. College of Water Resources and Architectural Engineering, Northwest A&F University, Yangling 712100, China . Key Laboratory of Agricultural Soil and Water Engineering in Arid Area of Ministry of Education, Northwest A&F University, Yangling 712100, China . Faculty of Geo-Information Science and Earth Observation, University of Twente, Enschede 7522 NH, the Netherlands . College of Soil and Water Conservation Science and Engineering, Northwest A&F University, Yangling 712100, China
Different canopy resistance (rc) parameterization has been used in land surface models to simulate actual evapotranspiration (ETc) and soil hydraulic variable for crop fields. However, the influence of rc parameterization on evapotranspiration (ET) partitioning and soil water dynamics has not been fully investigated with consideration of the coupled soil water and vapor physics. This study investigated the influential mechanisms of five rc methods (viz., Jarvis, Katerji-Perrier, Massman, Kelliher-Leuning, and Farias) on ET partitioning and soil water contents in an irrigated maize field under a semiarid climate through a soil water and vapor transfer model. The Jarvis method presented the best ET results (R2 = 0.86 and RMSE = 0.71 mm·d–1). Different rc parameterization mainly altered the simulated amount of soil water contents, while not changed the response of soil water dynamics to irrigation events. By the integrated analysis of the ET partitioning and root-zone water budget, different rc methods varied in the choice of the optimum irrigation water use strategies. This study identified the direct and indirect impacts of rc on the ET partitioning and emphasizes the necessity of both the ET partitioning and water supply sources in the decision-making for irrigation water management in semiarid regions.
Just Accepted Date: 30 August 2024Online First Date: 14 October 2024Issue Date: 12 November 2024
Cite this article:
Lianyu YU,Huanjie CAI,Delan ZHU, et al. Effects of canopy resistance parameterization on evapotranspiration partitioning and soil water contents in a maize field under a semiarid climate[J]. Front. Agr. Sci. Eng. ,
2024, 11(4): 544-560.
Fig.1 The experimental site and lysimeter: (a) summer maize growing in the filed with a rainproof shelter, (b) summer maize growing in the lysimeter, and (c) the structure of the lysimeter.
Crop growth stage
Date
Crop height (m)
LAI (m2·m–2)
Irrigation amount (mm)
Initial
Start
23 Jun.
0
0
Irrigation
26 Jun.
12.3
2 Jul.
8.97
Crop development
Start
6 Jul.
0.22
0.47
Irrigation
13 Jul.
51.2
22 Jul.
4.13
2 Aug.
58.8
Middle season
Start
14 Aug.
1.65
5.24
Irrigation
16 Aug.
67.5
9 Sep.
53.1
Late season
Start
14 Sep.
2.17
4.94
Harvest
2 Oct.
2.17
2.30
Tab.1 Crop growth stages and crop height for maize in 2013
Fig.2 Schematic of the STEMMUS-ET model with different canopy resistance parameterization. Blue module, i.e., root water uptake module, which used the potential transpiration as the input, and the actual transpiration and root water uptake sink term was calculated as the output. Gray module, i.e., soil water/vapor transport module, in which, soil water and vapor transfer among the topsoil, root-zone soil and bottom soil layers followed the Richards equation. Topsoil water is crucial in estimating actual soil evaporation. Bottom soil water was important in the calculation of the deep drainage water flux. Root-zone soil water was utilized to calculated the actual transpiration, which connects with the root water uptake module. Rns, net solar radiation; LAI, leaf area index; G, soil ground heat flux; VPD, vapor pressure deficit; ra, aerodynamic resisitance.
