some perspective on the sustainability of hydropower.
Hydropower in a warming world
As one of my colleagues put it: “Sometimes bedrock slopes just fail; there’s no specific trigger.” There are well-documented incidents where hydropower dams have been damaged or destroyed without any link to climate change. An infamous example is the 1963 Vajont disaster in northern Italy, where a valley wall slid into a reservoir and generated a mega-tsunami that engulfed the impounding dam, killing more than 2,500 people downstream.
The precise causes have been debated since, but it is thought that as the reservoir was being filled with water, clay-rich layers in the valley side were saturated. This wet clay would have served as a naturally weak plane along which the landslide could move.
Other energy sources and their infrastructure carry their own inherent risks – think the Chernobyl nuclear power plant, or the Deepwater Horizon oil drilling rig. Many of the world’s power stations are vulnerable to climate change because of their proximity to the coast, with many threatened by rising sea levels.
It may never have been wise to develop hydropower at the site of the Chamoli disaster. This same valley had experienced large ice avalanches in 2000 and 2016 and has seen several major floods in recent years. It is of course extremely difficult to predict if, when and where these sorts of events might occur, but this is evidently an unstable landscape.
Scientists have developed a number of ways to monitor how landscapes are changing, particularly using satellite images. We have the tools to spot warning signs and develop hydropower as safely as can be reasonably expected. Tragically though, these tools are not always used, or the warnings are ignored, as seems to have been the case at Chamoli.
There is a cruel irony that hydropower can help countries reduce carbon emissions at the same time as dams are becoming increasingly vulnerable in a climate warming as a result of those emissions. We can develop this energy source safely, but it requires careful decision making, informed by research, and with continued monitoring of changing landscapes and the climate.
About the author: Simon Cook is a Senior Lecturer in Environmental Change at the University of Dundee
Suggested further reading
Huggel, C., Clague, J. & Korup, O. (2011). Is climate change responsible for changing landslide activity in high mountains? Earth Surface Processes and Landforms, 37, 77 – 91. https://doi.org/10.1002/esp.2223.
Xu, J. & Grumbine, E. (2014). Building ecosystem resilience for climate change adaptation in the Asian highlands. WIREs climate change 5, 709 – 718. https://doi.org/10.1002/wcc.302