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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 10
Hydrol. Earth Syst. Sci., 14, 1801–1817, 2010
https://doi.org/10.5194/hess-14-1801-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 14, 1801–1817, 2010
https://doi.org/10.5194/hess-14-1801-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  11 Oct 2010

11 Oct 2010

Climatology-based regional modelling of potential vegetation and average annual long-term runoff for Mesoamerica

P. Imbach1, L. Molina1, B. Locatelli2, O. Roupsard1,3, P. Ciais4, L. Corrales5, and G. Mahé6 P. Imbach et al.
  • 1CATIE 7170, Turrialba, Cartago 30501, Costa Rica
  • 2CIRAD UPR Forest Ecosystem Services, Montpellier, France, CIFOR ENV Program, Bogor, Indonesia
  • 3CIRAD, UPR80, Fonctionnement et Pilotage des Ecosystémes de Plantations, Montpellier, France
  • 4IPSL – LSCE, CEA CNRS UVSQ, Centre d'Etudes Orme des Merisiers, 91191 Gif sur Yvette, France
  • 5The Nature Conservancy, P.O. Box, 230–1225, San José, Costa Rica
  • 6IRD/HydroSciences Montpellier, Case MSE, Université Montpellier 2, 34095 Montpellier, Cedex 5, France

Abstract. Mean annual cycles of runoff, evapotranspiration, leaf area index (LAI) and potential vegetation were modelled for Mesoamerica using the SVAT model MAPSS with different climatology datasets. We calibrated and validated the model after building a comprehensive database of regional runoff, climate, soils and LAI. The performance of several gridded precipitation climatology datasets (CRU, FCLIM, WorldClim, TRMM, WindPPT and TCMF) was evaluated and FCLIM produced the most realistic runoff. Annual runoff was successfully predicted (R2=0.84) for a set of 138 catchments, with a low runoff bias (12%) that might originate from an underestimation of the precipitation over cloud forests. The residuals were larger in small catchments but remained homogeneous across elevation, precipitation, and land-use gradients. Assuming a uniform distribution of parameters around literature values, and using a Monte Carlo-type approach, we estimated an average model uncertainty of 42% of the annual runoff. The MAPSS model was most sensitive to the parameterization of stomatal conductance. Monthly runoff seasonality was mimicked "fairly" in 78% of the catchments. Predicted LAI was consistent with MODIS collection 5 and GLOBCARBON remotely sensed global products. The simulated evapotranspiration:runoff ratio increased exponentially for low precipitation areas, highlighting the importance of accurately modelling evapotranspiration below 1500 mm of annual rainfall with the help of SVAT models such as MAPSS. We propose the first high-resolution (1 km2 pixel) maps combining average long-term runoff, evapotranspiration, leaf area index and potential vegetation types for Mesoamerica.

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