摘要
对用液氮消过冷雾和冷云催化增雨作业的宏、微观条件进行比较 ,找出其异同点。并根据消冷雾作业所出现的物理响应推演冷云催化后应出现的结果 ,以弥补飞机云中催化后缺少直接观测资料的缺陷 ,进而对液氮 (LN)增雨效果进行探讨。
Macro and micro physics conditions of supercooled fog dissipation operation using liquid Nitrogen with that of the cold cloud seeding are compared. For filling a gap of data after seeding by airplane, physical responses is elicited after seeding in cold clouds based on those that occurred in fog dissipation operation and then the effect of enhancement precipitation is discussed.
出处
《气象》
CSCD
北大核心
2001年第7期20-23,共4页
Meteorological Monthly
关键词
消雾
液氮
冷云
增雨效果
LN
催化剂
fog dissipation enhancement precipitation revelation
