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https://w3id.org/ro-id/648630a1-c6a3-4f64-8a39-e4cd29a55221/ http://schema.org/description The water supply from the Himalayan and Tibetan Plateau is of great importance for millions of people (Bookhagen & Burbank 2010). The water from this region provides drinking water, supports agricultural demands, is used for hydropower generation and other agro-economic activities (Ménégoz et al. 2013). The countries in the High Mountain Asia (HMA) region have a huge potential for developing hydropower making the shift towards a greener economy more feasible. The main objective of this study is to evaluate the Shyft modelling framework in its ability to simulate main water balance components, especially discharge, in the specific conditions of the Budhi-Gandaki catchment with scarce data and extreme topography. • Is the model able to capture precipitation variations on the leeward and windward sides of the catchment, and predict discharge adequately? • How sensitive the model is to the forcings, spatial representation (grid or triangular- irregular networks) and scales? References: Bookhagen, B. & Burbank, D. W. (2010), ‘Toward a complete himalayan hydrological budget: Spatiotemporal distribution of snowmelt and rainfall and their impact on river discharge’, Journal of Geophysical Research: Earth Surface 115(F3). Ménégoz, M., Gallée, H. & Jacobi, H. 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Jacob Qvam, Olga Silantyeva, Lena Merete Tallaksen, and Kristoffer Aalstad. 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