Directory UMM :Data Elmu:jurnal:A:Agricultural & Forest Meterology:Vol103Issue4July2000:
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The two-source model, allowing for sparse canopy cover (Shuttleworth and Wallace, 1985; Shuttleworth and Gurney, 1990), is added to the DAISY model struc- ture and modeled
Soil evaporation was estimated using a second eddy covariance system below the canopy, and these measurements suggest that soil evaporation explains only a small portion of
Sources and sinks of heat in the canopy of a dense corn crop (LAI ∼ 5) were inferred through an inverse Lagrangian dispersion analysis. Input data were the profiles of air
Free-air CO 2 enrichment (FACE): blower effects on wheat canopy microclimate and plant
For example, using eddy covari- ance measurements, Tsukamoto (1993) found a sig- nificantly smaller net CO 2 flux from the atmosphere to a rice canopy when the field was drained
The most obvi- ous difference between both experiments was S, where the sunflower canopy in the 1998 experiment would fluctuate between one to two azimuth preferences, but in the
A statistical interpolation method is proposed which allows calculation of the leaf area index LAI(t), the downward cumulative leaf area index L(z, t) and the canopy leaf area
For the LI-COR LI-200SA Pyranometer Sensor, systematic spectral errors for the global radiation reflected or penetrated by the canopy are high (20–40%), and this instrument cannot
