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Application of linear polarized light for the discrimination of frozen and liquid droplets in ice nucleation experiments

机译:直线偏振光在冰核实验中辨别冷冻和液滴的扫描

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We report on the development and test results of the new optical particle counter TOPS-Ice (Thermo-stabilized Optical Particle Spectrometer for the detection of Ice). The instrument uses measurements of the cross-polarized scattered light by single particles into the near-forward direction (42.5° ± 12.7°) to distinguish between spherical and non-spherical particles. This approach allows the differentiation between liquid water droplets (spherical) and ice particles (non-spherical) having similar volume-equivalent sizes and therefore can be used to determine the fraction of frozen droplets in a typical immersion freezing experiment. We show that the numerical simulation of the light scattered on non-spherical particles (spheroids in random orientation) considering the actual scattering geometry used in the instrument supports the validity of the approach, even though the cross-polarized component of the light scattered by spherical droplets does not vanish in this scattering angle. For the separation of the ice particle mode from the liquid droplet mode, we use the width of the pulse detected in the depolarization channel instead of the pulse height. Exploiting the intrinsic relationship between pulse height and pulse width for Gaussian pulses allows us to calculate the fraction of frozen droplets even if the liquid droplet mode dominates the particle ensemble. We present test results obtained with TOPS-Ice in the immersion freezing experiments at the laminar diffusion chamber LACIS (Leipzig Aerosol Cloud Interaction Simulator) and demonstrate the excellent agreement with the data obtained in similar experiments with a different optical instrument. Finally, the advantages of using the cross-polarized light measurements for the differentiation of liquid and frozen droplets in the realistic immersion freezing experiments are discussed.
机译:我们报告了新光学粒子计数器顶部冰的开发和测试结果(用于检测冰的热稳定光学粒子光谱仪)。该仪器使用单个颗粒进入近向方向(42.5°±12.7°)来区分球形和非球形颗粒的近向散射光的测量。这种方法允许液体水滴(球形)和具有相似体积等效尺寸的冰颗粒(非球形)之间的分化,因此可用于确定典型的浸没冻结实验中的冷冻液滴的级分。考虑到仪器中使用的实际散射几何体的非球形颗粒上散射的光散射的光的数值模拟,即使散射的光的偏振分量也支持该方法的有效性,即使是球形散射的光的交叉偏振分量液滴在这种散射角度不会消失。为了从液滴模式分离冰颗粒模式,我们使用在去极化通道中检测到的脉冲的宽度而不是脉冲高度。利用脉冲高度和高斯脉冲脉冲宽度之间的内在关系允许我们计算冷冻液滴的一部分,即使液滴模式主导粒子合奏。我们存在在层状扩散室Lacis(Leipzig气溶胶云相互作用模拟器)的浸入式冻结实验中使用顶层冰的测试结果,并与不同的光学仪器的类似实验中获得的数据展示了优异的一致性。最后,讨论了使用用于液体和冷冻液滴中的分化的交叉极化光测量的优点。

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