The<a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof"> flood on the Bhote Kosi</a> on Tuesday morning was a timely reminder about the risks Himalayan communities face from melting permafrost and glaciers, as well as the need for transboundary early warning. In the spring of 2024, I visited the Kanchenjunga Conservation Area (KCA) again. While in the village of Kampuchen (4,145) I visited Nupu Sherpa, friend and owner of the Kampuchen White House Lodge, to share <a href="https://tc.copernicus.org/articles/18/711/2024/">a new paper we had just published</a> about a massive ice-debris avalanche that had occurred in 2022 in the upper Nupchu valley. Although Nupu was interested in the results and implications of the avalanche, he was even more concerned about the recent and rapid development of several large, pro-glacial lakes upon the terminus of the Kanchenjunga glacier, an hour walk north of Kampuchen and across the seasonal yak pasture of Ramdang Kharka (4,375m).&nbsp; Like many high altitude, low gradient glaciers in the Himalaya, those in the Kanchenjunga region had shrunk to mere shadows of their former selves during the previous 125 years, leaving behind debris-covered remnant ice and small meltwater ponds.&nbsp; Nupu’s fear was that the lakes might soon coalesce to form a large and potentially dangerous glacial lake. Given a large enough trigger, such as a massive landslide or avalanche, a glacial lake outburst flood (GLOF) could result that could damage Kampuchen, Ghunsa, Phale, the Kangchenjunga Base Camp trail, and even beyond to the lower Tamor into India.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071204070_31e28d1fd0f5a976ad96fc5597cc386586d7de5b7d9714835d5b479104209fed.jpg" data-media-id="editor_2" data-image-id="2025071204070_31e28d1fd0f5a976ad96fc5597cc386586d7de5b7d9714835d5b479104209fed" data-rendition-name="original" width="1500" height="1635" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>The Kanchenjunga Conservation Area (KCA), eastern Nepal.</figcaption> </figure>  Since I was on my way to the village of Lhonak (4,792m) I stopped to take a look at the new lakes. Sure enough, from a lookout point on the lateral moraine of the Kanchenjunga Glacier I could see as many as ten newly formed and growing meltwater ponds upon the terminal moraine region of the glacier.&nbsp; The prospect was reminiscent of early satellite images taken of Imja Glacier in 1962 by the French, showing a number of meltwater ponds that within 15 years had grown and merged into a glacial lake half a square kilometer in size and containing 45 million cubic meters of water. Ten years after that Imja had grown to more than a square kilometer in size, was at least 120 m deep, and contained an estimated, and growing, 90 million cubic meters of water. Would the same scenario play out for the lower Kanchenjunga Glacier? To try and understand the situation better, glaciologist Sonam Wangchuk of ICIMOD put together a time series composite of lake development over time, from 2016 to 2024, where it was clear that the majority of the new lakes had only formed since 2019.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071204078_c65a5ec574a251489c502f3efdf842033e0d238fd57947f7eee2c5793aac2a29.jpg" data-media-id="editor_3" data-image-id="2025071204078_c65a5ec574a251489c502f3efdf842033e0d238fd57947f7eee2c5793aac2a29" data-rendition-name="original" width="602" height="686" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>Time-lapse satellite images of glacial lake development from 2016 to present. Animation of the process can be seen at https://www.mdpi.com/article/10.3390/w17101457/s1.</figcaption> </figure>  Sonam Rinzin of Newcastle University estimated the potential depth and volume of the future glacier lake using standard procedures based upon the surface slope of the Kanchenjunga Glacier combined with volume-area curves for similar glacial lakes, estimating that the future lake would have a volume of approximately 33 million cubic meters of water and depth of more than 116 m. Other modeling methods enabled the mapping of probable ice, debris, and/or rock avalanches into the lake that could trigger a GLOF.&nbsp; A third model was then used to simulate four different avalanche scenarios that could trigger a GLOF: from small (debris avalanche of 3 million cubic meters) to the worst case (15 million cubic meters) of fast-moving debris. Even under the small magnitude scenario, avalanche-triggered outburst floods would travel distances of almost 120km downstream, and under the worst-case scenario the floods would reach the Indo-Gangetic Plain and cross the border into India, damaging or destroying up to 90 buildings and 44 bridges. The prospective triggers of a future GLOF, however, are not limited to a nearby rock avalanche. A <a href="https://tc.copernicus.org/articles/11/443/2017/tc-11-443-2017.html">sudden release of water</a> from water-filled caves further up the glacier could trigger a surge wave capable of breaching the terminal moraine complex holding in the lake water.