Himalayan Hydropower “Clean but Risky”: Scientists

C. P. Rajendran, a paleo-seismic specialist and adjunct professor at the National Institute of Advanced Studies, Bangalore, says: “The great height of the Himalayas makes them inherently unstable. These disasters are early warnings that hydropower projects, infrastructure building and tourist activity are making the mountains more unstable.”

Additionally, says Rajendran, temperature rise from climate change could increase rockfalls in the Himalayas. “Mountain permafrost holds rocks together and helps stabilise the steep slopes but warming over the last few decades may have affected its role as a slope stabilizer.”

A signatory to the letter to the prime minister, Rajendran is the author of a palaeo-seismological study, published in August, which examines the effects of past earthquakes that have hit the eastern Himalayas. A quake in 1950 — rated at 8.6 on the Richter scale and the largest continental event ever recorded — devastated Tibet and India’s Assam state, killing thousands and causing extensive landslides and flash floods, Rajendran recalls.

“The 1950 quake, which also impacted Bangladesh and Myanmar, is a grim pointer to what we can expect in the north-eastern bend of the Himalayas where massive hydropower projects are coming up, in Tibet and the adjoining Indian state of Arunachal Pradesh,” says Rajendran.

Maharaj K. Pandit, professor at the Delhi University and director of the Centre for Inter-Disciplinary Studies of Mountain and Hill Environment tells SciDev.Net that the risks of building hydropower dams in the Himalayas need to be balanced against the growing demand for clean, renewable energy.

Pandit believes that precipitation in the cold and dry Tibetan plateau is too scanty to justify a mega dam while “the area around the Brahmaputra on the Indian side is tropical and among the wettest in the world”.

The starkest example of the effects of a major quake on hydropower projects comes from Nepal where the April 2015 temblor that killed 9,000 people temporarily knocked out 20 per cent of the country’s hydropower capacity and damaged 30 dam projects.

According to Basanta Raj Adhikari, assistant professor at Tribhuvan University’s Institute of Engineering, in Nepal, one solution is to construct small, run-of-river hydropower projects that produce electricity from the natural flow of river water without the need for large dam or reservoir.

“Studies show that there is a 500-year seismic gap in the western Himalayas and 300 years in the eastern Himalayas with energy from continuous northward movement of Indian plate beneath the Eurasian plate storing up,” says Adhikari. A seismic gap is an active fault in a segment of a structure that has not slipped for a long time, compared with other segments.

“We don’t know the magnitude of the anticipated large Himalayan earthquake,” says Adhikari, a known disaster risk reduction expert. “In my view, we are not prepared for the consequences of failure of high dams and large reservoir-based hydropower projects along the whole Himalayan chain.”

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Ranjit Devraj is Editor at SciDev.Net.This article, produced by SciDev.Net’s Asia & Pacific desk, is published courtesy of Scidev.net.