Evapotranspiration accounts for most of fifty percent of the terrestrial hydrological cycle. We illustrate here some ways to estimate it with the tools offered by the GEOframe system.
- Derivation of the simplified energy budget (a là Penman-Monteith after Schymanski and Or)
- A simple representation on how transpiration works at plants level (from Khan Academy)
- Transpiration (YouTube2020)
- Estimation of Evaporation and Transpiration with Prospero
- Values of Wilting Point and Field Capacity parameters (Table 19)
- Values of depletion fraction parameter (Table 22)
References
- Bonan, Gordon. 2019. Climate Change and Terrestrial Ecosystem Modeling. Cambridge University Press. (And references therein, especially from chapter 8 to 11)
- Bottazzi, Michele. n.d. “Transpiration Theory and the Prospero Component of GEOframe.” Supervised by R. Rigon and G. Bertoldi. Ph.D., Civil, Environmental and Mechanical Engineering of University of Trento. (And references therein. Look expecially at chapter 2 and 3)
AboutHydrology Resources
- Here: from the AboutHydrology blog in general.
- Here: Estimation of Soil-Plants-Atmosphere interactions with Lysimeter GEO 1D
Next day
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