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作 者:范思睿[1,2,3] 王维佳 王博为[3] 刘贵华 孙方林 张丰伟 张征东 FAN Sirui;WANG Weijia;WANG Bowei;LIU Cuihua;SUN Fanglin;ZHANG Fengwei;ZHANG Zhengdong(Weather Modification Office of Sichuan Province,Chengdu 610072,China;CMA Cloud-Precipitation Physics and Weather Modification Key Laboratory,Beijing 100081,China;Sichuan Meteorological Bureau,Chengdu 610072,China;Meteorological Institute of Shanxi Province,Xi'an 710016,China;Northwest Institute of Eco-Environment and Resources,CAS,Lanzhou 73000,China;AVIC(Chengdu)UAS Co.,Ltd.,Chengdu 611743,China)
机构地区:[1]四川省人工影响天气办公室,四川成都610072 [2]中国气象局云降水物理与人工影响天气重点开放实验室,北京100081 [3]四川省气象局,四川成都610072 [4]陕西省气象科学研究所,陕西西安710016 [5]中国科学院西北生态环境资源研究院,甘肃兰州730000 [6]中航(成都)无人机系统股份有限公司,四川成都611743
出 处:《成都信息工程大学学报》2025年第2期220-225,共6页Journal of Chengdu University of Information Technology
基 金:四川省科技计划资助项目(2019YJ0621);中国气象局创新发展专项资助项目(CXFZ2024J035)。
摘 要:为验证大型无人机在高原地区进行人工影响天气作业和飞行观测的可行性,也为研究高原地区的云降水特征和人工增雪作业效果,2022年四川省人工影响天气办公室联合中航(成都)无人机系统股份有限公司在青藏高原东侧(川西高原)开展多个架次人工增雪试验,并利用卫星资料和常规气象观测资料对2022年2月11-12日在青藏高原东侧开展的2架次人工增雪试验进行分析。结果表明:2022年2月青藏高原东侧人工增雪试验目标云的云底温度低于-10℃,云底粒子半径较大,云底粒子有效半径为31μm,云顶粒子有效半径为15~20μm。无降水云和降水云的云顶均发生冰晶化,在云顶存在冰晶粒子递减带,无降水云的冰晶化高度低于降水云,无降水云的冰化高度为-22℃,降水云的冰化高度为-29℃。In 2022,Weather Modification Office of Sichuan Province and AVIC(Chengdu)UAS Co.,Ltd.carried out several flights of artificial snow enhancement experiments on the eastern side of the Tibet Plateau,which has verified the feasibility of large-scale UAVs for artificial weather modification operation and flight observation on the Tibet Plateau,and has also provided a new effective way to study the characteristics of cloud precipitation and the effect of artificial snow enhancement on the Tibet Plateau.In this paper,two artificial snow enhancement experimental flights carried out on the eastern side of the Tibet Plateau on February 11-12,2022 were analyzed.Based on satellite data and routine meteorological observation data,the experimental flights were analyzed.The results show as following:On the eastern side of the Tibetan Plateau in February 2022,the temperature of the cloud bottom of the target clouds of the artificial snow enhancement experiment is lower than-10 C.The radius of cloud bottom particles is large,the effective radius of cloud bottom particles is 31μm,and the effective radius of cloud top particles are 15-20μm.Ice crystallization has occurred in the cloud tops of both non-precipitating and precipitating clouds.In the tops there are decreasing bands of ice crystal particles.The height of ice crystallization in non-precipitating clouds is lower than in precipitating clouds.The icing altitude is-22℃for non-precipitating clouds and-29℃for precipitating clouds.
分 类 号:P481[天文地球—大气科学及气象学]
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