1) Condensation -function precipitation
凝结函数降水
2) condensation function
凝结函数
1.
The diagnose and calculation of synoptic large-scale condensation function precipitation and moisture flux divergence are conducted on the isentropic coordinates system with the re-analysis data of T213 L31 model atmosphere.
对T213 L31再分析模式大气,在等熵坐标系上对天气学大尺度凝结函数降水、水汽通量散度降水做了诊断计算;同时,对整层对流不稳定性降水和气块(团)湿不稳定降水做了理想设计与诊断计算。
3) collecting water by cooling and vapor condensation
降温凝结收水
4) possibility function of precipitation
降水可能函数
1.
In this paper,the forecast is transformed into a forecast of a continuous variable—possibility function of precipitation(PFP).
将逐时段定点降水非连续量的预报问题转化为对一个连续的降水可能函数的预报问题。
2.
As the forecast of precipitation is actually considered as the forecast of a discontinuous variable, the forecast is translated into the forecast of a continuous variable—possibility function of precipitation (PFP).
将逐时段定点降水预报这个以往一般作为非连续量处理的预报问题转化为对一个连续的降水可能函数的预报问题。
5) Eta-coordinate
水汽凝结参数
6) precipitation infiltration recharge function
降水入渗补给函数
补充资料：凝结
分子式：
CAS号：
性质：使气体或蒸气转变为液态或固态的过程。
CAS号：
性质：使气体或蒸气转变为液态或固态的过程。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条