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millions of people (Bookhagen & Burbank 2010). The water from this region provides
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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. (2013), ‘Precipitation and snow cover in the himalaya: from reanalysis to regional climate simulations’, Hydrology and Earth System Sciences 17(10), 3921–3936.""";
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