Effect of the water stress on gross primary production modeling of a Mediterranean oak savanna ecosystem
Dehesa ecosystem consists of widely-spaced oak trees combined with crops, pasture and Mediterranean shrubs. It is located in the southwest of the Iberian Peninsula, where water scarcity is recurrent, severely affecting the multiple productions and services of the ecosystem. Upscaling in situ Gross P...
Saved in:
Published in | Proceedings of the International Association of Hydrological Sciences Vol. 380; pp. 37 - 43 |
---|---|
Main Authors | , , , , |
Format | Journal Article Conference Proceeding |
Language | English |
Published |
Gottingen
Copernicus GmbH
18.12.2018
Copernicus Publications |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Summary: | Dehesa ecosystem consists of widely-spaced oak trees combined with
crops, pasture and Mediterranean shrubs. It is located in the southwest of
the Iberian Peninsula, where water scarcity is recurrent, severely affecting
the multiple productions and services of the ecosystem. Upscaling in situ
Gross Primary Production (GPP) estimates in these areas is challenging for
regional and global studies, given the significant spatial variability of
plant functional types and the vegetation stresses usually present. The
estimation of GPP is often addressed using light use efficiency models
(LUE-models). Under soil water deficit conditions, biomass production is
reduced below its potential rate. This work investigates the effect of
different parameterizations to account for water stress on GPP estimates and
their agreement with observations. Ground measurements of GPP are obtained
using an Eddy Covariance (EC) system installed over an experimental site
located in Córdoba, Spain. GPP is estimated with a LUE-model in the
footprint of the EC tower using several approaches: a fixed value taken from
previous literature; a fixed value modified by daily weather conditions; and
both formulations modified by an additional coefficient to explicitly
consider the vegetation water stress. The preliminary results obtained during
two hydrological years (2015/2016 and 2016/2017) are compared, focusing on
specific wet and dry periods. |
---|---|
ISSN: | 2199-899X 2199-8981 2199-899X |
DOI: | 10.5194/piahs-380-37-2018 |