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Modeling Interactions among Carbon Dioxide, Nitrogen, and Climate on Energy Exchange of Wheat in a Free Air Carbon Dioxide Experiment

Robert F. Granta, Bruce A. Kimballb, Talbot J. Brooksb, Gary W. Wallb, Paul J. Pinter, Jr.b, Doug J. Hunsakerb, Floyd J. Adamsenb, Robert L. Lamorteb, Steven W. Leavittc, Thomas L. Thompsond and Allan D. Matthiasd

a Dep. of Renewable Resources, Univ. of Alberta, Edmonton, AB, Canada T6G 2H1
b USDA-ARS, U.S. Water Conserv. Lab., 4331 E. Broadway, Phoenix, AZ 85040
c Laboratory of Tree Ring Res., Univ. of Arizona, Tucson, AZ
d Dep. of Soil, Water, and Environ. Sci., Univ. of Arizona, Tucson, AZ



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Fig. 1. Hourly averages of air temperature and wind speed from 6 to 10 Mar. 1996 (DOY 66–70) at the FACE site near Phoenix, AZ

 


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Fig. 8. Seasonal time course of (a) aboveground phytomass and (b) LAI measured (symbols) and simulated (lines) under 35 vs. 7 g N m-2 fertilization and 363 vs. 548 µmol mol-1 CO2 concentration

 


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Fig. 2. Hourly averages of net radiation (Rn), latent heat (LE), and sensible heat (S) fluxes measured (symbols ± SE) and simulated (lines) from 6 to 10 Mar. 1996 (DOY 66–70) under 363 µmol mol-1 CO2 and (a) 35 g N m-2 and (b) 7 g N m-2 fertilization. Negative values represent upward fluxes

 


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Fig. 3. Differences in latent and sensible heat fluxes under 548 vs. 363 µmol mol-1 CO2 with (a) 35 g N m-2 and (b) 7 g N m-2 fertilization measured (symbols) and simulated (lines) from 6 to 10 Mar. 1996 (DOY 66–70). Positive values represent reductions in upward fluxes under 548 vs. 363 µmol mol-1 CO2

 


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Fig. 4. Hourly averages of air temperature and wind speed from 24 to 28 Apr. 1996 (DOY 115–119) at the FACE site near Phoenix, AZ

 


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Fig. 5. Hourly averages of net radiation (Rn), latent heat (LE), and sensible heat (S) fluxes measured (symbols ± SE) and simulated (lines) from 24 to 28 Apr. 1996 (DOY 115–119) under 363 µmol mol-1 CO2 and (a) 35 g N m-2 and (b) 7 g N m-2 fertilization. Negative values represent upward fluxes

 


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Fig. 6. Differences in latent and sensible heat fluxes under 548 vs. 363 µmol mol-1 CO2 with (a) 35 g N m-2 and (b) 7 g N m-2 fertilization measured (symbols) and simulated (lines) from 24 to 28 Apr. 1996 (DOY 115–119). Positive values represent reductions in upward fluxes under 548 vs. 363 µmol mol-1 CO2

 


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Fig. 7. Canopy CO2 fluxes measured (symbols) and simulated (lines) on 21 Feb. 1996 under 363 vs. 548 µmol mol-1 CO2 and 35 vs. 7 g N m-2 fertilization

 





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