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250712040716_20ed87368a9ac416b5d0232cf8e02211195ca6bc9fff960a1f7e43a95bdfbbf9.jpg" data-media-id="editor_5" data-image-id="20250712040716_20ed87368a9ac416b5d0232cf8e02211195ca6bc9fff960a1f7e43a95bdfbbf9" data-rendition-name="original" width="1500" height="1621" loading="lazy" alt="Meltpools"> <figcaption>Theoretical Kangchenjunga glacial lake of the future (blue) contained by a front moraine (purple) with a flood possibly triggered by a massive rock avalanche (red).</figcaption> </figure>  <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost">Weakening permafrost</a> at the highest altitudes could result in massive ice-debris avalanches, such as those believed to have triggered recent and catastrophic floods in the <a href="https://nepalitimes.com/here-now/remembering-the-seti-disaster">Seti River</a>, <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">Barun Khola</a>, <a href="https://nepalitimes.com/news/non-climate-cause-of-nanda-devi-flood">Chamoli</a>, <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">South Lhonak lake</a>, and Tuesday’s Bhote Kosi flood in <a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof">Rasuwa</a>. Weakening and eventual collapse of the terminal moraine complex through sub-surface piping could also result in an outburst flood. And a range of <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">cascading processes</a> currently unknown to scientists could trigger a flood as well.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250712040712_76336a4597c08dd735e57b09ae9840b6bd3d89c85907bb39424d9e6f3163581e.jpg" data-media-id="editor_13" data-image-id="20250712040712_76336a4597c08dd735e57b09ae9840b6bd3d89c85907bb39424d9e6f3163581e" data-rendition-name="original" width="740" height="565" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>Jannu glacier in 1899. Note how the level of the debris-covered glacier reached the top of the lateral moraines over a hundred years ago. Photo: V. SELLA</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250712040712_707dd365923a002e889c64a88796b445695ea9ca692ec639179bc70217ed63c5.jpg" data-media-id="editor_14" data-image-id="20250712040712_707dd365923a002e889c64a88796b445695ea9ca692ec639179bc70217ed63c5" data-rendition-name="original" width="5184" height="3888" loading="lazy" alt="Meltpools in the Himalaya"> <figcaption>Jannu glacier in 2022. The remaining debris-covered glacier is now several hundred meters below the crests of the lateral moraines. Photo: E. BYERS</figcaption> </figure>  But will a large and potentially dangerous glacial actually form at the Kanchenjunga glacier? There’s really no way to tell at this point, although the rapid development of lakes since 2016 is a strong indicator that a large lake is in the process of forming. And rather than wait and see, our current uncertainty does not diminish the need for a more proactive approach to the development of a large glacial lake at some point in the near future. For example, the lower Kanchenjunga Glacier clearly needs to be regularly monitored over the coming years to keep track of glacial lake growth and potential hazards. This could be done by the Department of Hydrology and Meteorology (DHM), ICIMOD, or Kathmandu University with results regularly shared with local people and local governments.&nbsp; In fact, such a service could be developed into a program that is offered to other communities throughout highland Nepal who experience similar situations of glacial lake development, growth, and prospective danger, especially since most communities presently feel that they have no one to turn to for similar information. Inexpensive, locally appropriate, user-friendly early warning systems (EWS) need to be developed for the Kanchenjunga region now, instead of waiting for a tragedy to happen. While the different options and costs are being assessed, the installation of new cell towers in the upper Ghunsa Khola would assure that local residents have access to one of the most effective and proven EWS systems available: cell phones, combined with a lake level monitoring device that broadcasts data and connects to cell phone alarm systems.