低的暖云比高的冷云发射更多的热能。
Low, warm clouds emit more thermal energy than high, cold clouds.
为了研究层状冷云自然降水和人工降水的机制建立了一维非定常的数值模式。
An one-dimensional time dependent numerical model has been developed to study the mechanism of natural and artificial precipitation from the cold layer clouds.
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。
Macro and micro physics conditions of supercooled fog dissipation operation using liquid Nitrogen with that of the cold cloud seeding are compared.
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