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Determination of the orientation of the ice crystals in a cloud

机译:确定云中冰晶的取向

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Abstract: Theoretical grounds are given in this paper for two methods of determining preferred orientation of crystal particles in a cloud. The methods proposed in the paper enable one to do this in a much simpler way than it could be done when measuring full backscattering phase matrix. One of the methods proposed assumes that a polarization lidar can be rotated as a whole, while the second technique uses rotation of the polariztion plane of a linearly polarized sounding beam. Feasibility of the former technique is illustrated in the paper with the results of field experiments on sounding of a snowfall. Recent experimental studies of crystal clouds conducted with a polarization lidar capable of measuring backscattering phase matrices (BPM) have revealed the fact that preferred orientation of symmetry axes of particles in crystal clouds is very often observed to be in horizontal plane. This conclusion is drawn from the fact that off-diagonal elements of BPMs measured differ from zero. Using a model ensemble of crystal particles of axially symmetric plates and columns one can determine the direction of preferred orientation and the degree of particles orientation about this direction. For many practical reasons it is quite desirable to try to construct a technique for detecting situations in clouds under study when a preferred orientation of crystal particles occurs, which is more simple than that based on measurements of BPMs of clouds. Below we describe two possible versions of lidar measurements using a polarization lidar with a linearly polarized sounding radiation. Such a lidar can record two cross polarized components of lidar returns from scattering medium, i.e. two first Stokes parameters. One of the versions assumes that a lidar facility can be turned around the sounding beam axis as a whole, white in the second version we need to use a $lambda@/2 phase plate in the lidar transmitter to enable changes of sounding beam polarization. In order to make understanding of the techniques proposed easier, let us remind basic relationships for a polarization lidar sensing scheme. !6
机译:摘要:本文为确定云中晶体粒子的优选取向的两种方法提供了理论依据。本文提出的方法使人们能够以比测量整个反向散射相位矩阵时更简单的方式来做到这一点。提出的方法之一假设极化激光雷达可以整体旋转,而第二种技术使用线性极化探测光束的极化平面的旋转。本文以降雪的现场试验结果说明了前一种技术的可行性。使用能够测量反向散射相位矩阵(BPM)的偏振激光雷达对晶体云进行的最新实验研究表明,经常观察到晶体云中粒子对称轴的首选方向通常是在水平面中。该结论是基于以下事实得出的:所测量的BPM的非对角元素不同于零。使用轴向对称的板和柱的晶体颗粒的模型集合,可以确定优选取向的方向和围绕该方向的颗粒取向的程度。出于许多实际原因,非常需要尝试构建一种技术来检测正在研究的云中何时出现晶体粒子的首选方向,该技术比基于云的BPM的测量更为简单。下面,我们描述使用具有线性极化探测辐射的极化激光雷达进行激光雷达测量的两种可能版本。这样的激光雷达可以记录来自散射介质的激光雷达回波的两个交叉极化分量,即两个第一斯托克斯参数。其中一个版本假定可以将激光雷达设施整体上围绕探测波束轴旋转,在第二个版本中,我们需要在激光雷达发射器中使用一个$ lambda @ / 2相位板来改变探测波束偏振,因此白色。为了使对所提出技术的理解更加容易,让我们提醒一下偏振激光雷达传感方案的基本关系。 !6

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