首页> 外文学位 >Analysis of cirrus particle size distributions from three in situ flight campaigns: Applications to cirrus microphysics and parameterization, remote sensing, and radar forward model simulators.
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Analysis of cirrus particle size distributions from three in situ flight campaigns: Applications to cirrus microphysics and parameterization, remote sensing, and radar forward model simulators.

机译:分析来自三个原位飞行运动的卷云粒径分布:卷云微物理和参数化,遥感和雷达前向模型模拟器的应用。

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摘要

A database of cirrus particle size distributions (PSDs), with concomitant meteorological variables, has been constructed using data collected with the Two-dimensional Stereo (2D-S) probe. Parametric functions are fit to each measured PSD. Full statistical descriptions are given for unimodal fit parameters. Three statistical tests were developed in order to determine the utility of bimodal fits and the efficacy of unimodal fits, and an investigation into the relationship between the parameterized PSDs and several meteorological variables was made.;Next, a parameterization of a "universal" cirrus PSD is given. This parameterization constitutes an improvement on earlier works due both to the size of the dataset and to updated instrumentation. Despite earlier works that predicted a gamma-distribution tail to the universal ice PSD, it is shown here that the tail is best described by an inverse gamma distribution. A method for predicting any PSD given the universal shape and two independent remote sensing measurements is demonstrated.;The constructed PSD database is then used to address a straightforward question: how similar are the statistics of PSD datasets collected using the recently developed 2D-S probe to cirrus PSD datasets collected using older Particle Measuring Systems (PMS) 2D Cloud (2DC) and 2D Precipitation (2DP) probes? It is seen, given the same cloud field and given the same assumptions concerning ice crystal cross-sectional area, density, and radar cross section, that the parameterized 2D-S and the parameterized 2DC predict similar distributions of inferred shortwave extinction coefficient, ice water content, and 94 GHz radar reflectivity. However, the parameterized 2DC predicts a statistically significant higher number of total ice crystals and a larger ratio of small ice crystals to large ice crystals.;Finally, the beginnings of two works in their early stages are presented. First, the probability structure of the parameterized PSDs is considered in light of application to the Bayesian inference of cirrus microphysical properties from remote sensing measurements. Then, the collection of measured PSDs, along with a forward model for radar reflectivity, is used to investigate uncertainty in computations of radar reflectivity from modeled moments of cirrus cloud PSDs.
机译:使用二维立体(2D-S)探针收集的数据,建立了具有伴随的气象变量的卷云粒径分布(PSD)数据库。参数函数适合每个测量的PSD。给出了单峰拟合参数的完整统计描述。为了确定双峰拟合的实用性和单峰拟合的有效性,进行了三个统计检验,并研究了参数化PSD与几个气象变量之间的关系。接下来,对“通用”卷云PSD进行参数化给出。由于数据集的大小和更新的仪器,此参数化构成了对早期工作的改进。尽管较早的工作预测了通用冰PSD的伽马分布尾巴,但此处显示该尾巴最好由反伽马分布来描述。演示了一种在给定通用形状和两个独立遥感测量值的情况下预测任何PSD的方法;然后使用构建的PSD数据库解决一个简单的问题:使用最近开发的2D-S探针收集的PSD数据集的统计数据有多相似使用较旧的粒子测量系统(PMS)2D云(2DC)和2D降水(2DP)探针收集的cirrus PSD数据集?可以看出,在相同的云场和相同的冰晶横截面面积,密度和雷达横截面假设的情况下,参数化的2D-S和参数化的2DC可以预测推断的短波消光系数,冰水的相似分布含量和94 GHz雷达反射率。但是,通过参数化的2DC预测,统计上总的冰晶数量更高,并且小冰晶与大冰晶的比例更高。最后,介绍了两个工作的早期阶段的开始。首先,考虑到参数化PSD的概率结构,将其应用于遥感测量的卷云微观物理特性的贝叶斯推断。然后,使用测量的PSD的集合以及雷达反射率的正向模型,来研究从卷云PSD的建模时刻计算雷达反射率的不确定性。

著录项

  • 作者单位

    The University of Utah.;

  • 授予单位 The University of Utah.;
  • 学科 Atmospheric Sciences.
  • 学位 Ph.D.
  • 年度 2014
  • 页码 229 p.
  • 总页数 229
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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