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Evapotranspiration on the basis of its conservativeness and because a fixed relation back exists between ultimate radiation used for heating the aerial and that put-upon in evaporation low potential conditions.
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The end of this projection is to comparison evapotranspiration measurements affected at flux towers to evapotranspiration estimates generated by the mod16 algorithm for modis.
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Chapter 1 - introduction to evapotranspiration.
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What is crop evapotranspiration under standard conditions?
Crop evapotranspiration under standard conditions (ET c) refers to the evaporating demand from crops that are grown in large fields under optimum soil water, excellent management and environmental conditions, and achieve full production under the given climatic conditions.
How is the evaporation power of the atmosphere expressed?
The evaporation power of the atmosphere is expressed by the reference crop evapotranspiration (ET o ). The reference crop evapotranspiration represents the evapotranspiration from a standardized vegetated surface. The ET o is described in detail later in this Chapter and in Chapters 2 and 4.
How is the partition of evapotranspiration and transpiration plotted?
In Figure 2 the partitioning of evapotranspiration into evaporation and transpiration is plotted in correspondence to leaf area per unit surface of soil below it. At sowing nearly 100% of ET comes from evaporation, while at full crop cover more than 90% of ET comes from transpiration.
How is the evapotranspiration rate expressed in MJ M-2?
The evapotranspiration rate expressed in units of MJ m -2 day -1 is represented by l ET, the latent heat flux. Table 1 summarizes the units used to express the evapotranspiration rate and the conversion factors. TABLE 1. Conversion factors for evapotranspiration
Last Update: Oct 2021
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