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dc.creatorVerhoef, Annees
dc.creatorEgea Cegarra, Gregorioes
dc.date.accessioned2018-05-08T17:41:56Z
dc.date.available2018-05-08T17:41:56Z
dc.date.issued2014
dc.identifier.citationVerhoef, A. y Egea Cegarra, G. (2014). Modeling plant transpiration under limited  soil water: comparison of different plant  and soil hydraulic parameterizations and  preliminary implications for their use in  land surface models. Agricultural and Forest Meteorology, 2014 (191), 22-32.
dc.identifier.issn0168-1923es
dc.identifier.urihttps://hdl.handle.net/11441/74330
dc.description.abstractAccurate estimates of how soil water stress affects plant transpiration are crucial for reliable land surface model (LSM) predictions. Current LSMs generally use a water stress factor, β, dependent on soil moisture content, θ, that ranges linearly between β = 1 for unstressed vegetation and β = 0 when wilting point is reached. This paper explores the feasibility of replacing the current approach with equations that use soil water potential as their independent variable, or with a set of equations that involve hydraulic and chemical signaling, thereby ensuring feedbacks between the entire soil–root–xylem–leaf system. A comparison with the original linear θ-based water stress parameterization, and with its improved curvi-linear version, was conducted. Assessment of model suitability was focused on their ability to simulate the correct (as derived from experimental data) curve shape of relative transpiration versus fraction of transpirable soil water. We used model sensitivity analyses under progressive soil drying conditions, employing two commonly used approaches to calculate water retention and hydraulic conductivity curves. Furthermore, for each of these hydraulic parameterizations we used two different parameter sets, for 3 soil texture types; a total of 12 soil hydraulic permutations. Results showed that the resulting transpiration reduction functions (TRFs) varied considerably among the models. The fact that soil hydraulic conductivity played a major role in the model that involved hydraulic and chemical signaling led to unrealistic values of β, and hence TRF, for many soil hydraulic parameter sets. However, this model is much better equipped to simulate the behavior of different plant species. Based on these findings, we only recommend implementation of this approach into LSMs if great care with choice of soil hydraulic parameters is taken.es
dc.description.sponsorshipUnión Europea NE/I006834/1es
dc.formatapplication/pdfes
dc.language.isoenges
dc.publisherElsevieres
dc.relation.ispartofAgricultural and Forest Meteorology, 2014 (191), 22-32.
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectPlant water stresses
dc.subjectGas exchangees
dc.subjectStomatal conductancees
dc.subjectHydraulic signalinges
dc.subjectWater retention curvees
dc.subjectLand surface modeles
dc.titleModeling plant transpiration under limited  soil water: comparison of different plant  and soil hydraulic parameterizations and  preliminary implications for their use in  land surface modelses
dc.typeinfo:eu-repo/semantics/articlees
dcterms.identifierhttps://ror.org/03yxnpp24
dc.type.versioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Ingeniería Aeroespacial y Mecánica de Fluidoses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Ciencias Agroforestaleses
dc.relation.projectIDNE/I006834/1es
dc.relation.publisherversionhttps://doi.org/10.1016/j.agrformet.2014.02.009es
dc.identifier.doi10.1016/j.agrformet.2014.02.009es
dc.contributor.groupUniversidad de Sevilla. AGR268: Naturación Urbana e Ingeniería de Biosistemases
idus.format.extent11 p.es
dc.journaltitleAgricultural and Forest Meteorologyes
dc.journaltitleAgricultural and Forest Meteorology
dc.publication.volumen2014es
dc.publication.issue191es
dc.publication.initialPage22es
dc.publication.endPage32es
dc.identifier.sisius19490es
dc.contributor.funderEuropean Union (UE)
dc.contributor.funderEuropean Union (UE)

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