hydrus的T_Level文件解释

hydrus的T_Level一共有21个变量,其具体的解释说明在help中已进行了解释和说明。这里把它们

一一对应起来方便查找。

         help含义 序号 变量名 manul 单位
          Time Time [T]
 Potential upper boundary flux (precipitation, irrigation, or potential evaporation) 1 rTop Potential Surface Flux [L/T]
 Potential root water uptake rate 2 rRoot Potential Root Water Uptake [L/T]
 Actual upper boundary flux (infiltration or actual evaporation rate) 3 vTop Actual Surface Flux [L/T] 关心 实际表面通量
 Actual root water uptake rate 4 vRoot Actual Root Water Uptake [L/T] 关心 实际根系水速率
 Lower boundary flux 5 vBot Bottom Flux [L/T] 关心 底部通量
 Cumulative potential upper boundary flux 6 sum_rTop Cum. Potential Surface Flux  [L]
 Cumulative potential root water uptake rate 7 sum_rRoot Cum. Potential Root Water Uptake  [L]
 Cumulative actual upper boundary flux 8 sum_vTop Cum. Actual Surface Flux  [L] 关心 累积实际表面通量
 Cumulative actual root water uptake rate 9 sum_vRoot Cum. Actual Root Water Uptake  [L] 关心 累积实际根吸水量
 Cumulative lower boundary flux 10 sum_vBot Cum. Bottom Flux  [L] 关心 累积底部通量
 Soil surface pressure head 11 hTop Surface Pressure Head  [L]
 Average root zone pressure head 12 hRoot Root Zone Pressure Head  [L]
 Lower boundary pressure head 13 hBot Bottom Pressure Head  [L]
All fluxes All Fluxes
All cumulative fluxes All Cumulative Fluxes
All pressure heads All Pressure Head
Surface runoff 14 RunOff Surface Run-Off [L/T]
15 sum_RunOff Cum. Surface Run-Off  [L]
Soil water storage 16 Volume Soil Water Storage  [L] 关心 土壤蓄水量
Cumulative infiltration 17 sum_Infil Cum. Infiltration  [L] 关心 累积入渗量
Cumulative evaporation 18 sum_Evap Cum. Evaporation  [L] 关心 累积蒸发量
19 Tlevel
Cumulative non-equilibrium water transfer (in dual-porosity models) 20 Cum_Wtrans Cum. Non-Equil. Water Transfer
Snow Layer 21 SnowLayer Snow Layer

其中这些变量之间还有一些内部平衡的关系:

累积表面通量=累积蒸发量-累积入渗量
累积底部通量=累积蒸发量+累积实际根吸水量-累积入渗量-储水量减少量
累积底部通量=ET-累积入渗量-储水量减少量
累积底部通量=累积表面通量+累积实际根吸水量-储水量减少量

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