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Waterflows decreasing in Nepal Himalayas
  • Waterflows decreasing in Nepal Himalayas

Copyright: Paul Quayle / Panos

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  • Decreasing water flows in the Nepal Himalayas can affect power production and food security

  • Local authorities need to consider adaptation methods in Nepal’s Dudh Kosi river basin

  • The predictions are, however, based on ‘uncertain’ models and more glacier studies are needed

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[KATHMANDU] A new study forecasts decreasing stream flows and ice volume in the Nepal Himalayas for the remainder of the century with negative consequences for power production, irrigation and food security.

The study, due to be published September in Science of the Total Environment, says stream flows in the Dudh Koshi river basin of Nepal are expected to decline 30 per cent by 2100, while ice volume in the glaciers feeding the river may decline by half during the same period.

Predicting negative impacts on agriculture and hydropower potential in the region, the authors urge authorities to prepare for a future decline in water availability.

“Climate change is already affecting crops in Nepal, and in the Dudh Koshi area, lack of irrigation water will worsen this effect,” says corresponding author Daniele Bocchiola, an associate professor at the Polytechnic University of Milan (PUM).

Bocchiola and colleagues collected data from the Dudh Koshi river area, during field expeditions in 2012—2014, on ice melt, debris thickness on the Khumbu glacier, ice flow velocity, hydrological fluxes within the river, and snow depth at high altitudes. The work was supported by PUM and the Nepal Academy of Science and Technology.
The field data was combined with historical ground and satellite data, as well as global climate models to assess changes in the hydrological cycle until the year 2100. A glacio-hydrological model for 2045—2054 and 2090—2099 emerged and this was compared against data for 2012—2014.
 
Currently, ice melt contributes about 55 per cent of stream flows annually, with snow melt accounting for 19 per cent. The scientists predicted a four per cent decrease in the flows, with ice melt making up 45 per cent of stream flows and snow melt 28 per cent. By the end of the century ice melt would account for just 31 per cent of stream flows in the river, while snow would contribute 39 per cent.
 
That would make the local population of 110,000 people — projected to climb to 140,000 by 2100 — more dependent on snow melt.
 
“In the Everest valley, as in many other areas in Nepal, there is tremendous need for irrigation to increase crop yield, and food security, and of hydropower plants to capture at least part of the tremendous, yet unexplored, potential of the area, especially given the low availability of electric power for the local population,” said Bocchiola, adding that local authorities need to study adaptation strategies. 
 
Ann Rowan, a research fellow in the department of geography at the University of Sheffield, who has studied hydrological changes in the region, says that the “detailed field observations from Khumbu Glacier are essential to understanding how fast this glacier changes.”
 
However, she cautions that, since the Himalayas are vast and contain many glaciers, model predictions like those discussed in the paper “contain uncertainties” in the predicted rates of ice loss and that more observations are required to understand “how the glaciers respond to climate change.”
 
This piece was produced by SciDev.Net’s South Asia desk.
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