Analyzing the major drivers of NEE in a Mediterranean alpine shrubland

Two years of continuous measurements of net ecosystem exchange (NEE) using the eddy covariance technique were made over a Mediterranean alpine shrubland. This ecosystem was found to be a net source of CO<sub>2</sub> (+ 52 ± 7 g C m<sup>−2</sup>...

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Main Authors: B. R. Reverter, E. P. Sánchez-Cañete, V. Resco, P. Serrano-Ortiz, C. Oyonarte, A. S. Kowalski
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/7/2601/2010/bg-7-2601-2010.pdf
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spelling doaj-3778167b4f874aeb92566a79f721fa0c2020-11-24T20:58:37ZengCopernicus PublicationsBiogeosciences1726-41701726-41892010-09-01792601261110.5194/bg-7-2601-2010Analyzing the major drivers of NEE in a Mediterranean alpine shrublandB. R. ReverterE. P. Sánchez-CañeteV. RescoP. Serrano-OrtizC. OyonarteA. S. KowalskiTwo years of continuous measurements of net ecosystem exchange (NEE) using the eddy covariance technique were made over a Mediterranean alpine shrubland. This ecosystem was found to be a net source of CO<sub>2</sub> (+ 52 ± 7 g C m<sup>−2</sup> and + 48 ± 7 g C m<sup>−2</sup> for 2007 and 2008) during the two-year study period. To understand the reasons underlying this net release of CO<sub>2</sub> into the atmosphere, we analysed the drivers of seasonal variability in NEE over these two years. We observed that the soil water availability – driven by the precipitation pattern – and the photosynthetic photon flux density (PPFD) are the key factors for understanding both the carbon sequestration potential and the duration of the photosynthetic period during the growing season. Finally, the effects of the self-heating correction to CO<sub>2</sub> and H<sub>2</sub>O fluxes measured with the open-path infrared gas analyser were evaluated. Applying the correction turned the annual CO<sub>2</sub> budget in 2007 from a sink (− 135 ± 7 g C m<sup>−2</sup>) to a source (+ 52 ± 7 g C m<sup>−2</sup>). The magnitude of this change is larger than reported previously and is shown to be due to the low air density and cold temperatures at this high elevation study site. http://www.biogeosciences.net/7/2601/2010/bg-7-2601-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. R. Reverter
E. P. Sánchez-Cañete
V. Resco
P. Serrano-Ortiz
C. Oyonarte
A. S. Kowalski
spellingShingle B. R. Reverter
E. P. Sánchez-Cañete
V. Resco
P. Serrano-Ortiz
C. Oyonarte
A. S. Kowalski
Analyzing the major drivers of NEE in a Mediterranean alpine shrubland
Biogeosciences
author_facet B. R. Reverter
E. P. Sánchez-Cañete
V. Resco
P. Serrano-Ortiz
C. Oyonarte
A. S. Kowalski
author_sort B. R. Reverter
title Analyzing the major drivers of NEE in a Mediterranean alpine shrubland
title_short Analyzing the major drivers of NEE in a Mediterranean alpine shrubland
title_full Analyzing the major drivers of NEE in a Mediterranean alpine shrubland
title_fullStr Analyzing the major drivers of NEE in a Mediterranean alpine shrubland
title_full_unstemmed Analyzing the major drivers of NEE in a Mediterranean alpine shrubland
title_sort analyzing the major drivers of nee in a mediterranean alpine shrubland
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2010-09-01
description Two years of continuous measurements of net ecosystem exchange (NEE) using the eddy covariance technique were made over a Mediterranean alpine shrubland. This ecosystem was found to be a net source of CO<sub>2</sub> (+ 52 ± 7 g C m<sup>−2</sup> and + 48 ± 7 g C m<sup>−2</sup> for 2007 and 2008) during the two-year study period. To understand the reasons underlying this net release of CO<sub>2</sub> into the atmosphere, we analysed the drivers of seasonal variability in NEE over these two years. We observed that the soil water availability – driven by the precipitation pattern – and the photosynthetic photon flux density (PPFD) are the key factors for understanding both the carbon sequestration potential and the duration of the photosynthetic period during the growing season. Finally, the effects of the self-heating correction to CO<sub>2</sub> and H<sub>2</sub>O fluxes measured with the open-path infrared gas analyser were evaluated. Applying the correction turned the annual CO<sub>2</sub> budget in 2007 from a sink (− 135 ± 7 g C m<sup>−2</sup>) to a source (+ 52 ± 7 g C m<sup>−2</sup>). The magnitude of this change is larger than reported previously and is shown to be due to the low air density and cold temperatures at this high elevation study site.
url http://www.biogeosciences.net/7/2601/2010/bg-7-2601-2010.pdf
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