Agronomy Journal Journal of Natural Resources and Life Sciences Education
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Published online 31 October 2006
Published in Agron J 98:1646-1654 (2006)
DOI: 10.2134/agronj2006.0031
© 2006 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
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Advection Influences on Evapotranspiration of Alfalfa in a Semiarid Climate

Judy A. Tolk*, Steven R. Evett and Terry A. Howell

USDA–Agricultural Research Service Conservation and Production Research Laboratory, P.O. Drawer 10, Bushland, TX 79012


Figure 1
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Fig. 1. Wind speed and wind direction analyses for the days included in the study.

 

Figure 2
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Fig. 2. Aerial view of the alfalfa field and surrounding landscape.

 

Figure 3
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Fig. 3. Layout of the lysimeter field.

 

Figure 4
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Fig. 4. The 20-yr average and 1998 Class A pan evaporation and precipitation for the cropping season.

 

Figure 5
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Fig. 5. (A) Daily evapotranspiration (ET), (B) average vapor pressure deficit (VPD), and (C) wind speed for the north and south lysimeters for the days used in the analyses.

 

Figure 6
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Fig. 6. Daily evapotranspiration (ET) partitioned into the equilibrium ET (ETeq) and imposed (ETimp) contributions as stacked bar graphs for the north and south lysimeters.

 

Figure 7
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Fig. 7. Changes in vapor pressure deficit (VPD) and wind, and partitioning between equilibrium evapotranspiration (ETeq) and imposed ET (ETimp) as stacked bar graphs on day of year (DOY) 155.

 

Figure 8
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Fig. 8. Changes in vapor pressure deficit (VPD) and wind, and partitioning between equilibrium evapotranspiration (ETeq) and imposed ET (ETimp) as stacked bar graphs on day of year (DOY) 164.

 

Figure 9
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Fig. 9. Partitioning of daily evapotranspiration (ET) into daytime losses (ETday) and nighttime losses due to ETimp only (ETimp-night).

 

Figure 10
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Fig. 10. Energy used in latent heat ({lambda}E) supplied by available energy (AE) and sensible heat (H) and equivalent evapotranspiration calculated using the latent heat of vaporization (2.45 MJ kg–1).

 

Figure 11
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Fig. 11. Energy balance fluxes on day of year (DOY) 155 and 164, including latent heat ({lambda}E), available energy (AE), and {lambda}E + sensible heat (H).

 

Figure 12
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Fig. 12. Difference between imposed evapotranspiration from the south lysimeter (ETimp-s) and the north lysimeter (ETimp-n) in relation to wind direction.

 

Figure 13
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Fig. 13. Wind speed and wind direction analyses for day of year 167.

 

Figure 14
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Fig. 14. Wind speed and wind direction analyses for day of year 151.

 

Figure 15
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Fig. 15. The relationships between wind speed and sensible heat flux (H), and vapor pressure deficit (VPD) and H.

 





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