Espa˝ol || Franšais
      AQUASTAT Home        About AQUASTAT     FAO Water    Statistics at FAO

Featured products

Main Database
Dams
Global map of irrigation areas
Irrigation water use
Water and gender
Climate info tool
Institutions

Geographical entities

Countries, regions, river basins

Themes

Water resources
Water uses
Irrigation and drainage
Wastewater
Institutional framework
Other themes

Information type

Datasets
Publications
Summary tables
Maps and spatial data
Glossary

Info for the media

Did you know...?
Visualizations and infographics
SDG Target 6.4
KWIP
UNW Briefs
     

Read the full profile

Nepal

Water resources

Average annual precipitation is an estimated 1 500 mm (Table 2). Nepal has more than 6 000 rivers, which provide a dense network with steep topographic conditions. All rivers in Nepal drain into the Ganges river. The country is divided into five river basins, which are from west to east:

  • Mahakali river basin, which is shared with India, with an average flow from the Indian tributaries into the border river, of arounds 15 km3/year and some 3.4 km3/year from the Nepalese tributaries.
  • Karnali river basin, with an average outflow of about 43.9 km3/year.
  • Gandaki river basin, with an average outflow of roughlys 50.7 km3/year;
  • Kosi river basin, with an average outflow estimated as 47.2 km3/year, which receives a contribution of some 12 km3/year from the upper catchment area located in China; and the
  • southern river basins, which produce some 65 km3/year of water flowing into India.


The seasonal distribution of flow is extremely variable. It might be as low as 1.5-2.4 percent of the total runoff in January, February and March, and as high as 20-27 percent in July and August for snowfed rivers, while the corresponding figures for purely rainfed rivers are 0.5-3 percent from March to May and 19-30 percent in July and August.

The surface water resources produced internally are estimated as 198.2 km3/year. The groundwater resources have not been fully assessed. Ongoing studies show that a good potential for groundwater extraction exists, especially in the southern terai lowland plains and inner valleys of the hilly and mountainous regions. Much of the terai physiographic region and some parts of siwalik valleys are underlain by deep or shallow aquifers, many of which are suitable for exploitation as sources of irrigation water. A rough estimate can be made by assuming a groundwater resource equivalent to 10 percent of surface water, i.e. approximately 20 km3/year, which corresponds to the base flow of the rivers. The total internal water resources would therefore amount to 198.2 km3/year. Chinese statistics mention an average outflow to Nepal of 12 km3/year, which brings the total renewable water resources of Nepal to 210.2 km3/year. It is assumed that all the renewable water resources of Nepal flow out of the country to India.

In 2009, the total dam capacity was 85 million m3, although the potential exists for at least 138 km3. Hydroelectricity accounted for more than 96 percent of total electricity generation. The two main diversion barrages are the Kosi and Gandaki reservoirs.

     
   
   
             

^ go to top ^

       Quote as: FAO. 2016. AQUASTAT website. Food and Agriculture Organization of the United Nations (FAO). Website accessed on [yyyy/mm/dd].
      © FAO, 2016   |   Questions or feedback?    [email protected]
       Your access to AQUASTAT and use of any of its information or data is subject to the terms and conditions laid down in the User Agreement.