The report finds that while meltwater contributes to annual streamflow in different proportions in various river basins, the share of the non-renewable component of glacial runoff increased from 16-30% in all basins to 26-46% across the basins represented in the study. However, the study also demonstrates that climate change related decrease in glaciers and snow cover will not heavily impact the mean annual flow, but will affect seasonality.

IWMI is a member of the Consultative Group on International Agriculture Research (CGIAR).

[Read the full report: Glacier Systems and Seasonal Snow Cover in Six Major Asian River Basins: Hydrological Role under Changing Climate, July 2013]

 

Leave a Reply

Your email address will not be published. Required fields are marked *