&nbsp; For example, hundreds of lives were saved when upstream witnesses called their family and friends downstream to warn them of the <a href="https://archive.nepalitimes.com/article/nation/Anatom-of-a-Himalayan-tsunami,1330">Seti River flood</a> near Pokhara in 2014. New zoning policies that prohibit the construction of lodges and other infrastructure in high-risk floodplain regions need to be developed now. Where the infrastructure already exists, villages should be encouraged to install gabion rock-filled wire cages along susceptible river channel or river interfaces to divert the flow of water during a flood event, a method used successfully in both highland and riverine Nepal. Local and national hazard training and response programs need to be developed now. Several examples of excellent programs developed by different organisations in the upper Khumbu region exist that provide excellent models, such as those tested by the US Agency for International Development <a href="https://www.hillarymedal.com/Khumbu-Nepal-Local-Adaptation-Plan-of-Action-%20report.pdf">(USAID) and ICIMOD</a> between 2011 and 2015. Glacial lake reduction&nbsp; Nepal was recently awarded a $36.1 million award by the Green Climate Fund (GCF) to directly confront many of hazards from glacial lake outburst floods jointly implemented by the United Nations Development Programme (UNDP) and the DHM building on past successes at Tso Rolpa and Imja Lakes. There are some lessons learned over the past decades of field work based in Nepal and Peru: 1. The DHM wants to use the project to reduce GLOF risks in Kosi and Gandaki basins and glacial lake reduction programs are planned for Thulagi, Lower Barun, Lumding Tsho, and Hongu 2 glacial lakes.&nbsp; However, the planned lowering depth for Tso Rolpa in 2000 was 20m, with the project ending once 3m lowering was achieved due to lack of funds. Imja lake, which scientists also determined needed to be lowered by at least 20m, was in fact lowered by 3m in 2016 ‘because that’s what they did at Tso Rolpa’.&nbsp; If glacial lake reduction programs are to be implemented under the GCF program they should be based upon good science, and lowered to an effective depth, otherwise the activity will be a waste of funds. <a href="https://sinia.minam.gob.pe/sites/default/files/siar-%20ancash/archivos/public/docs/usaid_glacial_lake_handbookrfs_0-ilovepdf-%20compressed_0.pdf">Peru offers experience</a> for glacial lake lowering. 2. Although large glacial lakes (more than 1sq km) will always command the most media and even scientific attention, it has become abundantly clear in recent years that even small glacial lakes can be just as deadly, given the correct sequence of cascading events, rainfall, snowmelt, and/or other triggers.&nbsp; The 2017 <a href="https://link.springer.com/article/10.1007/s10346-018-1079-9">Barun flood</a> and September 2024 <a href="https://www.stimson.org/event/the-%20thame-glof-disaster-climate-related-disaster-risk-management-in-the-high-himalayas/">Thame flood</a> are two excellent examples. Methods for assessing the flood risk of glacial lakes will need to be revised accordingly to include many of these smaller glacial lakes as well, in addition to the 21 large lakes already considered to be dangerous. 3. Existing and expensive EWS might benefit by some consideration of cheaper, more local, and possibly more effective alternatives. In 2015, for example, <a href="https://digitalcommons.macalester.edu/himalaya/vol37/iss2/7/">villagers</a> living below Tso Rolpa complained that they had no idea how the recently installed EWS worked, what it sounded like, and what to do in the event that it went off. With improved cell service and real-time lake level monitoring apps, local people could check on the lake whenever they wished, as opposed to waiting for some kind of communication from Kathmandu. 4. The GCF grant has the opportunity to become the ‘go to’ place for communities throughout highland Nepal to report any of their concerns related to glacial lakes and/or other observed cryospheric processes. This service could facilitate local people’s ability to adapt to, mitigate, or prevent a range of climate change-related hazards largely unknown to previous generations. Alton C Byers is a faculty research scientist at the Institute of Arctic and Alpine Research (INSTAAR) University of Colorado at Boulder and has visited the KCA including a six-month residency in Ghunsa supported by the Fulbright Nepal Scholar Program. This article is largely based on Evolution of a Potentially Dangerous Glacial Lake on the Kanchenjunga Glacier, Nepal, Predictive Flood Models, and Prospective Community Response. <a href="https://doi.org/10.3390/w17101457">Water</a>, 2025. (Byers AC, Rinzin S, Byers E, Wangchuk S.)

