With glacier retreat, permafrost melt, and extreme rainfall events, ICIMOD’s HIMAP report suggests that the countries of the Hindu Kush Himalayas have to start cooperating far more closely, or pay a huge price By Omair Ahmad Water in the Hindu Kush Himalayan (HKH) region is going through large and dramatic changes, caused by both climate change and human intervention, and the countries around it are unprepared for it. The stark message of the
Hindu Kush Himalayan Monitoring and Assessment Programme
(HIMAP), the most comprehensive analysis of what is happening in the HKH region, is one that concerns agriculture, hydropower, inland waterways, jobs, urbanisation, and international relations – some of the most sensitive and important issues in the region. These effects are complex, and will impact different regions differently, but some are already visible. Glacier retreat (and some advance) in the face of climate change will make the fragile mountains more prone to natural disasters such as landslides, and will make the impact of other natural disasters, such as earthquakes, far greater. Variations in rainfall will continue to rise, setting in place the possibility of catastrophic flooding, at the same time springs have been reducing their flows in the hills, and this may increase, leading to drought among communities that already have higher-than-national-average rates of poverty.
This will be a critical problem for India and Pakistan, who have both experienced devastating floods in their Himalayan regions, but it will have an immediate impact on Afghanistan, which experienced the worst drought of the century in 2018, primarily due to low snowfall early in the year. With no water-cooperation mechanisms with any country on its borders, Afghanistan will face increasing water uncertainty over the next decades with few tools to address it.
The eastern HKH region will experience the most glacier retreat. These are also the river basins – of the Ganga, Brahmaputra, and Mekong (as well as the Yellow and Yangtze in China) – which are the least reliant on glacier melt and snowmelt on water flow, accounting for less than 10 percent of the volume of water in the rivers. The hazards will largely be those faced by mountain communities – both of decreasing water during the summer months as well as the potential for landslides, GLOFs, and other related disasters. Given that 240 million people live in the HKH mountain communities, the risk to their lives and livelihoods will increase – both in the western and eastern Himalayas significantly. Hydropower – a dangerous wager The instability of the fragile HKH region – one of the youngest mountains in the world – will also pose a significant risk to hydropower projects. But because water flow in the region is unlikely to decline – and may marginally increase – until 2050 the incentive to build more of them is likely to remain. This is especially so since the HIMAP report states that there is a potential for 500 GW of barely tapped hydropower potential in the region, which is also critically energy-poor. There are large hydropower projects currently being
planned in the Indus
and
Brahmaputra
, with China playing an important role in both financing and development, particularly in Pakistan.
While the HIMAP report mentions some good practices emerging in the hydropower sector – from benefit sharing schemes with local communities to a push for more scientific understanding of environmental flows – these are far from established practice.
The other big infrastructural issue that will be impacted will be
India’s ambitious Inland River Waterways projec
t. With depots already being built in Nepal, this is a transboundary project that will involve not just the Indian lowlands, but also Nepal and Bangladesh, who will be key partners. With the risk of extreme weather events, combined with glacial retreat, the amount of debris and silt in the Ganga will rise, disrupting the flow of rivers as well as increasing the amount of dredging needed to keep waterways navigable for large freight carrying ships. “About one-third of the global sediment deposited to the oceans is estimated to be generated from the Tibetan Plateau and its neighbouring regions,” says the HIMAP report. Much of this is due to the fragile nature of the Himalayan range, and the monsoon system. While the former will not change, the number of extreme weather events due to climate change will add to the power of the latter. In the past – most
catastrophically in 2008
– rivers flowing through Nepal to India have radically changed their path due to build-up of silt, breaching embankments, leading to floods that have cost the lives and livelihoods in both countries. As the HIMAP report states, transboundary cooperation between India and Nepal has been marred by suspicion and blame-games. The addition of increased silt and debris into the river system is likely to exacerbate such tensions, unless key cooperation mechanisms evolve. Water dries up for agriculture The sector that will be impacted the most by variations in water will be agriculture. Of the eight countries in the region, seven use almost 90 percent of their water for agriculture (China uses 65 percent). There are four major sources of this water – the river systems, springs, groundwater, and rain. While the river systems are projected to supply the same amount of water up until 2050 (with maybe some increase), their variability of flow is likely to increase. More problematically the springs in much of the mid-HKH region seem to be drying up. The HIMAP report bluntly states, “Due to factors related to anthropogenic impacts (such as deforestation, grazing, exploitative land use resulting in soil erosion, etc.) and climate change (e.g., highly variable rainfall), springs fed during the monsoon by groundwater or underground aquifers are reported to be drying up and threatening whole ways of life for local communities in most parts of the mid–hills of the HKH.” The mountain regions already suffer from higher poverty rates than the rest of the countries, especially because infrastructure, and with it, access to services, is more costly to build. This will be added pressure on a region which is already deeply
food insecure
.