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极化与大气后向散射系数测量。

Polarization and atmospheric backscatter coefficient measurements.

作者信息

Anderson R

出版信息

Appl Opt. 1989 Mar 1;28(5):865-74. doi: 10.1364/AO.28.000865.

Abstract

Recently, it was pointed out that polarization effects must be considered in hard target calibration of lidars. A vector theory of radiometry is developed, and it is demonstrated for a real nonideal target that the reflectance is a matrix quantity and not a scalar quantity, and all its components must be measured. These concepts can be extended to actual field measurements of the volume backscatter coefficients. The volume backscatter coefficient at range R is an averaged (4 x 4) matrix, which is averaged over the sampling depth dR = ctau/2. The transmitted beam is polarized in a definite sense, the received beam is still polarized, and both are represented as (4 x 1) Stokes vectors so that the interaction must be represented by a (4 x 4) matrix called the volume backscatter coefficient beta. Present experiments are in error for data are considered a scalar quantity with only one value not a matrix with sixteen components. Some of these components may be zero but many are not.

摘要

最近有人指出,在激光雷达的硬目标校准中必须考虑偏振效应。发展了一种辐射测量的矢量理论,并且针对一个实际的非理想目标证明,反射率是一个矩阵量而非标量,其所有分量都必须进行测量。这些概念可以扩展到体积后向散射系数的实际野外测量。距离R处的体积后向散射系数是一个平均的(4×4)矩阵,它是在采样深度dR = cτ/2上进行平均的。发射光束在特定方向上偏振,接收光束仍然偏振,并且两者都表示为(4×1)斯托克斯矢量,因此相互作用必须由一个称为体积后向散射系数β的(4×4)矩阵来表示。目前的实验存在误差,因为数据被视为只有一个值的标量,而不是具有十六个分量的矩阵。其中一些分量可能为零,但许多并非如此。

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