Directory UMM :Data Elmu:jurnal:A:Agricultural & Forest Meterology:Vol104Issue4Sept2000:
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In 1986 and 1988, Akella and Kumar (for the innite horizon discounted cost) and Bielecki and Kumar (for the innite horizon average expected cost) show that the optimal policy is
Earlier experiments over dense, tall, and short canopies demonstrated that the surface renewal method works, but requires a correction for uneven heating (e.g. For sparse canopies,
Relative root mean square difference (RMSD/ λ EL) of the daytime BREB and lysimeter latent heat flux comparison correlated with the energy balance Bowen ratio, by days within leaf
An area-average soil heat flux from the array is compared with a set of three measurements from a standard micro-meteorological station judiciously positioned to obtain
Some examples: (a) in the discussion of the greenhouse effect, it is stated that greenhouse gases reflect terrestrial radiation — this, of course, is not correct.. It is the
Comparison of the mean duration (in days) of six wheat development phases calculated using the AFRCWHEAT2 model with observed daily data and daily data estimated using a sine
The effect of total radiation during Phase IV ( X 11 ) remained negative after dropping the interaction be- tween radiation and trial type ( X 13 ). Therefore, X 11 was excluded
One was the interpo- lation of measured global radiation sums (daily and monthly values) via atmospheric transmittance and the other, a parameterisation scheme with subsequent
