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Mean annual GPP of Europe derived from its water balance

Identifieur interne : 009E93 ( Main/Merge ); précédent : 009E92; suivant : 009E94

Mean annual GPP of Europe derived from its water balance

Auteurs : C. Beer [Allemagne] ; M. Reichstein [Allemagne] ; P. Ciais [France] ; G. D. Farquhar [Australie] ; D. Papale [Italie]

Source :

RBID : Pascal:07-0224361

Descripteurs français

English descriptors

Abstract

[1] On local scale, the eddy covariance technique is suited to estimate gross primary production (GPP). Scaling up such observations to the regional and continental level, however, remains a challenge. Here, we show that there is a surprisingly robust stoichiometric relationship between vegetation CO2 and H2O fluxes, mediated by vapor pressure deficit (VPD), across many different forest vegetation types. This relationship is used to provide a data-driven estimate of Europe's GPP from its water balance. Namely, watershed-wide evapotranspiration (ET), as derived from precipitation (P) and river runoff (R), is multiplied by the ratio of GPP to ET as derived from eddy covariance measurements (water-use efficiency, WUE). In doing so, GPP of Europe is estimated to range between 3.9 and 5.8 PgC/a (median 5 PgC/a). Such GPP estimate is an important independent benchmark for large-scale ecosystem models and may be extended to global scale when relevant data becomes available.

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Pascal:07-0224361

Le document en format XML

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<term>Europe</term>
<term>Planetary scale</term>
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<term>atmospheric precipitation</term>
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<term>Pression vapeur</term>
<term>Forêt</term>
<term>Bassin versant</term>
<term>Evapotranspiration</term>
<term>Précipitation atmosphérique</term>
<term>Rivière</term>
<term>Ruissellement eau sol</term>
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<term>Covariance</term>
<term>Efficacité</term>
<term>Ecosystème</term>
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<div type="abstract" xml:lang="en">[1] On local scale, the eddy covariance technique is suited to estimate gross primary production (GPP). Scaling up such observations to the regional and continental level, however, remains a challenge. Here, we show that there is a surprisingly robust stoichiometric relationship between vegetation CO
<sub>2</sub>
and H
<sub>2</sub>
O fluxes, mediated by vapor pressure deficit (VPD), across many different forest vegetation types. This relationship is used to provide a data-driven estimate of Europe's GPP from its water balance. Namely, watershed-wide evapotranspiration (ET), as derived from precipitation (P) and river runoff (R), is multiplied by the ratio of GPP to ET as derived from eddy covariance measurements (water-use efficiency, WUE). In doing so, GPP of Europe is estimated to range between 3.9 and 5.8 PgC/a (median 5 PgC/a). Such GPP estimate is an important independent benchmark for large-scale ecosystem models and may be extended to global scale when relevant data becomes available.</div>
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   |texte=   Mean annual GPP of Europe derived from its water balance
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