2015
DOI: 10.1080/07055900.2014.999745
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Modelling of Seasonal Evapotranspiration from an Agricultural Field Using the Canadian Land Surface Scheme (CLASS) with a Pedotransfer Rule and Multicriteria Optimization

Abstract: The performance of the Canadian Land Surface Scheme (CLASS 3.5) was assessed using turbulent fluxes derived from data recorded at two micrometeorological stations located in a potato field in Quebec, Canada. The minimum stomatal resistance, the maximum leaf area index, and the initial water content of the third soil layer were optimized using the Non-Dominated Sorting Genetic Algorithm-II and the mean square error of the latent heat flux. With respect to benchmark solutions, the optimization improved the sensi… Show more

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Cited by 4 publications
(2 citation statements)
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“…PTFs are frequently developed to estimate volumetric water content for any given matric potential, porosity, saturated hydraulic conductivity, or bulk density. PTFs are also used to estimate plant available water [1,2], to model physical properties of soil during seasonal evapotranspiration [3], or to characterize the parameters of water retention curve models [4,5]. The most common predictors of soil physical properties are soil particle size distribution, organic matter content, coarse fragment content, and sometimes bulk density.…”
Section: Introductionmentioning
confidence: 99%
“…PTFs are frequently developed to estimate volumetric water content for any given matric potential, porosity, saturated hydraulic conductivity, or bulk density. PTFs are also used to estimate plant available water [1,2], to model physical properties of soil during seasonal evapotranspiration [3], or to characterize the parameters of water retention curve models [4,5]. The most common predictors of soil physical properties are soil particle size distribution, organic matter content, coarse fragment content, and sometimes bulk density.…”
Section: Introductionmentioning
confidence: 99%
“…Among state‐of‐the‐art LSSs, one finds the Canadian Land Surface Scheme (CLASS), which has been tested across a wide range of landscapes over the North American continent, especially at middle and high latitudes. These include boreal aspen forests (Arain et al, ; Bartlett et al, ; ; Wang et al, ), peatlands (Lafleur et al, ; Wu et al, ), croplands (Arora, ; Bailey et al, ; Kothavala et al, ), tundras (Lafleur et al, ; Verseghy et al, ), and many others (Bartlett & Verseghy, ; Bellisario et al, ; Brown et al, ; Comer et al, ; Morais et al, ).…”
Section: Introductionmentioning
confidence: 99%