原始的热模型

原始的热模型

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Initial contribute: 2018-12-04

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岳天祥编著
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yue@lreis.ac.cn
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Method-focused categoriesData-perspectiveRemote sensing analysis
Method-focused categoriesProcess-perspectiveBiological process calculation

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原始的热模型

(1) 植被冠层的能量平衡方程的矩阵为:

式中,X是三层植被层的层平均温度;是长波吸收项矢量;Stefan-Boltzmann常数;B是长波发射项矢量;是短波吸收项矢量;是显热矢量;是蒸散量矢量。

(2) 在方向,冠层分层中的间隙概率为:

式中,是叶面积指数,即为每单位地面面积的单面叶面积;K是在方向上的平均冠层投影;是底角。

(3) 当考虑到路径长度对底角及方位角的变化,间隙概率表示为:

式中,是叶片密度;是在角度穿过冠层的累积距离。

 

参考文献:

McGuire M J, Smith JA, Balick L K et al::森林冠层的直接热辐射模型。Remote Sensing of Environment198927

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《资源环境数学模型手册》 (2018). 原始的热模型, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/98d92436-7acd-4309-ba09-9d9fda24b1bf
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Initial contribute : 2018-12-04

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Authorship

:  
岳天祥编著
:  
yue@lreis.ac.cn
:  
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