Modeling of Melting Layer in Cross-Platforms Radar Observation Operator ZJU-AERO: Multi-Stage Melting Particle Model, Scattering Computation, and Bulk Parameterization

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of Geophysical Research: Atmospheres Pub Date : 2024-10-10 DOI:10.1029/2024JD040725
Hejun Xie, Lei Bi, Zheng Wang, Wei Han
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Abstract

This study presents an implementation of a new melting layer model in the ZJU-AERO radar observation operator (Accurate and Efficient Radar Operator designed by ZheJiang University). The proposed model utilizes a coated spheroid to represent melting snow and graupel. It consists of three stages–coating, soaking, and melting–to account for the dielectric and density effects of melting particles. The scattering properties of the melting particles are computed with the Invariant-Imbedding T-Matrix (IITM) method, and the results are tabulated as look-up tables for the radar operator. Regarding the parameterization of bulk optical properties, a flux-conservation scheme is employed to estimate the size distribution of melting particles. To demonstrate its flexibility and superiority, the single and bulk scattering properties of our multi-stage melting model are compared against the traditional homogeneous model, which uses the effective medium approximation (EMA). The effectiveness of the multi-stage melting model has also been assessed by mapping model states in the regional mesoscale model of the China Meteorology Administration (CMA-MESO) to radar observations. In the microphysics package of CMA-MESO, the melting process is not explicitly represented, and we assume that melting hydrometeors occur where solid and liquid phases overlap. When compared with observations, the present multi-stage melting model successfully reproduces melting layer signatures, highlighting its potential for microphysic validation, quantitative precipitation estimations, and data assimilation studies.

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ZJU-AERO 跨平台雷达观测操作器中的熔融层建模:多级熔融粒子模型、散射计算和块体参数化
本研究介绍了一种新的融化层模型在 ZJU-AERO 雷达观测运算器(浙江大学设计的精确高效雷达运算器)中的应用。所提出的模型利用一个涂层球体来表示融化的雪和冰砾。它包括三个阶段--涂层、浸泡和融化,以考虑融化颗粒的介电效应和密度效应。熔化颗粒的散射特性是用因变-嵌入 T 矩阵(IITM)方法计算出来的,计算结果作为雷达算子的查找表。关于体光学特性的参数化,采用了通量守恒方案来估算熔化颗粒的尺寸分布。为了证明其灵活性和优越性,我们将多级熔化模型的单散射和体散射特性与使用有效介质近似(EMA)的传统均质模型进行了比较。此外,还通过将中国气象局区域中尺度模式(CMA-MESO)中的模式状态与雷达观测数据进行映射,评估了多级融化模式的有效性。在 CMA-MESO 的微观物理软件包中,没有明确表示融化过程,我们假设融化的水介质发生在固相和液相重叠的地方。与观测结果相比,本多级融化模式成功地再现了融化层特征,突出了其在微观物理验证、定量降水估算和数据同化研究方面的潜力。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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