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Methods of Calculating Actual Evaporation
实际蒸散发的计算方法
水文学原理
李红 (挪威奥斯陆大学)
lihong2291@gmail.com
2
Concepts
Epan (pan evaporation) is the evaporation measured
by a evaporation pan.
ETp (reference crop evapotranspiration or reference
evapotranspiration, or potential evapotranspiration) is
the evapotranspiration rate from a reference surface,
not short of water. PE
ETa (actual evapotranspiration) describes all the
processes by which liquid water at or near the land
surface becomes atmospheric water vapour under
natural condition. AE
3
Controlling factors
4
Controlling factors
Water
- Amount, depth, temperature, quality, …
Energy
- Solar radiation, net radiation, temperature, ...
 Dynamics
- Vapour pressure, wind speed, humidity, …
5
1. Lysimeter
2. Remote sensing (?)
Measurement
6
Input: Rainfall and Additional water
Output: Percolated water PE = R + A – P
R A
P
Measurement: Lysimeter
7
Input: Rainfall and Additional water
Output: Percolated water
R
P
Measurement: Lysimeter
8
Input: Rainfall and Additional water
Output: Percolated water AE = R – P – ΔS
R
P
Measurement: Lysimeter
9
Measurement: Remote Sensing
10
Measurement: Remote Sensing
PE
AE













 )( cc
k
ff
LAI
LAI
w
w
11,min
max

W: water content in soil, Wk: water capacity
LAI: leaf area index, LAImax: maximum LAI of the whole year,
fc: the fractional canopy coverage.
11
Methods of Calculating Actual Evaporation
12
– In arid case, P <<PE, water limited
AE = P
– In humid case, P >>PE
AE = PE, energy limited
Methods of Calculating Actual Evaporation
13
1 . Long-term water balance
2. Budyko types
3. Use of soil moisture functions
4. Complementary relationship approach
5. Turbulent-transfer/energy-balance methods
Methods of Calculating Actual Evaporation
14
1. Long-term water balance method
AE = P – Q
Input: P, Q
Application: Annual or longer time steps
Methods of Calculating Actual Evaporation
15
AE = P – Q – ΔS
Input: P, Q
Methods of Calculating Actual Evaporation
16
AE = P – Q – ΔS
Input: P, Q
Methods of Calculating Actual Evaporation
http://www.nasa.gov/mission_pages/Grace/index.html
Methods of Calculating Actual Evaporation
17
2. Budyko types
Methods of Calculating Actual Evaporation
18













P
PE
PAE exp1







PE
P
PEAE tanh
 2
1
PE
P
P
AE


2. Budyko types
Input: P, PE
Application: Annual or longer
Methods of Calculating Actual Evaporation
19
3. Use of soil moisture functions
)( relfPEAE 
pwpfc
pwp
rel






Input: PE,
Application: Monthly, daily or hourly

20







 1,
LPFC
minPA

EE
Soil moisture (mm)
0
1
act.evaporation/pot.evaporation
FCFC * LP
AE/PE

Methods of Calculating Actual Evaporation
3. Use of soil moisture functions
)( relfPEAE 
pwpfc
pwp
rel






21
Methods of Calculating Actual Evaporation
3. Use of soil moisture functions
)( relf 
22
Methods of Calculating Actual Evaporation
3. Use of soil moisture functions
AE/PE
rel
Increase of wetness
evapotranspiration
Based on heuristic arguments of Bouchet (1963)
AE + PE = 2 ETw
23
Methods of Calculating Actual Evaporation
4. Complementary relationship approach
24
CRAE (Morton, 1983)
Advection-aridity (AA) (Brutsaert and Stricker, 1979)
GG (Granger and Gray, 1989)
Methods of Calculating Actual Evaporation
4. Complementary relationship approach
AE = 2 ETw - PE
5. Turbulent-transfer/energy-balance methods
25
Methods of Calculating Actual Evaporation
FAO: http://www.fao.org/docrep/X0490E/x0490e00.htm
Penman-Monteith equation
5. Turbulent-transfer/energy-balance methods
26
Methods of Calculating Actual Evaporation
FAO: http://www.fao.org/docrep/X0490E/x0490e00.htm
Penman-Monteith equation

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