CAJ | 학술논문

该文综合分析了4次层状冷云人工增雨过程的雷达回波、粒子测量系统(PMS)探测资料，以及GPS定位资料，提出应以PMS的FSSP-100探头探测的云中粒子浓度以及2D-C探头探测的云中大粒子浓度作为判别云中可播性的主要技术参量，并发展了层状冷云飞机人工增雨实时监测指挥技术。FSSP-100探测的粒子浓度不小于20/cm3的云区才具有一定的可播性。其中2D-C探测的大粒子浓度小于20/L时，可确定为强可播区，否则为可播区。
해문종합분석료4차층상랭운인공증우과정적뢰체회파、입자측량계통(PMS)탐측자료，이급GPS정위자료，제출응이PMS적FSSP-100탐두탐측적운중입자농도이급2D-C탐두탐측적운중대입자농도작위판별운중가파성적주요기술삼량，병발전료층상랭운비궤인공증우실시감측지휘기술。FSSP-100탐측적입자농도불소우20/cm3적운구재구유일정적가파성。기중2D-C탐측적대입자농도소우20/L시，가학정위강가파구，부칙위가파구。
Based on integrated analysis of the cloud data obtained by digital radar,the particle measuring system (PMS) and the global positioning system (GPS), the main cloud physical parameters used to identify cloud seedability are proposed. Only when the relevant cloud particle concentration obtained by FSSP-100 probe of PMS is larger than 20/cm3, has the cloud area certain seedability. Furthermore, when the particle concentration obtained by 2D-C probe of PMS is less than 20/L, the cloud is highly seedable and otherwise it is seedable.