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a Dep. of Renewable Resour., Univ. of Alberta, Edmonton, AB, Canada T6G 2H1
b USDA-ARS, U.S. Water Conserv. Lab., 4331 E. Broadway, Phoenix, AZ 85040
c Lab. of Tree-Ring Res., Tucson, AZ 85721
d Dep. of Soil, Water, and Environ. Sci., Univ. of Arizona, Tucson, AZ 85721
e Maricopa Agric. Cent., Univ. of Arizona, Maricopa, AZ 85239
f Dep. of Geogr., Arizona State Univ., Tempe, AZ 85287
* Corresponding author (robert.grant{at}ualberta.ca)
Received for publication November 28, 2004.
Elevated concentrations of atmospheric CO2 (Ca) are believed to raise sorghum [Sorghum bicolor (L.) Moench] productivity by improving water relations. In ecosys, water relations are simulated by solving for the canopy water potential (
C) at which water uptake from a model of soilrootcanopy water transfer equilibrates with transpiration from the canopy energy balance. Simulated water relations were tested with
C, water uptake, and energy exchange measured under ambient (363 µmol mol1) and elevated (566 µmol mol1) Ca and high vs. low irrigation in a free air CO2 enrichment experiment during 1998 and 1999. Model results, corroborated by field measurements, showed that elevated Ca raised
C and lowered latent heat fluxes under high irrigation and delayed water stress under low irrigation. Changes in
C modeled under ambient vs. elevated Ca varied diurnally, with lower
C causing earlier midafternoon stomatal closure under ambient Ca. Modeled changes in sorghum water status caused elevated Ca to raise seasonal water efficiency under high and low irrigation by 20 and 26% (vs. 20 and 13% measured) in 1998 and by 9 and 27% (vs. 6 and 26% measured) in 1999. Ecosys was used to generate an irrigation response function for sorghum yield, which indicated that yields would rise by
13% for a range of irrigation rates if air temperatures were to rise by 3°C and Ca by 50%. Current high sorghum yields could be achieved with
120 mm or
20% less irrigation water if these rises in temperature and Ca were to occur.
Abbreviations: Ca, atmospheric CO2 Ci, intercellular CO2 concentration DOY, day of year FACE, free air CO2 enrichment (experiment) gC, stomatal conductance GCM, general circulation model gL, leaf conductance H, sensible heat IRTs, infrared thermometers LE, latent heat Rn, net radiation TC, canopy temperature VPD, vapor pressure deficit WUE, water use efficiency
C, canopy water potential
S, soil water potential
T, canopy turgor potential 
, osmotic potential
R, rootcanopy hydraulic resistances
S, soilroot hydraulic resistances
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