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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >An algorithm for retrieval of cloud microphysics using 95-GHz cloud radar and lidar - art. no. 4226
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An algorithm for retrieval of cloud microphysics using 95-GHz cloud radar and lidar - art. no. 4226

机译:一种使用95 GHz云雷达和激光雷达的云微物理学检索算法-art。没有。 4226

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摘要

1] We develop a new forward algorithm for the retrieval of effective size and ice water content (IWC) of ice crystals in clouds by using collocated 95-GHz (3.16 mm) cloud radar and lidar with the wavelength of 0.532 mum. Use of radar or lidar alone has a fundamental difficulty to obtain cloud microphysics because of the wide variety of size distributions of cloud particles, though it is effective to obtain cloud macrophysical information such as cloud boundaries. The combined use of radar and lidar can overcome this problem. One unique feature of the algorithm is the attenuation-correction to the lidar signals according to the cloud microphysics determined by look-up tables of backscattering and extinction for the radar and lidar signals. Consequently, the combined system enables the retrieval of vertical profiles of the effective radius (r(eff)) and ice water content (IWC). We perform several numerical analyses of the retrieved values for potential sources of errors, that is, the shape of the size distribution, biases in the radar and lidar signals, and the effect of multiple scattering. Then we provide the formulations that describe the retrieval errors as a function of the given bias and optical thickness. Finally, we demonstrate retrieval of microphysics for ground-based observation of cirrus clouds in February 2000 in Kashima, Japan. We examine the vertical distributions of r(eff), IWC, fall velocity, and depolarization ratio as well as the interrelationships between them. The radius of the particles turns out to be the largest near the cloud bottom, and the fall velocity also shows a trend consistent with the r(eff) tendency. There are no in situ measurements to validate the retrieved parameters for the observations. Instead, supporting arguments are given on the basis of information about the expected behavior of the relationships between the cloud microphysical parameters from the literature. [References: 46
机译:1]我们开发了一种新的前向算法,该算法通过使用波长为0.532微米的95 GHz(3.16毫米)云雷达和激光雷达并置来检索云中冰晶的有效尺寸和冰水含量(IWC)。雷达或激光雷达的单独使用对获得云微物理学有一个根本的困难,因为云颗粒的尺寸分布范围很广,尽管获得诸如云边界之类的云宏观物理信息是有效的。雷达和激光雷达的组合使用可以克服此问题。该算法的一个独特功能是根据云微观物理学对激光雷达信号的衰减校正,该云微物理学是由雷达和激光雷达信号的反向散射和消光查找表确定的。因此,组合系统可以检索有效半径(r(eff))和冰水含量(IWC)的垂直轮廓。我们对检索到的值进行了一些数值分析,以找出潜在的错误源,即大小分布的形状,雷达和激光雷达信号中的偏差以及多重散射的影响。然后,我们提供将取回误差描述为给定偏差和光学厚度的函数的公式。最后,我们演示了2000年2月在日本鹿岛进行的微观物理学检索,用于对卷云进行地面观测。我们检查了r(eff),IWC,下降速度和去极化率的垂直分布以及它们之间的相互关系。颗粒半径在云底附近最大,并且下降速度也显示出与r(eff)趋势一致的趋势。没有用于验证观测值的原位测量结果。取而代之的是,根据有关文献中有关云微物理参数之间关系的预期行为的信息,给出了支持性论据。 [参考:46

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