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云中过冷水识别的飞机观测研究:云粒子数浓度与积冰概率和球形粒子占比的相关性OACSTPCD

Identifying Supercooled Liquid Water in Cloud Based on Airborne Observations:Correlation of Cloud Particle Number Concentration with Icing Probability and Proportion of Spherical Particles

中文摘要英文摘要

云中过冷水区的识别无论对人工影响天气、航空飞行安全和大气辐射研究等都至关重要.迄今为止,过冷水区的飞机识别多依赖于经验估计,迫切需要观测的验证和量化的识别标准.2018和2019年,空中国王B-10GD飞机上同时装载云粒子探头、积冰探测仪和云粒子成像仪等仪器在中国华中和华东区域开展了探测.本文利用7个架次的综合观测数据,统计分析了层状冷云中小云粒子(直径小于50μm)数浓度(Nc)、球形粒子占比和飞机积冰的相关性.然后,提出了云粒子数浓度结合温度识别过冷水区的方法,并利用积冰探测仪和云粒子成像仪观测结果,使用TS(Threat Score)和TSS(True Skill Statistic)对该方法的可靠性进行了评估.七次飞行大量的空中观测表明,在0~-18℃之间,Nc,积冰概率和球形粒子占比之间有较好的相关性.当Nc大于一定阈值(5~20cm-3)时积冰概率和球形粒子占比均较高.因此,在温度低于0℃时,Ne= 5 cm-3可作为识别过冷水的最低标准.选取的Nc 阈值越大,积冰概率和球形粒子占比也越大,方法对过冷水识别的命中率越高,同时过冷水的含量也越高.本文所提出的方法,对于在飞机仅配备Ne探头而没有搭载CPI和RICE情况下的过冷水识别具有重要作用.

Identifying supercooled liquid water(SLW)in clouds is critical for weather modification,aviation safety,and at-mospheric radiation calculations.Currently,aircraft identification in the SLW area mostly depends on empirical es-timation of cloud particle number concentration(Nc)in China,and scientific verification and quantitative identifica-tion criteria are urgently needed.In this study,the observations are from the Fast Cloud Droplets Probe,Rosemount ice detector(RICE),and Cloud Particle Imager(CPI)onboard a King Air aircraft during seven flights in 2018 and 2019 over central and eastern China.Based on this,the correlation among Nc,the proportion of spherical particles(Ps),and the probability of icing(Pi)in supercooled stratiform and cumulus-stratus clouds is statistically analyzed.Subsequently,this study proposes a method to identify SLW areas using Nc in combination with ambient temperat-ure.The reliability of this method is evaluated through the true skill statistics(TSS)and threat score(TS)methods.Numerous airborne observations during the seven flights reveal a strong correlation among Nc,Ps,and Pi at the temperature from 0 to-18℃.When Nc is greater than a certain threshold of 5 cm-3,there is always the SLW,i.e.,Pi and Ps are high.Evaluation results demonstrate that the TSS and TS values for Nc =5 cm-3 are higher than those for Nc<5 cm-3,and a larger Nc threshold(>5 cm-3)corresponds to a higher SLW iden-tification hit rate and a higher SLW content.Therefore,Nc = 5 cm-3 can be used as the minimum criterion for identi-fying the SLW in clouds at temperature lower than 0℃.The SLW identification method proposed in this study is es-pecially helpful in common situations where aircraft are equipped with only Nc probes and without the CPI and RICE.

周毓荃;宋灿;蔡淼;刘思瑶;高扬;张荣

中国气象科学研究院,中国气象局云雾物理环境重点开放实验室,北京,100081河南省人工影响天气中心,郑州,450000北京师范大学全球变化地球系统科学研究院,北京,100875

积冰概率;云粒子形状;云粒子数浓度;过冷水

supercooled liquid water(SLW);icing probability;cloud particle shape;cloud particle number concen-tration

《气象学报(英文版)》 2022 (004)

1-33 / 33

Supported by the National Key Research and Development Program of China(2016YFA0601701),Fengyun Application Pioneering Project(FY-APP-2021.0102),and National High Technology Research and Development Program of China(2012AA120902).

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