岸遥感遥测会议论文集
  • 会议名称:第五届海峡两岸遥感遥测会议
  • 会议地点:哈尔滨
  • 主办单位:中国地理学会
  • 语种:chi
  • 分类号:TG1;TB1
摘要
from Two-layer Rough Surfaces Peng XU 1 , Leung TSANG 2 , Kun-Shan CHEN 3 1. School of Electronic Information, Wuhan University, Wuhan 430079, China; 2. Department of Electrical Engineering, University of Washington, Seattle, WA 98195, USA; 3. Center for Space and Remote Sensing, National Central University, Chung-Li 32054, Taiwan ABSTRACT It is shown in our previously published results that the large fourth Stokes parameter can be created from a rough surface over multi-layered media. In this paper we consider the four Stokes parameters in microwave emission from two-layer rough surfaces. The rough surfaces vary in one horizontal direction so that azimuthal asymmetry exists in the 3-D problem. Periodic boundary conditions are used. The numerical results show that the two-layer periodic rough surfaces can also reduce the vertical and horizontal brightness temperatures remarkably. The interactions between the two rough surfaces also enhance the third and fourth Stokes parameters. In particular, the fourth Stokes parameter can be larger than previous layered structure. The results presented in this paper are compared with the previously published results from a rough surface over multi-layered media, the new structure can remove the large valleys in the vertical and horizontal brightness temperatures from the former sastrugi structure. It is found that the reasons resulting in the large fourth Stokes parameter are not interfaces乫 shapes below the first rough surface but the first rough surface乫s shape and relative magnitude of permittivities of region 1 and 2, all cases with the large fourth Stokes parameter should satisfy ε2 ε1 due to total internal reflection from layers.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700