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首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >A methodology for simultaneous retrieval of ice and liquid water cloud properties. Part 2: Near-global retrievals and evaluation against A-Train products
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A methodology for simultaneous retrieval of ice and liquid water cloud properties. Part 2: Near-global retrievals and evaluation against A-Train products

机译:同时获取冰和液态水云特性的方法。第2部分:针对A-Train产品的近乎全局的检索和评估

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摘要

This article presents results of a novel methodology capable of simultaneously retrieving optical and microphysical properties of multi-level ice and liquid clouds. The method was introduced in Part I, which theoretically demonstrated its capabilities, and its results are here analysed and evaluated against A-Train operational products. In addition to being robust to multi-layer conditions, another advantage of the method is that rigorous uncertainties and analysis tools are attached to its retrievals. Also, the combined use of short-wave and thermal infrared channels provides a wide range of sensitivity from moderately thin to thick ice cloud layers. Finally, the method is also novel in that the ice water path (IWP) is directly retrieved. These new retrievals should therefore be useful in providing new data for evaluating climate model predictions of IWP. In this study, our methodology has been applied to one year of A-Train measurements, narrowed to daytime conditions over oceanic surfaces. The retrievals and their uncertainties are statistically analysed, after a thorough discussion of the filtering process. It appears that our method is sensitive to IWPs ranging between about 0.5 and 1000gm(-2), with uncertainties better than 25% between 5 and 500gm(-2). Retrievals of the optical depth and effective radius of liquid layers have uncertainties better than 20%. Our retrievals are then compared to five independent operational A-Train products. Very good agreements, well within a factor of 2, are found by comparisons to products from active and passive instruments. These results overall lead to the validation of our method. Additionally, the robustness of passive operational products to multi-layer conditions is discussed. Preliminary comparisons show a possible overestimation of retrievals obtained under the single-layer approximation. A thorough assessment of this problem will be addressed in a following study.
机译:本文介绍了一种新型方法的结果,该方法能够同时检索多层冰和液云的光学和微物理特性。该方法在第I部分中进行了介绍,从理论上证明了其功能,并在此根据A-Train的操作产品对结果进行了分析和评估。除了对多层条件具有鲁棒性之外,该方法的另一个优点是,严格的不确定性和分析工具已附加到其检索中。此外,短波和热红外通道的组合使用可提供从中等厚度的薄到厚的冰云层的广泛灵敏度。最后,该方法也是新颖的,因为直接检索冰水路径(IWP)。因此,这些新的检索结果应有助于提供新数据,以评估IWP的气候模型预测。在这项研究中,我们的方法已应用于一年的A-train测量,范围仅限于海洋表面的白天条件。在对过滤过程进行了全面讨论之后,对检索结果及其不确定性进行了统计分析。看来我们的方法对IWP敏感,范围在0.5至1000gm(-2)之间,不确定性在5至500gm(-2)之间优于25%。液体层的光学深度和有效半径的检索不确定性优于20%。然后将我们的检索结果与5种独立的A火车产品进行比较。通过与有源和无源仪器的产品进行比较,可以找到很好的协议(大约在2倍以内)。这些结果总体上证明了我们方法的有效性。此外,讨论了无源操作产品对多层条件的鲁棒性。初步比较显示,在单层近似下可能会高估检索结果。在接下来的研究中将对这个问题进行彻底的评估。

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