首页|岱海流域一次降雨过程微物理特征分析

岱海流域一次降雨过程微物理特征分析

扫码查看
利用 2018 年 5 月 10 日岱海流域一次飞机增雨探测资料,对层状云降水微物理特征进行分析.结果表明:此次降水过程受500 hPa高空槽与700 hPa河套气旋影响,是一次典型的春季层状云降水过程.飞机探测降水过程中层状云中下部降水粒子数浓度、云粒子数浓度均较小,且云微物理量的水平分布均表现出明显的不均匀性.云中 62.6%的液态水含量大于0.002 g·m-3,83.2%的过冷水含量大于0.01 g·m-3,过冷水含量主要介于0.01~0.05 g·m-3.
Microphysical Characteristics Analysis of a Precipitation Process in the Daihai Basin
The microphysical characteristics of pallio-nimbuses were analyzed based on the aircraft precipitation enhancement detection data of the Daihai Basin on May 10,2018.The results showed that this precipitation process was affected by the 500 hPa high-level trough and the 700 hPa Hetao cyclone,representing a typical stratiform precipitation process in spring.The number concentrations of precipitation particles and cloud particles in the middle and lower parts of stratiform clouds were low,and the horizontal distribution of cloud microphysical quantities exhibited significant inhomogeneity.62.6%of the liquid water content was greater than 0.002 g·m-3,and 83.2%of the supercooled water content was greater than 0.01g·m-3,with the supercooled water mainly located within the range of 0.01 to 0.05 g·m-3.

Soaking rainCould microphysical structureArtificial precipitation stimulation

许志丽、毕力格、郑旭程、贺志宇、张峰、张杰

展开 >

内蒙古自治区人工影响天气中心,内蒙古 呼和浩特 010051

内蒙古自治区人工影响天气重点实验室,内蒙古 呼和浩特 010051

降雨过程 云微物理结构 人工增雨

2024

内蒙古气象
内蒙古气象局 内蒙古气象气象学会

内蒙古气象

影响因子:0.206
ISSN:1005-8656
年,卷(期):2024.(6)