Soil evaporation from tiger-bush in south-west Niger
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Urban evapotranspiration estimation based on anthropogenic activities and modified Penman-Monteith model
2022, Journal of HydrologyEvapotranspiration partitioning and its interannual variability over a winter wheat-summer maize rotation system in the North China Plain
2021, Agricultural and Forest MeteorologyEvaluation of alternative two-source remote sensing models in partitioning of land evapotranspiration
2021, Journal of HydrologyMethods to estimate heat balance in coastal wetlands
2018, Coastal Wetlands: An Integrated Ecosystem ApproachImproving the prediction of soil evaporation for different soil types under dryland cropping
2017, Agricultural Water ManagementCitation Excerpt :This is because the wheat crop was grown during winter season with lower rainfall intensity and duration, causing lower numbers of wetting-drying events, than the summer season. Although it is possible for ES1 phase to last for several days (Wallace and Holwill, 1997), ES1 is often found to be short lived, e.g. a day or less (Yunusa et al., 1994; Wallace and Holwill, 1997). This leads to much longer ES2 phase and its greater contribution to the net in-crop ES.
Simulation of the evaporation of soil water beneath a wheat crop canopy
2014, Agricultural Water ManagementCitation Excerpt :1) The change from the energy dependent to the soil limited stage of evaporation is not abrupt, but occurs gradually, and it has been postulated that during the transition period, evaporation is sensitive to both the drying potential of the air and the hydraulic properties of the soil (Jalota and Prihar, 1991; Yunusa et al., 1994). ( 2) Stage 1 drying does not always last for an integral number of days and could be less than 1 day in very sandy soils (Eberbach and Pala, 2005; Wallace and Holwill, 1997) or even non-detectable during periods of high evaporation (Johns, 1982), which makes it difficult to define the beginning of stage 2 drying accurately. ( 3) The assumption of a decline in cumulative stage 2 evaporation as a function of the square root of time (Hillel, 1980; Monteith, 1981; Ritchie, 1972) appears to have little empirical support.