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Meltpools in the Himalaya

<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52a49c7e80680e052308jpeg.jpg" alt="" width="2592" height="848"/><figcaption>Gabions above Chukung with the summit of Lhotse peeking through the clouds last month. All photos: ALTON C BYERS</figcaption></figure>In an example of local people adapting to the <a href="https://www.nepalitimes.com/banner/a-terrifying-assessment-of-himalayan-melting/">climate crisis</a> with little outside help, the people of <a href="https://www.nepalitimes.com/banner/on-thin-ice-in-the-khumbu/">Nepal’s Khumbu region</a> are building embankments to protect themselves from increasingly frequent floods coming out of melting glaciers upstream.While major glacial lake outburst floods (GLOFs) that destroy infrastructure get a lot of press, these local initiatives in remote and high altitude locations do not get much attention.While on a field survey of the impacts of the <a href="https://www.google.com/url?client=internal-uds-cse&amp;cx=011870630917993763279:opm7uqsat-4&amp;q=https://www.nepalitimes.com/here-now/on-everest-4-years-after-the-nepal-earthquake/&amp;sa=U&amp;ved=2ahUKEwjYya7W_efjAhUJinAKHZLsAcsQFjABegQIDxAC&amp;usg=AOvVaw0h7aKRfWj4B_kVdyZ1-PZZ">25 April and 12 May 2015 earthquakes</a> on three of Nepal’s potentially dangerous glacial lakes — <a href="https://digitalcommons.macalester.edu/cgi/viewcontent.cgi?article=2306&amp;context=himalaya">Imja, Tso Rolpa and Thulagi</a> – local lodge owners in Chukhung village (4,730m) talked of a mysterious flood from the <a href="http://archive.nepalitimes.com/news.php?id=16562#.XUYpei0Q0Wo">Lhotse Glacier</a>, immediately upstream, on 25 May that year.The USAID-supported study followed our recently completed High Mountain Adaptation Partnership (HiMAP) program, which worked with communities in the Khumbu and Cordillera Blanca of Peru to develop local adaptation plans of action based on concurrent glacial lake and climate change studies, which were routinely shared with local people.Further investigation revealed that the source of the Lhotse flood was the interior of the glacier itself, now similar to a massive piece of Swiss cheese, with hundreds of water-filled caves in the shrinking and <a href="https://archive.nepalitimes.com/article/nation/ice-to-water-glacier-lake-outburts-himalayas-nepal,4197">rapidly ablating glacier</a>. Many of the caves are linked to surface meltwater ponds that can drain rapidly, in some cases triggering the release of water from dozens of conduits that converge to create a major flood.<img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52a79c7e80680e052309jpeg.jpg" alt="" width="1000" height="989">Photo: GOOGLE EARTHThe 6m high wave generated by the May 2015 flood destroyed the bridge to Island Peak Base Camp and narrowly missed Chukung. It came in the middle of the night and, combined with the memory of the <a href="https://www.google.com/url?client=internal-uds-cse&amp;cx=011870630917993763279:opm7uqsat-4&amp;q=https://archive.nepalitimes.com/article/nation/melting-mountains-shake,3073&amp;sa=U&amp;ved=2ahUKEwjh7pL9_efjAhUDk3AKHWsyBAEQFjAIegQIBhAC&amp;usg=AOvVaw2mkMt6PodwsV2PgkTJG1uR">devastating earthquakes</a> the month before, caused widespread panic. Cell phone messages were passed rapidly down the valley.  People from Chukung to Lukla gathered their loved ones and carrying the elderly, ran for higher ground. They feared it might be a massive GLOF from Imja Tsho (5,010m), but in fact it was a smaller flood that impacted only the uppermost settlements.<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52aa9c7e80680e05230ajpeg.jpg" alt="" width="1500" height="1125"><figcaption> </figcaption></figure><figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52ad9c7e80680e05230bjpeg.jpg" alt="" width="1500" height="1125"><figcaption> </figcaption></figure>After the flood, local volunteers in the Khumbu Alpine Conservation Committee decided to begin building a dozen or more gabions, or rock-filled wire cages, immediately next to Chukung, on its southernmost side.A year later, on 12 June 2016, <a href="http://www.crwr.utexas.edu/video/Lhotse_Flood_Supplement_V3.mp4">a second and larger conduit flood</a> from Lhotse occurred, this time headed directly for Chukung. But the flood waters were successfully diverted by the gabions built the year before, resulting in only minor flooding of several lodge courtyards immediately next to the river.  Armed with the knowledge of their successful action, the community continued to devote its resources to construct more gabion walls along the glacial streams that run on the north and south sides of the settlement.<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52b09c7e80680e05230cjpeg.jpg" alt="" width="1826" height="507"><figcaption> </figcaption></figure>Yet another englacial conduit flood from the Lhotse Nup Glacier occurred a few weeks ago. Once again, there was minimal damage to the village thanks to the new gabions.With support from the Nepal Mountaineering Association, the Buffer Zone Council, local municipal government and their own resources, villagers have been able to fund and use effective local technology in response to what appears to be a new era of fairly routine flooding from the glaciers.Such phenomena <a href="http://archive.nepalitimes.com/news.php?id=16563#.XUYqJS0Q0Wo">have occurred for decades</a>, but never with the apparently increasing frequency of the past 10-15 years. Chukung probably should never have been built next to a vulnerable flood plain, but when most of the lodges were constructed 20 years ago, <a href="http://archive.nepalitimes.com/article/nation/melting-mountains-shake,3073">glacier floods</a> happened only every 30-60 years, not every year.