This document discusses various methods for calculating actual evaporation from land and vegetation. It introduces concepts like pan evaporation, reference evapotranspiration, and actual evapotranspiration. Methods covered include long-term water balance, Budyko curves, soil moisture functions, complementary relationship approaches, and turbulent transfer models like Penman-Monteith. Measurement techniques involve lysimeters and remote sensing of factors like leaf area index and fractional canopy coverage.
1. 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. 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
18. 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
19. Methods of Calculating Actual Evaporation
19
3. Use of soil moisture functions
)( relfPEAE
pwpfc
pwp
rel
Input: PE,
Application: Monthly, daily or hourly
20. 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
23. 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. 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