Future hydrological regimes and glacier cover in the Everest region: The case study of the upper Dudh Koshi basin
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We pursued glacio-hydrological modeling of the Dudh Koshi river of Nepal.

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We used in situ data gathered during 2012–2014, historical ground and satellite data.

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We investigated the impact of climate change until 2100 using IPCC AR5 scenarios.

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Stream flows will be largely reduced (− 30% or so) until 2100.

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Ice volume in the catchment will largely decrease (− 50% or so) until 2100.

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