Estimation of bare soil evaporation using skin temperature measurements
作者： Gabriel G. Katul , Marc B. Parlange
DOI: 10.1016/0022-1694(92)90174-T
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摘要: A simple model based on the Monin-Obukhov surface layer similarity theory of heat and momentum transport can be used to predict latent flux for a variety atmospheric soil moisture conditions. Experiments were carried out Campbell Tract at University California, Davis, from 14 September 23 November 1990. The was measured precisely with large weighing lysimeter temperature by thermal IR transducer. evaporation predictions measurements overall in good agreement (R2 = 0.86), including cases dry Even low daily order 1 mm could modeled procedure studied.
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