Articles | Volume 15, issue 13
https://doi.org/10.5194/gmd-15-5233-2022
https://doi.org/10.5194/gmd-15-5233-2022
Model evaluation paper
 | 
07 Jul 2022
Model evaluation paper |  | 07 Jul 2022

Evaluating the Atibaia River hydrology using JULES6.1

Hsi-Kai Chou, Ana Maria Heuminski de Avila, and Michaela Bray

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Cited articles

Best, M. J., Pryor, M., Clark, D. B., Rooney, G. G., Essery, R. L. H., Ménard, C. B., Edwards, J. M., Hendry, M. A., Porson, A., Gedney, N., Mercado, L. M., Sitch, S., Blyth, E., Boucher, O., Cox, P. M., Grimmond, C. S. B., and Harding, R. J.: The Joint UK Land Environment Simulator (JULES), model description – Part 1: Energy and water fluxes, Geosci. Model Dev., 4, 677–699, https://doi.org/10.5194/gmd-4-677-2011, 2011. 
Beven, K. J. and Kirkby, M. J.: A physically based, variable contributing area model of basin hydrology/Un modèle à base physique de zone d'appel variable de l'hydrologie du bassin versant, Hydrol. Sci. J., 24, 43–69, https://doi.org/10.1080/02626667909491834, 1979. 
Buytaert, W. and Beven, K.: Models as multiple working hypotheses: hydrological simulation of tropical alpine wetlands, Hydrol. Process., 25, 1784–1799, 2011. 
Campos, R. S. and de Carneiro, C. D. R.: Geologia da região de Atibaia e possíveis causas das inundações de 2009 e 2010, Terræ, 10, 21–35, 2013. 
Cavalcanti, I. F., Nunes, L. H., Marengo, J. A., Gomes, J. L., Silveira, V. P., and Castellano, M. S.: Projections of precipitation changes in two vulnerable regions of São Paulo State, Brazil, Am. J. Clim. Change, 6, 268–293, 2017. 
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Short summary
Land surface models allow us to understand and investigate the cause and effect of environmental process changes. Therefore, this type of model is increasingly used for hydrological assessments. Here we explore the possibility of this approach using a case study in the Atibaia River basin, which serves as a major water supply for the metropolitan regions of Campinas and São Paulo, Brazil. We evaluated the model performance and use the model to simulate the basin hydrology.