<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52b39c7e80680e05230djpeg.jpg" alt="" width="980" height="735"><figcaption> </figcaption></figure><figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52b69c7e80680e05230ejpeg.jpg" alt="" width="979" height="733"><figcaption> </figcaption></figure><figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52b89c7e80680e05230fjpeg.jpg" alt="" width="960" height="716"><figcaption> </figcaption></figure>Such floods were so infrequent that in the mid-1950s, glaciologist Fritz Müller was nearly kicked out of the Khumbu by villagers angered over a large flood, most likely from Lhotse Nup Glacier, which destroyed half of Chukung’s grazing land as well as the prayer wheel ghatta at Phunki. They felt Müller had angered the gods by his research activities on the Khumbu glacier.Fortunately, the then 14-year-old abbot of Tengboche Monastery, the Venerable Ngawang Tenzing Zangpo Rinpoche, intervened on Müller’s behalf and all was forgiven. These days glacier floods happen nearly every year, but they rarely make the national news since they are so much smaller than the major GLOFs that destroy downstream infrastructure, they occur in high and remote locations, and sometimes escape the notice of even local people.<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52bb9c7e80680e052310jpeg.jpg" alt="" width="594" height="404"><figcaption> </figcaption></figure>The climate change adaptation demonstrated by Chukung has yet to make global news, but it is one more example of how Himalayan people themselves, with little or no help from the outside, are quietly <a href="https://www.nepalitimes.com/banner/weather-warning-for-climate-meeting/">adapting to the impacts of climate change</a> in real and effective ways.Bridges are being built higher to cope with more frequent and higher floods. Lodges and new infrastructure are built well above floodplains that until recently were considered to be safe. Many gabions are being built along river banks that only 10 years ago had none.And life in the high Himalaya goes on.<figure><img src="https://superdesk-pro-c.s3.amazonaws.com/sd-nepalitimes/20221108131156/636a52bd9c7e80680e052311jpeg.jpg" alt="" width="501" height="376"><figcaption> </figcaption></figure>Alton C Byers, PhD, is Senior Research Associate and Faculty at the Institute of Arctic and Alpine Research (INSTAAR), University of Colorado at Boulder, in the US.

Living below Nepal’s melting mountains

Where will Nepal be in 2050? It is only 25 years away. The country’s population will be peaking at 36 million, the poverty rate will drop to near zero. Maternal and child mortality rates will fall further. Nepal will be generating up to 40,000MW of hydro and solar power, more than half of that for export. Upgraded highways will improve connectivity, railways will make transport cheaper. Pokhara and Birganj will only be two hours away from Kathmandu. Nijgad airport could be Nepal’s new aviation hub, reducing Kathmandu’s congestion. Nepal will hitch its wagon to the engines of economic growth in India and China. Investment and job creation will reduce outmigration, Nepal's data centres will be powered with surplus electricity. Remote areas will prosper with high-value tourists. That is if all goes well. But if Nepal’s politics remains dysfunctional with incompetent leadership, then the country will muddle along as it is doing now. Society will be more unequal, public discontent may boil over as politicians resort to faith to hide failures, the exodus abroad of youth will continue. Climate breakdown will exacerbate these crises. Global average temperature will have risen to 2.7°C above pre-industrial levels (it is 1.1°C now). The remaining Himalayan icecap will shrink by half, glacial lakes will threaten valleys. The hydrology of rivers will change, reducing dry season flow. Severe and prolonged heat waves in the Tarai will force people to migrate back to the mountains. In the final analysis, it all boils down to a political system that is more accountable, and displays more integrity and efficiency. <h2>Mission 2050</h2> · Melamchi Water Supply Project · Pokhrara International Airport · Bhairawa International Airport · Upper Tama Kosi Hydroelectric Project . Kathmandu-Tarai Expressway What do these biggest infrastructure projects in Nepal have in common? All ended up being more expensive than they should, all have been delayed and are not fully operational, two were badly damaged in climate-related disasters that should have been foreseen. The $800 million Melamchi is Nepal’s most expensive infrastructure project to date. It took 30 years to build, but was nearly destroyed by a glacial debris flow in June 2021. The headworks need major repairs. The 456MW Upper Tama Kosi was severely damaged by