Pho Chhu

Pho Chhu
Confluence of the Pho Chhu (right) and the Mo Chhu (left) below Punakha Dzong (center)
Location
CountryBhutan
Physical characteristics
Source 
 • locationHimalayas
Mouth 
 • location
Puna Tsang Chhu

Pho Chhu is a major river in Bhutan. The rivers arises in the slopes of Kula Kangri in the Himalayas. It flows towards the Punakha valley, where its joins the Mo Chhu at near Punakha Dzong to form the Puna Tsang Chhu river, which forms part of the Brahmaputra river system.

Geography

The headwaters of the Pho Chhu are located in the hills of Lunana Gewog in northern Bhutan. The river is fed by glaciers in the Himalayas. The rivers arises in the western slope of Kula Kangri in the Himalayas. The rivers has two branches, with the eastern branch fed by various glaciers near Lunana and the western branch fed by glaciers near Tarina in the gewog.

The Pho Chu basin consists of 154 glaciers covering 334.36 km2 (129.10 sq mi) with an estimated ice reserve of 32.27 km3 (7.74 cu mi). Of these, 71 glaciers feed the western branch while the remaining feed the eastern branch of the river. The largest glaciers feeding the eastern and western branches are Tshoju Glacier and Wachey Glacier respectively.

The Pho Chu flows towards Punakha, where it joins the Mo Chhu near the Punakha Dzong. The two rivers combine to form the Puna Tsang Chhu river at their confluence, and is joined by Tang Chu at Wangdue Phodrang. The Puna Tsang Chu later joins the Brahmaputra. The river supports freshwater fish species such as Schizothorax richardsonii and Salmo trutta.

Ecology and climate change

Climate change has increased the risk of glacial lake outburst floods in the Pho Chhu basin as increasing temperatures had accelerated glacier retreat and led to the expansion of glacial lakes. As the river flows through several settlements, it poses a risk to downstream communities, agriculture, and other infrastructure. Since 2008, the Government of Bhutan, with the aid of United Nations Development Programme, has implemented adaptation measures aidmed at reducing the risk of such floods in the Punakha and Wangdue valleys.

Cultural significance

In Bhutanese culture, the Pho Chhu and Mo Chhu are known as "father river", and "mother river" respectively. Situated at the confluence of Mo Chhu and Pho Chhu, the Punakha Dzong, constructed by Ngawang Namgyal in 1637–1638, is one of the important religious and political centres of Bhutan.

References

  1. 1 2 3 "Punakha Dzong". Government of Bhutan. Archived from the original on 29 August 2026. Retrieved 5 October 2026.
  2. ↑ Major Rivers and Mountain Passes in Bhutan (PDF). Royal Education Council, Department of School Education, Government of Bhutan. p. 23. Archived (PDF) from the original on 4 April 2025. Retrieved 5 October 2026.
  3. ↑ "Punatsangchhu-I Hydroelectric Project". Government of Bhutan. Archived from the original on 25 September 2026. Retrieved 1 October 2026.
  4. 1 2 3 Hydro-meteorology of Bhutan. International Centre for Integrated Mountain Development. p. 14. Archived from the original on 29 April 2026. Retrieved 1 October 2026.
  5. ↑ "Survey of the Waters of Bhutan: Physiography and Fisheries Potential". Food and Agriculture Organization. Archived from the original on 18 August 2026. Retrieved 5 October 2026.
  6. ↑ Negi, Sharad Singh (1991). Himalayan Rivers, Lakes, and Glaciers. Indus Publishing. p. 109. ISBN 978-8-185-18261-2.
  7. ↑ "Schizothorax richardsonii (Gray, 1832)". National Research Centre for Riverine and Lake Fisheries. Archived from the original on 14 June 2026. Retrieved 5 October 2026.
  8. ↑ "Salmo trutta (Linnaeus, 1758)". National Research Centre for Riverine and Lake Fisheries. Archived from the original on 15 March 2026. Retrieved 5 October 2026.
  9. ↑ "Reducing Climate Change-induced Risks from Glacial Lake Outburst Floods in Bhutan". United Nations Development Programme. Archived from the original on 22 October 2026. Retrieved 1 October 2026.
  10. ↑ "Dzongs of Bhutan". UNESCO. Archived from the original on 13 December 2024. Retrieved 1 October 2026.

27°34′42″N 89°51′58″E / 27.5783°N 89.8662°E / 27.5783; 89.8662