Title:
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
2Motivation
- 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.
3Objectives
- 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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5Corn for Harvest
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9July 04 02 Rainfall (mm)
10Total Rainfall (6/1/02-8/19/02) (cm)
11Study Site
- Walnut Creek Watershed, Ames Iowa
- 5100 ha typical corn/soy rotation
- Privately owned production fields
12Instrumentation - EC
- 12 EC 3-D sonic anemometer (CSAT3)
- 10 Open path CO2/H2O IRGA (LI7500)
- 2 KH20
- Time series and flux averages
13Instrumentation - 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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15- Twin Otter
- Instrumentation
- SMEX02 Flights
- Twin Otter FLUX measurements
- Latent Heat (LE)
- Sensible Heat (H)
- CO2
16CO2 Gradient in Corn Canopy
DOY 202 Nighttime
DOY 202 Daytime
17Soil 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-
18Data 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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20Exploratory 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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29Observations
- 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
30Observations
- 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.
31Conclusions
- 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