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Echo characteristics and application of "20230322" Leping heavy rainstorm |
Zheng Kani1, Ji Wei2 |
1. Leping Meteorological Bureau, Leping 333000; 2. Jingdezhen Meteorological Bureau, Jingdezhen 333000 |
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Abstract In order to better predict the heavy rainstorm and short-time heavy precipitation in Leping, this paper analyzes the echo of the 2023-03-22 heavy rainstorm process and short-time heavy precipitation by using MICAPS weather map, rainfall of Leping Automatic Weather Station, radar echo and other data, using synoptic, radar meteorology and other principles and image recognition technology.The results show that the convective characteristics of heavy rainstorm are obvious, accompanied by strong convective weather such as heavy precipitation and lightning.On the sounding map, there is a typical "horn mouth" structure, the trough moves eastward, cold air intersects with southwest airflow, upper level divergence, and ground convergence, leading to heavy precipitation.Heavy precipitation is accompanied by significant strong lightning, and the lightning density in Leping, where precipitation intensity is highest, is also the strongest.At the beginning of heavy precipitation, strong lightning generally occurs before heavy precipitation, while during or near the end of the heavy precipitation process, strong lightning lags behind heavy precipitation.The areas south of the TBB strong center with dense contour lines have the strongest convection and are most likely to induce heavy precipitation.When a large area of strong echoes above 45 dBZ appears upstream of the measuring station and moves towards the measuring station, the area of the strong echoes reaches ≥300 km2, which will lead to heavy precipitation ≥30 mm/h.Early warning information should be issued.It is hoped that the research results can play a guiding role in monitoring, warning and forecasting services of Leping heavy rainstorm and short-term heavy rainfall.
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Received: 18 June 2024
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[1] |
张延亭,林铍德.致洪暴雨成因分析及预报[J].江西气象科技,1994(2):10-14.
|
[2] |
张延亭,张瑛.江西“98.6”连续暴雨形成的特殊性[J].气象,1999(6):9-13.
|
[3] |
金米娜.江西省汛期暴雨气候特点及预报方法综合分析[J].气象与减灾研究,2009,32(1):69-72.
|
[4] |
尹洁,何拥凤,陈云辉,等.2013年6月江西一次持续性暴雨过程分析[J].暴雨灾害,2013,32(4):314-323.
|
[5] |
尹洁,郑婧,张瑛,等.一次梅雨锋特大暴雨过程分析及数值模拟[J].气象,2011,37(7):827-837.
|
[6] |
陈鲍发,马中元,王立志,等.江西昌江流域特大暴雨短时强降水回波特征分析[J].气象,2022,48(11):1418-1427.
|
[7] |
陈鲍发,马中元,黄龙飞,等.赣东北致洪暴雨的天气分型和回波特征分析[J].气象水文海洋仪器,2021,38(3):18-22.
|
[8] |
陈鲍发,黄龙飞,马中元,等.2020年7月710日江西连续性大暴雨过程成因分析[J].江西科学,2021,39(3):457-463.
|
[9] |
陈鲍发,黄龙飞,蔡俊峰,等.超低空急流背景下的景德镇市大暴雨过程分析[J].江西科学,2018,36(1):101-105,140.
|
[10] |
郑卡妮,马中元,陈鲍发.2022-06中旬乐平连续性大暴雨特征分析[J].气象水文海洋仪器,2023,40(1):79-81,85.
|
[11] |
蔡俊峰,陈鲍发,余欣.赣东北3类致洪暴雨的对比分析[J].江西科学,2017,35(2):219-225.
|
[12] |
刘懿枢,马中元,余剑浩,等.“2022-3-16”一次超级单体冰雹回波特征分析[J].气象水文海洋仪器,2022,39(3):15-18.
|
[13] |
张王鹏,程成,廖满庭,等.铜鼓及上游地区短时强降水回波特征分析[J].气象水文海洋仪器,2024,41(2):14-16.
|
[14] |
李密,刘懿枢,杨洁.鹰潭2023年7月短时强降水雷达回波特征分析[J].气象水文海洋仪器,2024,41(1):53-55,59.
|
[15] |
卢秋芳,马中元,陈鲍发,等.江西省副高边缘强天气的云图和回波特征分析[J].气象水文海洋仪器,2020,37(3):25-31.
|
|
|
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