洪延超. 1999: 冰雹形成机制和催化防雹机制研究. 气象学报, (1): 30-44. DOI: 10.11676/qxxb1999.003
引用本文: 洪延超. 1999: 冰雹形成机制和催化防雹机制研究. 气象学报, (1): 30-44. DOI: 10.11676/qxxb1999.003
Hong Yanchao. 1999: STUDY ON MECHANISM OF HAIL FORMATION AND HAIL SUPPRESSION WITH SEEDING. Acta Meteorologica Sinica, (1): 30-44. DOI: 10.11676/qxxb1999.003
Citation: Hong Yanchao. 1999: STUDY ON MECHANISM OF HAIL FORMATION AND HAIL SUPPRESSION WITH SEEDING. Acta Meteorologica Sinica, (1): 30-44. DOI: 10.11676/qxxb1999.003

冰雹形成机制和催化防雹机制研究

STUDY ON MECHANISM OF HAIL FORMATION AND HAIL SUPPRESSION WITH SEEDING

  • 摘要: 利用文献1发展的三维弹性冰雹云催化模式模拟研究了1997年7月8日陕西省旬邑防雹试验区出现的一块冰雹云,分析其冰雹形成的物理机制,对雹云做了高度催化试验,研究了催化防雹机制。结果表明,97%的雹块是以冻滴为核心增长的,在云中冰雹还未形成前,于强上升气流区的适当高度催化效果较好,而在上升气流极值高度,亦是高含水量区催化效果最好。催化使霰和冻滴的浓度增加,粒子质量减小,向雹的转化比例大为降低,因此雹块的质量和浓度都减小,达到了防雹的目的。

     

    Abstract: Using the 3-D hail cloud numerical model developed by author,a hail cloud occurred in Xunyi area,Shanxi province on July 8,1997 is simulated to analyze mechanismof hail formation and hail suppression with seeding.The results show that embryoes of 97% of hailare frozen drops.The seeding experiments with AgI for heig hts show that if the seeding is made before hail formation,the o ptimum seeding position is located in the maximumupdraft area and its center,i.e.,AgI is seeded in the zone with high water content to be coordinated with maximum zone of the updraft.The seeding make concentration of graupe land frozen drop increase and their average mass/size decrease, so that proportion of conversion from graupeland frozen drop into hail descend greatly and mass and concentration of hailstone are all decrease to achieve our purpose for hail suppression.

     

/

返回文章
返回