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USDA-ARS, Conservation and Production Research Lab., P.O. Drawer 10, Bushland, TX 79012
* Corresponding author (jtolk{at}cprl.ars.usda.gov)
Received for publication September 30, 2005. Nighttime evapotranspiration (ETN) has typically been neglected in estimating water loss from land surfaces. Our objective was to quantify the contribution of ETN to daily (24-h) ET (ET24) of irrigated and dryland cotton (Gossypium hirsutum L.) and irrigated alfalfa (Medicago sativa L.) grown in a semiarid climate. The results were then examined using a PenmanMonteith ET model which separates control of ET into its radiation (equilibrium) and atmospheric demand (imposed) components. Nighttime ET was measured at Bushland, TX using weighing lysimeters containing monolithic soil cores of Pullman clay loam (fine, mixed, superactive thermic Torrertic Paleustoll) for alfalfa in 1998 and cotton in 2001. Measured ratios of ETN to ET24 ranged from an average of 3% for a dryland cotton crop to 7.2% for irrigated alfalfa over a season. In the largest events, ETN was as much as 12% of ET24 with single nighttime losses approaching 2 mm. Model calculations showed that virtually all ETN was the result of imposed atmospheric conditions, primarily vapor pressure deficit. However, ETN was also related to sensible heat transfer to the canopy. Nighttime ET can be an important part of total ET of irrigated crops in a semiarid environment.
Abbreviations: DOY, day of year ET, evapotranspiration ETeq, equilibrium ET ETimp, imposed ET ETN, nighttime ET ET24, daily (24-h) ET G, soil heat flux H, sensible heat flux IRT, infrared thermometer LAI, leaf area index
E, latent heat flux (Rn + G), net radiation + soil heat flux
, decoupling factor ra, aerodynamic resistance rs, surface resistance VPD, vapor pressure deficit
This article has been cited by other articles:
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J. A. Tolk, S. R. Evett, and T. A. Howell Advection Influences on Evapotranspiration of Alfalfa in a Semiarid Climate Agron. J., October 31, 2006; 98(6): 1646 - 1654. [Abstract] [Full Text] [PDF] |
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