Ground evaporation formula (Water Overlay): Difference between revisions

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Underground evaporation is calculated per cell.
Underground evaporation is calculated per cell.


For all underground evaporation, the height of the unsaturated zone is used.
For all underground evaporation calculation, the ground water depth at time t is used.
: ''H<sub>unsat</sub> = H<sub>surface</sub> - WL<sub>underground</sub>''
<math>d_{gw,t} = b_{s} - w_{g,t}</math>


First the capacity for saturated evaporation is calculated, based on how much of the saturated area is in contact with the roots.
Feddes oxygen stress factor:
: ''C<sub>sat</sub> = max( 0 , min( RD , GBDM ) - H<sub>unsat</sub> ) * WSP''
<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>


Next the height of the unsaturated zone, and based on that the capacity for unsaturated evaporation is calculated.
Feddes saturated zone root update factor:
: ''C<sub>unsat</sub> = max( 0 , min( RD , H<sub>unsat</sub> ) ) * ( W<sub>unsat</sub> / H<sub>unsat</sub> )''
<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>


Finally, the actual evaporation is calculated:
Max potential evaporation:
: ''Δw<sub>unsat</sub> = min( C<sub>unsat</sub> , Δt * E<sub>weather</sub> * E<sub>top</sub> )''
<math>E_{max} = f_t \cdot E_w \cdot f_o</math>
: ''Δw<sub>sat</sub> = min( C<sub>sat</sub> , (Δt * E<sub>weather</sub> * E<sub>top</sub>) - Δw<sub>unsat</sub> )''
: ''Δw = Δw<sub>unsat</sub> + Δw<sub>sat</sub>''


Where:
Evaporation unsaturated:
* Δw = The total amount of evaporation which takes place.
<math>E_{u} =  
* Δt = Computational timestep.
\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>


* Δw<sub>unsat</sub> = The amount of evaporation which takes place from the unsaturated zone.
Evaporation saturated:
* Δw<sub>sat</sub> = The amount of evaporation which takes place from the saturated zone.
<math>h_{s} = w_{g,t} - ( b_{s} - d_{gb} )</math>
* C<sub>sat</sub> = The amount of evaporation that can take place from the saturated zone.
<math>h_{r} = max( 0.0 ,  w_{g,t} - ( b_{s} - d_{r,1} ))</math>
* C<sub>unsat</sub> = The amount of evaporation that can take place from the unsaturated zone.
<math>E_{sp} = (E_{max} - E_{u}) \cdot f_s</math>
* H<sub>unsat</sub> = The height (column) of the unsaturated zone.
<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.


* W<sub>unsat</sub> = The amount of water in the saturated zone. The height of the water column if the equivalent amount of water was placed on the surface.
* WL<sub>underground</sub> = The [[Groundwater level formula (Water Overlay)|groundwater level]], relative to {{datum}}.
* H<sub>surface</sub> = The [[Terrain height (Water Overlay)|terrain height]] in the cell, relative to {{datum}}.
* RD = The [[Root depth m (Water Overlay)|ROOT_DEPTH_M]] of the construction if present, the [[Terrain root depth m (Water Overlay)|ROOT_DEPTH_M]] of the surface terrain otherwise.
* GBDM = The [[Ground bottom distance m model attribute (Water Overlay)|GROUND_BOTTOM_DISTANCE_M]] of the Water Overlay. (effectively available height in the underground).
* E<sub>weather</sub> = The [[Evaporation_m_(Water_Overlay)|evaporation rate]] of the [[weather]].
* E<sub>top</sub> = The [[Water evaporation factor (Water Overlay)|WATER_EVAPORATION_FACTOR]] of the building (construction, plant) if present, the [[Terrain water evaporation factor (Water Overlay)|WATER_EVAPORATION_FACTOR]] of the surface terrain otherwise.


==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