We pursued glacio-hydrological modeling of the Dudh Koshi river of Nepal.
We used in situ data gathered during 2012–2014, historical ground and satellite data.
We investigated the impact of climate change until 2100 using IPCC AR5 scenarios.
Stream flows will be largely reduced (− 30% or so) until 2100.
Ice volume in the catchment will largely decrease (− 50% or so) until 2100.