a rockfall and floods in last September’s floods. It is still not operating at full capacity, and other hydropower plants were damaged in recent glacial floods. Pokhara and Bhairawa airports were supposed to be the new aviation gateways to Nepal to take the pressure off Kathmandu, and become game changers for tourism and pilgrimage. Nearly three years later, both handle domestic flights. Poor and inadequate design, kickbacks on contracts, cost overruns, failure of diplomacy to get India’s nod on air routes, and lack of planning and marketing have made the airports a pair of white elephants. Some of these setbacks can be blamed on natural calamities, but mostly it is political incompetence and greed, lack of accountability and poor implementation. That is no surprise, since these are the hallmarks of doing business in Nepal, often delaying projects, adding to the cost, and even when completed they are already outdated. That is the story of the last 25 years, are the next 25 going to be any different? Not if governance does not improve. “What we really need for the future is vision, idea, and understanding, and then the domestic capacity to implement them,” says infrastructure expert Surya Raj Acharya, who laments the total absence of technical and planning expertise. “None of our national highways meet technical standards, our cities are unplanned. The priority was never on quality. Politicians sold us short-term infrastructure that have now become a barrier to prosperity,” he adds. One silver lining has been private sector involvement in hydropower, and the energy strategy aims to generate 11,769MW by 2030. But hydropower is high-investment, high-risk due to climate breakdown, and ecologically damaging. “Hydropower is a good example of how government incentives and public-private partnership can work wonders, although we now have to take climate change into account,” explains economist Kalpana Khanal of the Policy Research Institute. She adds, “We now have to identify other key infrastructure areas that also enhance the growth of other sectors.” The National Planning Commission’s periodic plans guide overall social and economic strategy for the country into the coming decade. Nepal’s current five-year plan (2024-2029) has set a target of 7.3% annual economic growth against the current 3.9%, $2,351 per capita income up from $1,456 at present, and poverty reduction to 12%. The plan aims to export nearly half the hydropower generated by 2030, earning the country Rs41 billion annually. But there is no real coordination between line agencies, and bureaucratic lethargy leads to constant delays, says former member of the National Planning Commission (NPC) Min Bahadur Shahi. “Development in Nepal is still very much synonymous with building roads and bridges, and infrastructure is rudimentary,” he says. “Elsewhere in the world, digital infrastructure and governance go hand in hand, we are far behind.” The frustration of a man who served in the National Planning Commission is an indication where the problem lies: in actually executing plans and implementing strategies. “We need to prioritise projects based on our geography, climate, societal needs,” Shahi continues. “We want to push Nijgad airport when we can’t even operate Pokhara and Bhairawa. Have we even studied potential air routes and needs of international carriers?”  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250726070744_0547e5a7fd4424b5de8c279cab637ee7ebd9e65f2673b15e6dbd4eb2aa2524f2.jpg" data-media-id="editor_0" data-image-id="20250726070744_0547e5a7fd4424b5de8c279cab637ee7ebd9e65f2673b15e6dbd4eb2aa2524f2" data-rendition-name="original" width="3600" height="2400" loading="lazy" alt="Pokhara airport"><figcaption>NO FLY ZONE: Pokhara airport was supposed to be the new aviation gateway to Nepal but nearly three years after its inaguration, it mostly handles domestic flights. Photo: RADHIKA KANDEL </figcaption></figure>  TARGET PRACTICE Export of hydropower, manpower and lately information technology are the mainstays of Nepal’s economy, and will carry the country to its graduation from Least Developed Country status to a developing country in November 2026, and hopefully to middle-income by 2030. Nepal has an installed capacity of about 3,800MW, most of it from hydropower, and increased adoption of electric cars has reduced the import of petroleum products, decreasing the trade deficit with India. Meanwhile, Nepalis abroad sent home $11 billion in remittances last year, and at least $900 million in backend IT exports. But demographer Yogendra B Gurung is not impressed: “Despite the reduction in the poverty rate, and our improving income status, life expectancy, income, even maternal and infant mortality are not on par with countries with similar economic status.” He says relying on remittances is an unsustainable economic model, vulnerable to external factors and remittances are mostly spent on day-to-day needs, and not invested in productive sectors. Remittance is credited with reducing poverty in Nepal which is down to 20.27% from 42% in 1990. Money sent home by workers abroad has allowed families to afford basic healthcare and education, in turn helping to reduce childhood malnutrition and maternal mortality while improving female literacy. But the progress