宏观地面气温场气候学方程

宏观地面气温场气候学方程

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contributed at 2018-12-04

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Affiliation:  
岳天祥编著
Email:  
yue@lreis.ac.cn
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Classification(s)

Geography SubjectPhysical GeographyClimatology
Earth System SubjectEarth Surface SystemAtmosphere

Detailed Description

宏观地面气温场气候学方程

 

对平坦地区来说,一地的温度T是地理纬度(y),经度(l)和高度(h)的函数,可写为,也可以简单的表达为多元一次回归方程:

式中,a0a1a2a3为系数;y(N°)为纬度;l(E°)为经度;h(100m)为高度。

对于山区来说由于受地形影响,需要引入地形温度订正项(Tg),温度场的气候学方程可改写为:

在一阶回归方程中可写为:

式中,引入Tg的气候学方程,为代表山地的实际温度。

 

参考文献

王菱:华北山区温度推算模式和应用。自然资源学报,1996,11(2)

 

How to cite

《资源环境数学模型手册》 (2018). 宏观地面气温场气候学方程, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/df04c44b-b3d0-4750-b3ea-64ebc42d42f7
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Contributor

contributed at 2018-12-04

Authorship

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

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