Ground evaporation formula (Water Overlay): Difference between revisions
No edit summary |
No edit summary |
||
Line 1: | Line 1: | ||
Underground evaporation is calculated per cell. | Underground evaporation is calculated per cell. | ||
For all underground evaporation, the | For all underground evaporation calculation, the ground water depth at time t is used. | ||
<math>d_{gw,t} = b_{s} - w_{g,t}</math> | |||
Feddes oxygen stress factor: | |||
<math>f_o = | |||
\begin{cases} | |||
1.0 & \text{if } d_{gw,t} \text{ is } >= d_{r,3}} \\ | |||
\frac{d_{gw,t} - d_{r,4}}{d_{r,3} - d_{r,4}} & \text{if } d_{gw,t} \text{ is } >= d_{r,4}} \\ | |||
0.0 & \text{otherwise} \\ | |||
\end{cases} | |||
</math> | |||
Feddes saturated zone root update factor: | |||
<math>f_s = | |||
\begin{cases} | |||
0.0 & \text{if } d_{gw,t} \text{ is } >= d_{r,1}} \\ | |||
1.0 - \frac{d_{gw,t} - d_{r,2}}{d_{r,1} - d_{r,2}} & \text{if } d_{gw,t} \text{ is } >= d_{r,2}} \\ | |||
1.0 & \text{otherwise} \\ | |||
\end{cases} | |||
</math> | |||
Max potential evaporation: | |||
<math>E_{max} = f_t \cdot E_w \cdot f_o</math> | |||
Evaporation unsaturated: | |||
<math>E_{u} = | |||
\begin{cases} | |||
0.0 & \text{if } d_{us} \text{ is } <= 0.0} \\ | |||
min(E_{max}, h_u \cdot \frac{d_{r,1}}{d_{gw,t}})& \text{otherwise} \\ | |||
\end{cases} | |||
</math> | |||
Evaporation saturated: | |||
<math>h_{s} = w_{g,t} - ( b_{s} - d_{gb} )</math> | |||
<math>h_{r} = max( 0.0 , w_{g,t} - ( b_{s} - d_{r,1} ))</math> | |||
<math>E_{sp} = (E_{max} - E_{u}) \cdot f_s</math> | |||
<math>E_{s} = max (0.0 , min ( E_{sp}, h_{s}\cdot f_{gw}, h_r \cdot f_{gw}</math> | |||
Evaporation total is the sum of evaporation in the saturated and unsaturated zone: | |||
<math>E = E_u + E_s</math> | |||
where | |||
: <math>b_{s}</math> is the datum height of the surface. | |||
: <math>w_{g}</math> is the underground water level. | |||
: <math>d</math> is the column height of the unsaturated zone. | |||
: <math>f_t</math> is the [[Water evaporation factor (Water Overlay)|transpiration factor]] of the buildings (plants) on the surface, or the surface terrain's | |||
[Terrain_water_evaporation_factor_(Water_Overlay)|transpiration factor]] if none present. | |||
: <math>E_{w,t}</math> is the [[Evaporation_m_(Water_Overlay)|evaporation rate]] of the [[weather]] at time t | |||
: <math>f_0</math> is the feddes oxygen stress factor, calculated using the 3rd and 4th [[root depths (Water Overlay)|root depths]] and the feddes trapezium interpolation model and the ground water depth. | |||
==Related== | ==Related== |
Revision as of 12:49, 25 February 2021
Underground evaporation is calculated per cell.
For all underground evaporation calculation, the ground water depth at time t is used.
Feddes oxygen stress factor: Failed to parse (unknown function "\begin{cases}"): {\displaystyle f_o = \begin{cases} 1.0 & \text{if } d_{gw,t} \text{ is } >= d_{r,3}} \\ \frac{d_{gw,t} - d_{r,4}}{d_{r,3} - d_{r,4}} & \text{if } d_{gw,t} \text{ is } >= d_{r,4}} \\ 0.0 & \text{otherwise} \\ \end{cases} }
Feddes saturated zone root update factor: Failed to parse (unknown function "\begin{cases}"): {\displaystyle f_s = \begin{cases} 0.0 & \text{if } d_{gw,t} \text{ is } >= d_{r,1}} \\ 1.0 - \frac{d_{gw,t} - d_{r,2}}{d_{r,1} - d_{r,2}} & \text{if } d_{gw,t} \text{ is } >= d_{r,2}} \\ 1.0 & \text{otherwise} \\ \end{cases} }
Max potential evaporation:
Evaporation unsaturated: Failed to parse (unknown function "\begin{cases}"): {\displaystyle E_{u} = \begin{cases} 0.0 & \text{if } d_{us} \text{ is } <= 0.0} \\ min(E_{max}, h_u \cdot \frac{d_{r,1}}{d_{gw,t}})& \text{otherwise} \\ \end{cases} }
Evaporation saturated:
Evaporation total is the sum of evaporation in the saturated and unsaturated zone:
where
- is the datum height of the surface.
- is the underground water level.
- is the column height of the unsaturated zone.
- is the transpiration factor of the buildings (plants) on the surface, or the surface terrain's
[Terrain_water_evaporation_factor_(Water_Overlay)|transpiration factor]] if none present.
- is the evaporation rate of the weather at time t
- is the feddes oxygen stress factor, calculated using the 3rd and 4th root depths and the feddes trapezium interpolation model and the ground water depth.
Related
The following topics are related to this formula.
- Formulas
- Groundwater level formula
- Models
- Underground model
- Evaporation model