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Modelling annual pasture dynamics: Application to stomatal ozone deposition
Authors:Ignacio González-Fernández  Victoria Bermejo  Susana Elvira  Javier Sanz  Benjamín S. Gimeno  Rocío Alonso
Affiliation:1. Professor, Departamento de Ecología, Universidad Complutense de Madrid, 28040 Madrid, Spain.;2. Associate Professor, Departamento de Ecología, Universidad Complutense de Madrid, 28040 Madrid, Spain.;3. Professor, Departamento de Ecología, Universidad de Alcalá, 28871 Alcalá de Henares, Madrid, Spain.;1. IPSP-CNR, Via Madonna del Piano 10, 50019 Sesto Fiorentino, Italy;2. IBIMET-CNR, Via Caproni 8, 50145 Firenze, Italy;3. INCDS, B-dul Eroilor 128, Voluntari, Ilfov, Romania
Abstract:Modelling ozone (O3) deposition for impact risk assessment is still poorly developed for herbaceous vegetation, particularly for Mediterranean annual pastures. High inter-annual climatic variability in the Mediterranean area makes it difficult to develop models characterizing gas exchange behaviour and air pollutant absorption suitable for risk assessment. This paper presents a new model to estimate stomatal conductance (gs) of Trifolium subterraneum, a characteristic species of dehesa pastures. The MEDPAS (MEDiterranean PAStures) model couples 3 modules estimating soil water content (SWC), vegetation growth and gs. The gs module is a reparameterized version of the stomatal component of the EMEP DO3SE O3 deposition model. The MEDPAS model was applied to two contrasting years representing typical dry and humid springs respectively and with different O3 exposures. The MEDPAS model reproduced realistically the gs seasonal and inter-annual variations observed in the field. SWC was identified as the major driver of differences across years. Despite the higher O3 exposure in the dry year, meteorological conditions favoured 2.1 times higher gs and 56 day longer growing season in the humid year compared to the dry year. This resulted in higher ozone fluxes absorbed by T. subterraneum in the humid year. High inter-family variability was found in gas exchange rates, therefore limiting the relevance of single species O3 deposition flux modelling for dehesa pastures. Stomatal conductance dynamics at the canopy level need to be considered for more accurate O3 flux modelling for present and future climate scenarios in the Mediterranean area.
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