| 一次冷锋云系的宏微观物理特征分析 |
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| 引用本文： | 孟宪罗,汤达章,郭金平,裴宇杰,赵娜,秦彦硕,段宇辉,赵利品.一次冷锋云系的宏微观物理特征分析[J].南京气象学院学报,2014,6(6):539-548. |
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| 作者姓名： | 孟宪罗 汤达章 郭金平 裴宇杰 赵娜 秦彦硕 段宇辉 赵利品 |
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| 作者单位： | 南京信息工程大学 大气科学学院, 南京, 210044;河北省气象技术装备中心, 石家庄, 050021;南京信息工程大学 大气科学学院, 南京, 210044;河北省人工影响天气办公室, 石家庄, 050021;河北省气象台, 石家庄, 050021;河北省气象服务中心, 石家庄, 050021;河北省人工影响天气办公室, 石家庄, 050021;河北省气象台, 石家庄, 050021;河北省人工影响天气办公室, 石家庄, 050021 |
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| 基金项目： | 河北省科技厅项目(11277107D) |
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| 摘 要： | 利用常规气象资料、自动站资料、卫星云图、CINRAD-SA多普勒天气雷达资料以及NCEP再分析资料,结合飞行探测数据,对影响2011年4月17日河北抚宁县森林大火的一次冷锋云系进行分析.结果表明:1)宏观分析,过程降水的水汽仅来自冷锋自身所携带的微弱水汽,水汽辐合值较小,不利降水;2)微观分析,冷锋层状云系在水平和垂直方向上存在较薄的过冷水云区,小粒子数浓度大于20 cm-3的云区占一定比例.飞机催化作业后,雷达回波强度增强,CAS(云气溶胶粒子探头)探测的小粒子数浓度、云含水量及粒子平均直径均有明显变化,说明该次冷锋云系有一定的增雨潜力.
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| 关 键 词： | 冷锋 层状云 增雨潜力 过冷水 |
| 收稿时间： | 2013/12/10 0:00:00 |
Analysis of macro-scale and micro-scale characteristics of a cold-front cloud |
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| MENG Xianluo,TANG Dazhang,GUO Jinping,PEI Yujie,ZHAO N,QIN Yanshuo,DUAN Yuhui and ZHAO Lipin.Analysis of macro-scale and micro-scale characteristics of a cold-front cloud[J].Journal of Nanjing Institute of Meteorology,2014,6(6):539-548. |
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| Authors: | MENG Xianluo TANG Dazhang GUO Jinping PEI Yujie ZHAO N QIN Yanshuo DUAN Yuhui and ZHAO Lipin |
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| Institution: | School of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044;Hebei Meteorological Equipment Center, Shijiazhuang 050021;School of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing 210044;Weather Modification Office of Hebei Province, Shijiazhuang 050021;Hebei Meteorological Observatory, Shijiazhuang 050021;Hebei Meteorological Service Center, Shijiazhuang 050021;Weather Modification Office of Hebei Province, Shijiazhuang 050021;Hebei Meteorological Observatory, Shijiazhuang 050021;Weather Modification Office of Hebei Province, Shijiazhuang 050021 |
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| Abstract: | The characteristics of a cold-front cloud during the forest fire on April 17,2011 in Funing county of Hebei province,were analyzed at macro and micro scale.Meteorological data of conventional observations,satellite cloud image,Doppler weather Radar data,aircraft observation,and the NCEP reanalysis data were used to analyze the precipitation enhancement potential of this cold-front cloud.Macroanalysis shows that the water vapor carried by the cold-front cloud is the only source of the artificial precipitation enhancement,which is small in moisture convergence thus not favorable for precipitation.Microanalysis shows that relatively thin supercooled water area exists in both horizontal and vertical direction of the cold-front stratiform cloud system,with certain proportion of small particle concentration>20 cm-3 in size.After the feeding operation,the radar echo intensity is enhanced,parameters of the particle concentration,LWC and the mean diameter of particles detected by CAS change significantly.Results show that the cold-front cloud has certain precipitation enhancement potential. |
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| Keywords: | cold-front stratiform cloud precipitation enhancement potential super-cooled water |
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