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1
  
Water, Energy and Carbon Fluxes From Tower and
Aircraft Measurements During SMACEX   J. H.
Prueger, W. P. Kustas, J. L. Hatfield, L.E.
Hipps, F. Li, C.M.U. Neale, J.I. MacPherson, M.C.
Anderson, T.B. Parkin 
2
Motivation
  • Estimated 124 Pg C (Peta grams 1012 kg) added to
    the atmosphere 1850-1990.
  • 13 from the conversion of mid-latitude
    grasslands to cultivated cropland.
  • Houghton, R.A. 1999. The annual net flux of
    carbon to the atmosphere from changes in land use
    1850-1990. Tellus.

3
Objectives
  • Quantify water use and CO2 uptake in space and
    time over corn and soybeans.
  • Compare tower E.C. measurements with an aircraft
    E.C. system.

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Corn for Harvest
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July 04 02 Rainfall (mm)
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Total Rainfall (6/1/02-8/19/02) (cm)
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Study Site
  • Walnut Creek Watershed, Ames Iowa
  • 5100 ha typical corn/soy rotation
  • Privately owned production fields

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Instrumentation - EC
  • 12 EC 3-D sonic anemometer (CSAT3)
  • 10 Open path CO2/H2O IRGA (LI7500)
  • 2 KH20
  • Time series and flux averages

13
Instrumentation - Ancillary
  • Net radiation (Kipp Zonen, REBS)
  • Soil heat flux plates w/soil TC (REBS)
  • Vitel ?v sensors
  • Temperature/humidity (Vaisala)
  • Radiometric temps (soil canopysoil)
  • Wind speed and rain gauge

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  • Twin Otter
  • Instrumentation
  • SMEX02 Flights
  • Twin Otter FLUX measurements
  • Latent Heat (LE)
  • Sensible Heat (H)
  • CO2

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CO2 Gradient in Corn Canopy
DOY 202 Nighttime
DOY 202 Daytime
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Soil CO2 flux Measurements
  • For soil CO2 flux spatial variability
  • 3 types of soil chambers
  • Non-portable continuous hourly fluxes
  • Portable chamber but not continuous
  • Hybrid-

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Data Quality/Conditioning
  • Data screening
  • Diurnal trends
  • Suspect data removed
  • Gap filling Falge et al. Ag For. Met.
    (107,2001)
  • 2-D Coordinate rotation
  • Density effects (Webb, Pearman and Leuning)

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Exploratory Equivalence Analysis(are the EC
equivalent)
Variable June 06 Sept. 17 CV
CO2 Yes Yes lt09
H Yes Yes lt11
LE Yes Yes lt10

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Observations
  • Transition (grass to corn/soy) results in
    considerable variation in the way Rn-G is part.
  • More variation in H for soy than corn more LE for
    corn than soy, variations decrease after full
    canopy
  • Differences in CO2 fluxes significant (corngtgtsoy)
    and consistent with phenotype differences.
  • Strong correlation between LAI, LE and CO2

30
Observations
  • Tower network fluxes were representative of
    regional values obtained from aircraft.
  • Single corn and soy tower meas. based on remotely
    sensed LAI provided similar regional flux values
    from the tower network.

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Conclusions
  • Results indicate highly dynamic system
  • Variability observed across spatial/temporal
    scales
  • Results represent only one component of a complex
    system (veg.atmos.)
  • Integration with soil and within canopy processes
    need to be considered
  • Further detailed analysis forthcoming
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