摘要
用液滴催化暖云降水,达到“以小得大”的降水目的,结果指出:液滴催化暖云降水的最佳播撒高度和最佳播撒效率受到云中垂直气流速度(ω),云含水量(Q),云滴半径(r)和云层厚度(ΔH)的制约。
In the paper, The result indicates that the optimum seeding height and the optimum seeding efficiency of liquid droplet seeding precipitation in warm cloud is restricted by vertical velocity of the air (w), Water content of the clouds (Q), radius of thd clouds drops (r), and thickness of the clouds (ΔH).
出处
《热带气象学报》
CSCD
1994年第3期266-273,共8页
Journal of Tropical Meteorology