has stalled in recent years, and many doubt Nepal will meet its Sustainable Development Goals (SDGs) targets. The National Planning Commission has said Nepal is likely to achieve just 60% of the targets by 2030. Sex ratio at birth, which is 112 boys to 100 girls in Nepal in particular, is worrying, as it is much higher than the biological ratio of 105 to 100. This is much more pronounced in Karnali, Sudurpaschim and Madhes Provinces which suffer from historical neglect. Despite a rise in female literacy, patriarchy is still deeply entrenched and the provinces are behind the rest of the country for gender equality, education, healthcare, nutrition and economic opportunities. “Karnali is resource-rich, especially hydropower and the recent discovery of the methane gas, but inequality is much greater,” says Shahi, who is with the Karnali Integrated Rural Development and Research Centre (KIRDARC). “Federalism in Nepal is only on paper, we need a total structural reform to devolve political power to really bring about change.”  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250726070744_fd4a218656e1fbf6f13f5f87a47bfe624516c6a0232481b6be77875ae866deb9.jpg" data-media-id="editor_1" data-image-id="20250726070744_fd4a218656e1fbf6f13f5f87a47bfe624516c6a0232481b6be77875ae866deb9" data-rendition-name="original" width="3600" height="2400" loading="lazy" alt="Butwal-Narayangadh "><figcaption>The Daunne section of the Butwal-Narayangadh road notorious for traffic jams and accidents, it has been in never-ending construction for three years. Photo: BISHNU PRASAD GAUDEL / RSS </figcaption></figure>  Despite limited resources, Nepal also suffers from wasteful investment as a result of politically (mis)guided decision-making, instead of people-centric plans and policies, says demographer Gurung. “People are overwhelmingly moving to the cities but our leaders are hell bent on building roads to every village and now there are empty schools in the mountains,” he adds. Nepal needs data-driven planning but its long-term economic vision 2020-44 seems more of a wish-list than realistic goals, including average annual GDP growth of 10.5%, $12,000 per capita income and population under the absolute poverty line at 0. Other goals include raising electricity generation capacity to 40,000MW, access to motor transport to 99%, life expectancy at birth to 80, maternal mortality down to 20% and literacy to 99% and 100% access to the internet, among others. Meanwhile, Nepal is committed to net-zero by 2045 and 100% renewable energy by 2050. “Our planners have no idea what kind of infrastructure we need 20, 30 years down the line to sustain and accelerate growth. We need a big structural change in the political leadership, in technocratic planning, and for policy implementation,” says infrastructure expert Surya Raj Acharya. Meeting such targets would require large investment, and it would be unwise to rely on remittances for the longer run, especially as Nepal’s demographic dividend will diminish as it turns into an aged society by 2065. Reversing out migration requires a favourable investment climate so jobs are created. Good governance marked by accountability and transparency are the basic prerequisite for ease of doing business. But lack of rule of law and illicit funds put Nepal in the grey list of the Financial Action Task Force (FATF), the global money-laundering watchdog. “Everything comes down to a political will. The established parties must realise that if they don’t perform, they will be replaced by alternatives,” says Kalpana Khanal. “In the meantime, we must engage the youth and find ways to retain them as well as attract the diaspora to invest in Nepal.”

Nepal in 2050

MetLife Nepal has signed Rohit Paudel and Indu Barma, the captains of the national men’s and women’s cricket teams, to promote the importance of life insurance.

Metlife signs Nepal cricket captains

Many of us former Nepal Peace Corps volunteers (PCVs) would agree that our time in Nepal changed in significant but very different ways our perspectives on life if not the future paths we chose to follow. Of no one was this truer than Dorothy Mierow. Dorothy was born in 1920, in Colorado Springs. Her father Charles C Mierow was a classics scholar and Latin professor, who served for ten years as president of Colorado College.&nbsp; Dorothy developed an interest in animals as a child, graduated with a BA degree in natural history from Carlton College in 1942, a Master’s in biology from the University of Pittsburgh, and another Master’s in geography from the University of Minnesota.&nbsp; As a young woman, Dorothy traveled with her father throughout Europe, including a visit to ancient Greek ruins, and took a Magellan Tour by cruise ship around the world in 1958.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071901074_0bad133ab22aada319e74bbad95d563e191371db291c08f373839fbd15440262.jpg" data-media-id="editor_0" data-image-id="2025071901074_0bad133ab22aada319e74bbad95d563e191371db291c08f373839fbd15440262" data-rendition-name="original" width="903" height="1178" loading="lazy" alt="How the Peace Corps changed a volunteer's life"> <figcaption>HOME AWAY FROM HOME: Dorothy Mierow as a college student in her native Colorado.