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Determination of 3D Cloud Ice Water Contents by Combining Multiple Data Sources from Satellite, Ground Radar, and a Numerical Model

机译:通过组合来自卫星,地面雷达和数值模型的多个数据源确定3D云冰水含量

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This study aims at determining the three-dimensional distribution of ice water content over a broad area near the Atmospheric Radiation Measurement Program Southern Great Plains site, where cloud radar and meteorological observations have been routinely conducted. Together with wind fields from other measurements, the ice water content retrievals can be used to derive the cloud ice water advective tendency terms needed for single-column model simulations. In this study, a Bayesian retrieval algorithmhas been developed that combines multiple data sources from satellite high-frequency microwave radiometry, ground cloud radar observations, and mesoscale numerical model analysis. The cloud radar observations allow the characteristics of vertical ice water content structures to be inferred. The numerical model data are used to locate the cloud height. The satellite data provide information on the integrated ice water path, its horizontal distribution over a broad area, and, to a lesser extent, the vertical structure of ice water content. The approach herein is to retrieve the three-dimensional cloud ice water content in a 10 deg × 10 deg area surrounding the cloud radar site by combining all the information contained in the above datasets through aBayesian framework. Validation of the algorithm has been done by comparing the retrievals with measurements from two ground radars. The comparison shows that the mean ice water content profiles and the two-dimensional (height–ice water content) probability density functions retrieved for 19 coincident cases agree fairly well with the validation data. However, the retrieved ice water contents generally lack detailed vertical structures because of the low sensitivity of satellite data to the vertical variation of cloud ice.
机译:这项研究的目的是确定大气辐射测量计划南部大平原站点附近广阔区域中冰水含量的三维分布,在那里定期进行云雷达和气象观测。结合其他测量的风场,冰水含量的反演可用于得出单塔模型模拟所需的云冰水对流趋势项。在这项研究中,开发了一种贝叶斯检索算法,该算法结合了来自卫星高频微波辐射测量,地云雷达观测和中尺度数值模型分析的多个数据源。通过云雷达观测可以推断出垂直冰水含量结构的特征。数值模型数据用于定位云层高度。卫星数据可提供有关综合冰水路径,其在大面积上的水平分布以及较小程度的冰水含量垂直结构的信息。本文中的方法是通过贝叶斯框架合并上述数据集中包含的所有信息,以获取围绕云雷达站点的10度×10度区域中的三维云冰水含量。通过将检索结果与两个地面雷达的测量值进行比较,对算法进行了验证。比较结果表明,从19个重合情况中获得的平均冰水含量曲线和二维(高冰水含量)概率密度函数与验证数据非常吻合。但是,由于卫星数据对云冰垂直变化的敏感性较低,因此,取回的冰水含量通常缺乏详细的垂直结构。

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