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Titel Improving sensitivity to vegetation variability in the EC-Earth Earth System Model
VerfasserIn Andrea Alessandri, Franco Catalano, Matteo De Felice
Konferenz EGU General Assembly 2014
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 16 (2014)
Datensatznummer 250092728
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2014-7087.pdf
 
Zusammenfassung
The EC-Earth earth system model has been recently developed to include the dynamics of vegetation through the coupling with the LPJ-Guess model. In its original formulation, the coupling between atmosphere and vegetation variability is simply operated by the vegetation Leaf Area Index (LAI), which affects climate by only changing the vegetation physiological resistance to evapotranspiration. This coupling with no implied change of the vegetation fractional coverage has been reported in previous work to have a weak effect on the surface climate modeled by EC-Earth. The effective vegetation fractional coverage can vary at seasonal and interannual time-scales as a function of leaf-canopy growth, phenology and senescence, and therefore affect biophysical parameters such as the surface roughness, albedo and soil field capacity. To adequately represent this effect in EC-Earth, we included an exponential dependence of the vegetation density to the LAI, based on a Lambert-Beer formulation. By comparing historical 20th-century simulations and retrospective forecasts performed applying the new effective fractional-coverage parameterization with the respective reference simulations using the original constant vegetation-fraction, it is demonstrated an increased effect of vegetation on the EC-Earth surface climate. The analysis shows noticeable sensitivity of EC-Earth surface climate at seasonal to interannual time-scales due to the variability of vegetation effective fractional coverage. Particularly large effects are shown over boreal winter middle-to-high latitudes, where the cooling effect of the new parameterization appears to correct the warm biases of the control simulations.