干旱区研究 ›› 2024, Vol. 41 ›› Issue (1): 13-23.doi: 10.13866/j.azr.2024.01.02 cstr: 32277.14.j.azr.2024.01.02

• 天气与气候 • 上一篇    下一篇

冰雹天气的环境参量及预报模型

衣娜娜1(),苏立娟1(),郑旭程1,辛悦1,蔡敏1,李慧1,靳雨晨2   

  1. 1.内蒙古自治区人工影响天气中心,内蒙古 呼和浩特 010051
    2.内蒙古自治区气象科学研究所,内蒙古 呼和浩特 010051
  • 收稿日期:2023-08-25 修回日期:2023-10-13 出版日期:2024-01-15 发布日期:2024-01-24
  • 作者简介:衣娜娜(1989-),女,工程师,硕士研究生,主要从事云降水物理、模式研究和人工影响天气. E-mail: yinndongzhl@163.com
  • 基金资助:
    国家自然科学基金(42030604);国家自然科学基金(41965003);中国气象局创新发展专项(CXFZ2022J033);内蒙古自治区科技计划项目(2022YFSH0132);内蒙古自治区自然科学基金(2021MS04026);内蒙古自治区自然科学基金(2022MS04018);内蒙古自治区自然科学基金(2022LHMS04003)

Environmental parameters and forecast models of hail events

YI Nana1(),SU Lijuan1(),ZHENG Xucheng1,XIN Yue1,CAI Min1,LI Hui1,JIN Yuchen2   

  1. 1. Weather Modification Center of Inner Mongolia, Hohhot 010051, Inner Mongolia, China
    2. Meteorological Science Institute of Inner Mongolia, Hohhot 010051, Inner Mongolia, China
  • Received:2023-08-25 Revised:2023-10-13 Published:2024-01-15 Online:2024-01-24

摘要:

利用1959—2021年内蒙古119个国家站的冰雹观测记录与ERA5再分析数据,对比分析冰雹与非冰雹层结、水汽、特殊温度层高度、垂直风切变及云微观物理量的差异,建立冰雹预报模型,为冰雹的潜势预报提供客观定量的依据。结果表明:冰雹、非冰雹K指数、假相当位温差、垂直风切变、比湿及云微观结构差异不显著。总指数(TT)>50 ℃,850 hPa与500 hPa温度差≥28.4 ℃,大气可降水量≤24 mm,-20 ℃层高度<7.05 km,-20 ℃距0 ℃高度≤3.15 km,以上环境参量阈值可以判别超过70%的冰雹样本,同时,反向条件能判别超过70%的非冰雹样本。基于环境参量的分析,采用Fisher判别方法,利用TT、850 hPa与500 hPa温度差、-20 ℃距0 ℃高度、大气可降水量建立冰雹预报模型,模型判别准确率超过80%。

关键词: 冰雹, 降水, 环境参量, 冰雹预报模型, 内蒙古

Abstract:

Based on the hail observation records of 119 national stations in Inner Mongolia and ERA5 reanalysis data from 1959 to 2021, the differences in layer formation, water vapor, typical temperature layer height, vertical wind shear, and cloud microphysical quantities between hail and nonhail were analyzed. A hail prediction model was established to provide an objective and quantitative basis for potential hail forecasting. The results revealed that the K-index, pseudo-equivalent temperature difference, vertical wind shear, specific humidity, rain water mixing ratio, snow water mixing ratio, ice water mixing ratio, and liquid water mixing ratio were not well distinguished between hail and nonhail. The total index was >50 °C, temperature difference between 850 hPa and 500 hPa was ≥28.4 °C, precipitable water vapor was ≤24 mm, height of -20 °C was <7.05 km, and the height of -20 °C to 0 °C was ≤3.15 km. The above environmental parameter thresholds were able to identify >70% of hail samples, and the reverse condition can identify >70% of nonhail samples. Based on the analysis of the environmental parameters of hail and nonhail samples, the Fisher discriminant method was used to establish a hail prediction model using the total index, temperature difference between 850 hPa and 500 hPa, height of -20 °C to 0 °C, and precipitable water vapor. The accuracy of the model discrimination exceeded 80%.

Key words: hail, precipitation, environmental parameters, forecast model of hail, Inner Mongolia