Directory UMM :Data Elmu:jurnal:A:Agricultural & Forest Meterology:Vol106.Issue2.2001:
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Tower eddy flux measurements above the aspen canopy showed maximum daily evapotranspiration rates from 3.5 to 4.0 mm day − 1 during the 1994 growing season (Black et al.
Measurements of aerodynamic conductance and evaporation above and below an olive orchard allowed the calibration of a transpiration model of olive trees based on the Penman –
(a) Rainfall and irrigation; (b) soil water content; (c) hydraulic potential; (d) soil temperature, all soil measurements at 0.15, 0.25 and 0.5 m below the top of the bed in the
Using a whole year’s worth of data, soil heat flux was estimated by a two-step version of the null-alignment method using soil temperature, water content and bulk density
Keywords: Aerodynamic gradient method; Eddy covariance; Continuous ammonia denuders; Bi-directional fluxes; Passive flux samplers.. ∗
The vertical distribution of sources and sinks within the canopy is derived from direct measurements of both the NH 3 concentration profile and the turbulence within the canopy,
The daytime (07:00–18:00 hours) 20 min and hourly latent heat flux values, average evaporation for the earlier mentioned three periods and evaporation on individual days were
The ratio of the gap fraction estimated using hemispherical photography to that measured using the Licor LAI-2000 plant canopy analyser at five zenith viewing angles in eight stands
