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A matrix inversion approach of computing T-matrix for axially symmetrical particles of extreme shape and dielectrically large dimension

机译:计算极端形状且介电大尺寸的轴向对称粒子的T矩阵的矩阵求逆方法

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摘要

[1] The T-matrix method has been widely used in radar meteorology because hydrometeors approximate to spheroidal shapes and their sizes are comparable to the sensing wavelength. However, it is considered unsuitable to solve in remote sensing problems concerning vegetation because the particles of interest, leaves and branches, are considered extremely shaped and of large dielectric dimensions, therefore beyond the domain of direct T-matrix algorithms. By solving two linear equation sets, this paper proposes a matrix inversion approach to calculate indirectly the T-matrix of regularly shaped scatterers in the crown layer of canopies. We adopt an existing electromagnetic (EM) model to calculate the scattering amplitudes as the left hand side of the equations. The number of the unknowns in the equations decreases by almost half, thus reducing the kernel computation to a significant extent when we assume that the particles are symmetrical in most remote sensing applications. The observed consistency between the scattering coefficients computed by the obtained T-matrix and those by the EM model indicates that the valid aspect ratio of this proposed method spans from 0.02 to 200, although this ratio may possibly extend with further verification. The proposed T-matrix calculation method can work at either the far-zone or the near-zone. However, it should be noted that the T-matrix obtained in the far-zone could not yield correct scattering results in the near-zone; on the contrary, the T-matrix obtained from the near-zone can produce accurate scattering fields/coefficients in what is further than the region of matching.
机译:[1] T型矩阵方法已广泛用于雷达气象学中,因为水凝体近似于球体形状,其大小可与传感波长相媲美。然而,由于感兴趣的粒子,叶子和树枝被认为是形状极大且介电尺寸较大,因此不适合直接T矩阵算法的领域,因此不适合解决有关植被的遥感问题。通过求解两个线性方程组,本文提出了一种矩阵求逆方法,间接计算冠层冠层规则形状散射体的T矩阵。我们采用现有的电磁(EM)模型来计算散射振幅,将其作为方程的左侧。等式中未知数的数量减少了近一半,因此,当我们假设粒子在大多数遥感应用中是对称的时,内核的计算将大大减少。观测到的由获得的T矩阵计算的散射系数与EM模型计算的散射系数之间的一致性表明,尽管有可能通过进一步的验证来扩展此方法,但该方法的有效纵横比范围为0.02至200。所提出的T矩阵计算方法可以在远区或近区工作。但是,应该注意的是,在远区获得的T矩阵不能在近区产生正确的散射结果。相反,从近区获得的T矩阵可以在比匹配区域更远的地方产生准确的散射场/系数。

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  • 来源
    《Radio Science》 |2012年第5期|RS5005.1-RS5005.14|共14页
  • 作者单位

    Institute of Remote Sensing and GIS, Peking University, Beijing, China,School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, Oklahoma, USA;

    Institute of Remote Sensing and GIS, Peking University, Beijing 100871, China;

    School of Civil Engineering and Environmental Sciences, University of Oklahoma, Norman, Oklahoma, USA,Atmospheric Radar Research Center, University of Oklahoma, Norman, Oklahoma, USA;

    Atmospheric Radar Research Center, University of Oklahoma, Norman, Oklahoma, USA,School of Meteorology, University of Oklahoma, Norman, Oklahoma, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
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