干旱气象 ›› 2023, Vol. 41 ›› Issue (6): 933-943.DOI: 10. 11755/j. issn. 1006-7639(2023)-06-0933

• 论文 • 上一篇    下一篇

基于深度学习的积层混合云对流泡降水粒子特征研究

  

  1. 1. 山东省气象局气象防灾减灾重点实验室,山东 济南 250031;
    2. 山东省气象数据中心,山东 济南 250031;
    3. 山东省人民政府人工影响天气办公室,山东 济南 250031;
    4. 河北省人工影响天气中心,河北 石家庄 050021;
    5. 中国气象局人工影响天气中心,北京 100081;
    6. 山东省气象台,山东 济南 250031
  • 收稿日期:2022-11-14 修回日期:2023-10-10 出版日期:2023-12-31 发布日期:2024-01-03
  • 通讯作者: 王烁(1992—),男,山东邹城人,工程师,主要从事云降水物理研究。E-mail:wskfg123@163.com
  • 作者简介:袁雅涵(1996—),女,山东东明人,工程师,主要从事机器学习算法研究。E-mail:foreverlamaara@163. com
  • 基金资助:

    中国气象局创新发展专项(CXFZ2022J034)、山东省气象局科研项目(2022sdqxz13、2022SDQN03)、中部区域积层混合云人工增 雨(雪)研究试验(商丘)项目(ZQC-H22256)

A study on particle characteristics of generating cells in stratiform-cumulus mixed cloud based on convolution neural network

  1. 1. Shandong Key Laboratory for Meteorological Disaster Prevention and Reduction, Ji’nan 250031, China; 

    2.Shandong Meteorological Data Center,Ji’nan 250031,China; 

    3.Shandong Weather Modification Office,Ji’nan 250031,China; 

    4.Hebei Weather Modification Center, Shijiazhuang 050021,China;

    5. CMA Weather Modification Center, Beijing 100081, China; 

    6.Shandong Meteorological Observatory, Ji’nan 250031, China

  • Received:2022-11-14 Revised:2023-10-10 Online:2023-12-31 Published:2024-01-03

摘要:

为实现对降水粒子的高精准分类,整理3 a机载探测降水粒子图像,构建山东省降水粒子图像 数据集(Shandong Province Precipitation Particle Image Dataset, SD-PPID)。结合多维度混和的模型放 缩方法,提出一种基于EfficientNet卷积神经网络的降水粒子识别模型(A Precipitation particle Recogni⁃ tion model based on EfficientNet convolutional neural Network,PREN)。通过多模型、多指标评价对比, 验证了 PREN 模型具有较好的性能和分类识别能力,模型的识别准确率、精准率和召回率均为 98%。 使用 PREN模型分析对流泡降水粒子特征,选取 2次典型积层混合云降水过程的 3个时段,结合机载 Ka 波段云雷达(Airborne Ka-Band Precipitation Cloud Radar,KPR)和 DMT 粒子测量系统(Droplet Mea⁃ surement Technologies)分析对流泡内部与外部、不同强度和不同高度的降水粒子形状占比,并研究其 降水机制。结果表明,PREN可有效识别对流泡降水粒子的特征。对流泡内,主要是球状、针状、不规 则状和柱状降水粒子,而对流泡外降水粒子主要为球状和针状。不同强度的对流泡云微物理参数各 不相同。降水成熟阶段对流泡内霰粒子和针状粒子占比高于消散阶段,降水成熟阶段降水粒子平均 弦长415 µm,而消散阶段粒子平均弦长367 µm。对流泡上部降水粒子以球状和六边形板状为主,主 要通过凝华过程增长。在0 ℃层,不规则状粒子和柱状粒子的比例增加,融化过程与动力条件有利于 碰并增长形成不规则状粒子,柱状粒子主要来自于高层掉落。

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Abstract:

Arranging 3 years’ worth of airborne precipitation particle images to construct a precipitation particle image dataset in Shan⁃ dong Province. Building a precipitation particle recognition model based on EfficientNet convolutional neural network, named PREN (Precipitation particle Recognition model based on EfficientNet convolutional neural Network).The accuracy rate is 98%, and the multimodel and multi-index evaluation and comparison experiments verify that PREN demonstrates excellent robustness and generalization ability. Taking typical stratiform-cumulus mixed cloud precipitation as two examples (total 3 time periods), PREN is applied to the par⁃ ticle characteristics analysis of generating cells. Combined with airborne Ka-band cloud radar and DMT particle measurement system, an analysis conducted on the shape proportion of precipitation particles inside and outside the generating cells and indifferent intensity generating cells, revealing the precipitation mechanism. The results show that the shapes of precipitation particles in the generating cells are mainly spherical, needle-like, irregular and columnar. Precipitation particles outside the generating cells are mostly spherical and needle-like. The cloud microphysical parameters in the generating cells with different intensities vary. The proportion of graupel and needle particles in the precipitation maturity stage is higher than that in the dissipation stage. The average chord length of precipi⁃ tation particles in the maturity stage is 415 µm. While the average chord length of particles in dissipation stage is 367 µm. The particles on the top of generating cells are mainly spherical and hexagonal, primarily growing through the process of deposition. The ratio of irregular particles and columnar particles in the 0 ℃ are increasing, and the melting process and dynamic conditions favor aggregation and growth, forming irregular particles, while columns mainly originate from the upper levels of the atmosphere.

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