双月刊

ISSN 1006-9895

CN 11-1768/O4

基于多源资料的东北冷涡降水垂直结构分析
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1.辽宁省人工影响天气办公室;2.辽宁省气象信息中心

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基金项目:

中国气象局沈阳大气环境研究所联合开放基金课题( 2022SYIAEKFZD03),中国气象局创新发展专项(CXFZ2022J059)


Vertical Structure Analysis of Cold Vortex over Northeast China Based on Multisource Data
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Affiliation:

1.Liaoning Weather Modification Office,Shenyang;2.Liaoning Meteorological Information Centre,Shenyang

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    摘要:

    为进一步研究东北冷涡云系降水的垂直结构,本文利用布设在辽宁省阜新蒙古族自治县国家级地面观测站内的微雨雷达和激光雨滴谱仪等设备,对2020年以来阜蒙县的三次东北冷涡降雨天气过程的微物理特征进行分析。结果表明:在层云稳定性降水主导的个例中,微雨雷达和雨滴谱仪测得的雨滴谱吻合程度较高,而在对流性降水较多的个例中,微雨雷达与雨滴谱仪观测的平均雨滴谱仅在中等粒子段(1-2.5mm)表现出较好的一致性;在层云性降水阶段,较小的冰晶粒子更快的通过零度层开始融化,小云滴在零度层下方累积,出现数浓度的极值,在该极值下方,较大的冰晶粒子经历了更长的融化距离,成为较大雨滴,同时,小云滴的累积进一步促进了大云滴的收集及碰并效应的发生,利于大雨滴的形成,在零度层下方出现一个谱宽的极值,表现为垂直方向的雨滴谱的“凸起”,“凸起”的发生到下落发生在2-3分钟之内。垂直方向雨滴谱的“凸起”可以看做在层云性降水阶段亮带促进降水的直观表现,但这种对于降水的促进在地面能否带来明显的雨强的明显增大,要取决于近地层大气中水汽含量,在辽西地区即表现为,干旱的春季,大气相对湿度较低,亮带对于地面雨滴谱的拓宽无明显帮助,但在水汽相对充沛的夏季,“凸起”的下移一定程度上导致了近地层雨滴谱拓宽及雨强的增大;相对其他地区,辽西地区降水数浓度偏小,但层云性降水和对流性降水的平均数浓度差别不大,质量加权直径的差异导致了雨强的差异。

    Abstract:

    In order to study the vertical structure of precipitation in the northeast cold vortex cloud system further, this paper analyzes the microphysical characteristics of the three northeast cold vortex rainfall weather processes in Fumeng County since 2020 by using the micro-rain radar and laser raindrop spectrometer deployed in the national ground observation station of Fuxin Mongol Autonomous County, Liaoning Province. The results show:in the cases dominated by stable precipitation of Stratus clouds, the raindrop spectra measured by the micro rain radar and the raindrop spectrometer have a good consistency, while in the cases with more convective precipitation. The average raindrop spectrum observed by the micro rain radar and the raindrop spectrometer only shows good consistency in the medium particle segment (1-2.5mm); in the stratus precipitation stage, the smaller ice crystal particles begin to melt faster through the 0℃ layer, and the small cloud droplets accumulate below the 0℃ layer, and several concentrations of extreme values appear, below the extreme value, the larger ice crystal particles experience a longer melting distance and become larger raindrops, at the same time, the accumulation of small cloud drops further promotes the collection and collision effect of large cloud droplets, which is conducive to the formation of large raindrops, and a spectral width extreme value appears below the zero degree layer, which is manifested as a vertical raindrop spectrum "Bulge", "Bulge" occurs within 2-3 minutes from the onset to the fall. The "bulge" can be seen as the intuitive performance of the bright band promoting precipitation in the stratus precipitation stage, but whether this promotion of precipitation can bring a significant increase in rainfall intensity on the ground depends on the water vapor content in the near-ground atmosphere, which is manifested in western Liaoning, in dry spring, the relative humidity of the atmosphere is low, and the bright band does not help the broadening of the raindrop spectrum on the ground, but in the summer when the water vapor is relatively abundant, the downward movement of the "Bulge" to a certain extent leads to the widening of the near-ground raindrop spectrum and the increase of rain intensity; Compared with other regions, the precipitation concentration in western Liaoning is small, but the average concentration of stratus precipitation and convective precipitation is not much different, and the difference in mass-weighted diameter leads to the difference in rain intensity.

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  • 收稿日期:2023-07-11
  • 最后修改日期:2023-12-19
  • 录用日期:2024-04-01
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