Models
Statistics
Soil moisture (m3·m–3)
20 cm
40 cm
60 cm
80 cm
100 cm
JA
BIAS
–0.0077
–0.0110
–0.0186
–0.0083
–0.0031
d
0.799
0.541
0.478
0.527
0.444
RMSE
0.0151
0.0207
0.0206
0.0115
0.0116
KP
BIAS
–0.0055
–0.0083
–0.0160
–0.0059
–0.0020
d
0.827
0.566
0.549
0.666
0.482
RMSE
0.0139
0.0195
0.0179
0.0093
0.0111
MA
BIAS
–0.0001
–0.0015
–0.0091
0.0011
0.0022
d
0.691
0.216
0.394
0.552
0.580
RMSE
0.0174
0.0235
0.0158
0.0077
0.0069
KL
BIAS
0.0076
0.0079
0.0001
0.0099
0.0055
d
0.567
0.0667
0.148
0.356
0.519
RMSE
0.0219
0.0288
0.0169
0.0148
0.0071
FA
BIAS
–0.0076
–0.0109
–0.0184
–0.0081
–0.0028
d
0.787
0.516
0.474
0.539
0.463
RMSE
0.0155
0.0212
0.0206
0.0111
0.0110
Tab.2 Comparative statistics values of models with different canopy resistance parameterization for soil moisture in 2013
Fig.3 Time series of measured and model simulated hourly soil water contents at different depths using the Jarvis (JA), Katerji-Perrier (KP), Massman (MA), Kelliher-Leuning (KL), and Farias (FA) canopy resistance methods.
Fig.4 Daily variation in and the correlation relationship between observed evapotranspiration (ET) and simulated ET, based on the (a) and (b) Jarvis (JA), (c) and (d) Katerji-Perrier (KP), (e) and (f) Massman (MA), (g) and (h) Kelliher-Leuning (KL), (i) and (j) Farias (FA) methods. I, irrigation.
Fig.5 Time series of (a) the observed and simulated daily soil evaporation (E), and (b) the cumulative errors (), using the Jarvis (JA), Katerji-Perrier (KP), Massman (MA), Kelliher-Leuning (KL), and Farias (FA) canopy resistance methods. I, irrigation.
Crop stage
Initial
Crop development
Middle season
Late season
All
Observed
ETc (mm)
37.5
141
125
31.2
335
JA
E (mm)
29.0
28.6
22.6
8.71
89.0
Tr (mm)
5.21
94.5
108
27.0
235
ET (mm)
34.2
123
131
35.7
324
EF (%)
84.8
23.3
17.3
24.4
27.5
KP
E (mm)
28.9
30.3
23.1
8.61
90.9
Tr (mm)
4.84
71.2
105
28.4
210
ET (mm)
33.8
102
124
37.0
296
EF (%)
85.7
29.8
18.6
23.3
30.7
MA
E (mm)
28.4
29.8
26.0
10.3
94.6
Tr (mm)
7.58
71.4
69.6
25.2
174
ET (mm)
36.0
101
95.6
35.5
268
EF (%)
78.9
29.5
27.2
29.1
35.3
KL
E (mm)
29.4
31.9
28.1
11.8
101
Tr (mm)
2.30
57.7
53.5
20.3
134
ET (mm)
31.7
89.6
81.6
32.0
235
EF (%)
92.8
35.6
34.4
36.7
43.1
FA
E (mm)
28.3
28.3
23.1
8.63
88.3
Tr (mm)
8.28
92.5
100
29.8
231
ET (mm)
36.6
121
123
38.4
319
EF (%)
77.4
23.4
18.8
22.5
27.7
Tab.3 The actual evapotranspiration (ETc), and model simulated soil evaporation (E), transpiration (Tr), evapotranspiration (ET), and evaporation fraction (EF) for each development stage of maize using the Jarvis (JA), Katerji-Perrier (KP), Massman (MA), Kelliher-Leuning (KL), and Farias (FA) canopy resistance methods
Fig.6 Model estimated water budget components for the root zone, using the Jarvis (JA), Katerji-Perrier (KP), Massman (MA), Kelliher-Leuning (KL), and Farias (FA) canopy resistance methods. qbot, bottom water flux; ΔV, change of soil water storage; I, irrigation; E, soil evaporation; and Tr, crop transpiration.
Fig.7 Integrated irrigation water use efficiency (IUE) index estimated using the model with the Jarvis (JA), Katerji-Perrier (KP), Massman (MA), Kelliher-Leuning (KL), and Farias (FA) canopy resistance methods.
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