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Consistent increase in High Asia's runoff due to increasing glacier melt and precipitation

Author

Listed:
  • A. F. Lutz

    (FutureWater, Costerweg 1V
    Utrecht University)

  • W. W. Immerzeel

    (FutureWater, Costerweg 1V
    Utrecht University
    International Centre for Integrated Mountain Development)

  • A. B. Shrestha

    (International Centre for Integrated Mountain Development)

  • M. F. P. Bierkens

    (Utrecht University
    Deltares)

Abstract

The impact of climate change on the water resources and hydrology of High Asia is uncertain. This work uses a cryospheric hydrological model to quantify the hydrology of five major rivers in the region and project future water availability. Runoff is expected to increase until at least 2050 due to an increase in precipitation in the upper catchment of four rivers and increased melt entering the fifth river.

Suggested Citation

  • A. F. Lutz & W. W. Immerzeel & A. B. Shrestha & M. F. P. Bierkens, 2014. "Consistent increase in High Asia's runoff due to increasing glacier melt and precipitation," Nature Climate Change, Nature, vol. 4(7), pages 587-592, July.
    • Handle: RePEc:nat:natcli:v:4:y:2014:i:7:d:10.1038_nclimate2237
    DOI: 10.1038/nclimate2237
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