露水形成的最大速率及其形成总量的计算公式

露水形成的最大速率及其形成总量的计算公式

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Initial contribute: 2018-12-04

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Affiliation:  
岳天祥编著
Email:  
yue@lreis.ac.cn
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Application-focused categoriesNatural-perspectiveLand regions
Application-focused categoriesNatural-perspectiveAtmospheric regions

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Chinese {{currentDetailLanguage}} Chinese

露水形成的最大速率及其形成总量的计算公式

   1)露水形成的最大速率(Ep):

 

式中,s是饱和水蒸气压曲线在气温和露点之间区域的斜率的平均值;γ是湿度计常数;Rn是净辐射;λ是水分气化/凝结的潜热。

   2)露水形成的总量计算公式为:

      

式中,Y是日露水总量;A是气温的夜晚冷却率;B是相对湿度;C1.5m处风速;D是总的净辐射。

参考文献

    Jackson T JMoy L:露水对被动式地表微波观测的影响。Remote Sensing of Environment199970

How to Cite

《资源环境数学模型手册》 (2018). 露水形成的最大速率及其形成总量的计算公式, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/d8f6ed67-3049-4ff5-9cb8-903b19a60b23
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Last modifier : 
wu kai
Last modify time : 
2020-12-02
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Contributor

Initial contribute: 2018-12-04

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Authorship

Affiliation:  
岳天祥编著
Email:  
yue@lreis.ac.cn
Homepage:  
View
Is authorship not correct? Feedback

History

Last modifier : 
wu kai
Last modify time : 
2020-12-02
Modify times : 
View History

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