The microphysical characteristics of high supercooled water area in stratiform cloud of autumn .

秋季层状云中高值过冷水区的微物理特征。

Even after the negative charge had worn off , the water remained in supercooled liquid form .

甚至有时当负电荷消耗殆尽，水仍能保持它低于常温的液体状态。

Snow crystals form when tiny supercooled cloud droplets freeze .

雪花晶体是极小的超冷云滴结冰时形成的。

Similarly , water 's freezing point is negotiable , with " supercooled " water able to remain liquid down to around 40 degrees , and even colder at extreme pressures .

同样，水的凝固冰点也是可变的，那些“过冷”的水可以在零下40度时保持液态，并在极度压力作用下变得更冷。

By using the particles measuring system ( pms ) via 23 sortie flying the cloud structure in autumn precipitating clouds was sampled from 1989 to 2008 in shandong province . The distribution of supercooled water and ice crystal concentration within the clouds is analyzed .

利用山东省19892008年23架次秋季降水云系云结构的粒子测量系统（pms）探测试验资料，分析了云中过冷水以及冰晶浓度的分布特征。