J4 ›› 2008, Vol. 26 ›› Issue (4): 35-40.

• 论文 • 上一篇    下一篇

2008年北京一次春季层状云探测分析

金 华,马新成,黄梦宇,何 晖,李睿劼,周 嵬   

  1. 北京市人工影响天气办公室,北京 100089
  • 收稿日期:2008-10-30 修回日期:2008-11-20 出版日期:2008-12-30 发布日期:2008-12-30
  • 作者简介:金华(1976-) ,男,河南省卫辉市人,硕士,工程师,从事人工影响天气工作. E-mail: jinhuawm@gmail. com
  • 基金资助:

    北京市优秀人才培养资助项目“新型云粒子探测系统对北京地区云和降水的机理研究”(20081D0200800058)及国家科技支撑计划课题“北京地区人工消雾技术研究”(2006BAC12B04)资助

An AircraftObserva tion of a Stra tiform Cloud in Spring 2008 of Beijing

 JIN Hua, MA Xincheng, HUANGMengyu, HE Hui, L I Ruijie, ZHOU Wei   

  1. Beijing Weather Modif ication Office , B eijing 100089, China
  • Received:2008-10-30 Revised:2008-11-20 Online:2008-12-30 Published:2008-12-30

摘要:

利用云和降水探测设备(DMT - PMS)对一次层状云降水过程进行了探测。分析发现CAS(云及气溶胶粒子探头)在该弱降水云中测得的云粒子平均浓度大于FSSP在其他地区层状云中所测平均值, CIP (二维云粒子图像探头)与2D - C及2D - GA2所测冰晶粒子平均浓度接近, P IP (二维降水粒子探头)与2D - P所测降水粒子平均浓度相当。观测发现云区雪晶浓度与冰晶浓度呈正相关关系,在冰晶浓度< 104个/m3时,雪晶、冰晶浓度之比与冰晶浓度为负相关关系;在冰晶浓度> 104个/m3的时刻,雪晶、冰晶浓度之比不因冰晶浓度变化而变化。温度为- 10~ - 12 ℃的云区云水条件丰富,有较多的冰晶在该层孕育;降水粒子在温度- 7~ - 10 ℃的云区生长。温度为- 5~ - 7 ℃的云区云水不丰富,降水粒子蒸发变小;温度为- 4~ - 5 ℃的云区仅有少量的降水粒子。

关键词: DMT - PMS, 云探测, 云粒子, 降水粒子

Abstract:

A stratiform cloud wasmeasured with a ParticleMeasurement System ( PMS) p roduced byDrop letMeasurement Technologies (DMT) and mounted on a Y - 12 aircraft in sp ring of 2008, Beijing. It was found that the average concentration of cloud particles measured by CAS (Cloud and Aerosol Spectrometer) was bigger than those valuesmeasured by FSSP in other areas of north China. It was also found that the average concentrations of ice particlesmeasured by CIP (Cloud Imaging Probe) , 2D - C and 2D - GA2 were all similar. A positive correlation was found between snow and ice crystals’concentrations. A negative correlation was found between the concentration of ice crystal and the ratio of snow and ice crystal concentrationswhen the concentration of ice crystalswas less than 104 m- 3 , butwhen more than 104 m- 3 , the ratio of snow and ice crystal concentration is a constant. Many ice crystals were found in the cloud field where the temperature ranged from - 10 to - 12 ℃, and there wasmore supercooled water in the field. The p recip itation particleswere p ropagated in the cloud filed where the temperature ranged from - 7 to - 10 ℃. Precip itation particles evaporated and became smaller in the cloud filed where the temperature ranged from - 5 to - 7 ℃. L ittle p recip itation particleswas found in the cloud field where the temperature ranged from - 4 to - 5 ℃.

Key words: DMT - PMS, cloud observation, cloud particle, p recip itation particle

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