</figcaption> </figure>  She was a college teacher during much of the 1940s, also teaching at a girls’ school in Hawaii. Then back to her native Colorado in 1953, where she became a curator and later director of the Colorado College Natural History Museum. She taught geography classes, and in her free time, Dorothy climbed 22 of Colorado’s 14,000-foot peaks. Traveling in India in 1960, Dorothy decided to spend two weeks in Nepal. In late 1961, she filled out an application to join the Peace Corps and specified that she wanted to go to Nepal, ‘because I admired the people so much when my father and I were there on our trip’.&nbsp; Dorothy reached Kathmandu in September 1962 as the first group of American Peace Corps volunteers in Nepal. She stood out from the others: one of the few women in that group, surely the oldest at age 41, a world traveler, and a woman who already had established a professional career.&nbsp; One doubts if Dorothy had had a husband and children whether she would ever have gone to work and spend much of the rest of her life in Nepal.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071901078_68e84ade1ffb0f6c83c7f8fa5c1e7315b5f6c543217f96cde012e4d86f171515.jpg" data-media-id="editor_1" data-image-id="2025071901078_68e84ade1ffb0f6c83c7f8fa5c1e7315b5f6c543217f96cde012e4d86f171515" data-rendition-name="original" width="1259" height="910" loading="lazy" alt="How th Peace Corps changed a volunteer's life NT"> <figcaption>Pokhara Bazar in 1962.</figcaption> </figure>  The Peace Corps assigned Dorothy to teach geography at Tri-Chandra College. After the school closed in the winter due to lack of heating, USAID and the College of Education asked Dorothy to help train general science teachers.&nbsp; She taught for two months and became involved in a textbook-writing project, commenting: ‘I would like the children to know something about public health, conservation (the trees are going fast and so is the soil), and learn the names of some of their common birds, trees, and flowers. They are more impressed with electricity, airplanes, and cell structure.’ When a new college opened in Pokhara in 1963, Dorothy was transferred there and lived with a Nepali family. The college boasted 30 students and no permanent buildings.&nbsp; In October 1963, Dorothy wrote: ‘Pokhara is a town of almost 5,000 people … We are in a fertile valley surrounded by foothills … There is a small Mission Hospital … a Leper Hospital and Tibetan Refugee Camp started by the Red Cross and now run by the Swiss. With winter approaching, more Tibetans are appearing in town, often with pack horses or donkeys. Some have been carrying large boxes of powdered milk,donated (by USAID) to the camp from the airport … There is no electricity, and the transportation problems make many items scarce and expensive. I am really a sort of a museum. The landlord brings all kinds of people in to see how I live and count my shoes and dresses. They express amazement at my books, pictures, tin oven, Nepali dolls from Kathmandu, screened food shelves and curtained closet.’ The standard term for Peace Corps volunteers was two years, but Dorothy extended her term and was still at Prithvi Narayan College at the end of 1965, when she wrote that she had 20 Geography students in the first-year class and 6 in the second year preparing for the IA Examination. The college enrollment was 125 students, and the foundation for a new science building was being excavated.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071901074_c6a80e5e0db0c705b2f8733c6d30dc0386fe3abbd2238ea9d947b7d746f94a29.jpg" data-media-id="editor_2" data-image-id="2025071901074_c6a80e5e0db0c705b2f8733c6d30dc0386fe3abbd2238ea9d947b7d746f94a29" data-rendition-name="original" width="902" height="605" loading="lazy" alt="How the Peace Corps changed a volunteer's life"> <figcaption>Mierow and friends at Phewa Lake.</figcaption> </figure>  Dorothy noted that she ate one meal a day at the (Shining Mission) Hospital but otherwise lived on dal-bhat, momo, and potato curry at local shops. However, she had developed a new passion: to build what she initially called the Pokhara Museum of the Himalaya. In commendable Peace Corps fashion, Dorothy always worked with Nepalis and respected the culture. ‘The greatest joy and satisfaction I have had has been from the building of a Museum-Library in memory of my parents … It has been possible to feel like a wealthy benefactor with the money saved by father for the family’s education and now available for the education of others… (Father) would have loved to be in on the founding of a new college and be able to plan a library. Several hundred of the books to be in the museum-library came from his collection and were carefully selected to be of use for students in Nepal…’&nbsp; ‘The museum part is to satisfy my own inclinations and was thought of when I found how little diversion there was for the people of Pokhara… It is part of the University requirements for the college that it should have a geography and biology museum. The museum building is small but adequate.&nbsp; I have tried to design it in harmony with Nepalese architecture and decorate it with some of the art of the best artists or woodcarvers… Posts holding up the porch roof are carved by Cottage Industries to represent different peoples of Nepal in typical costumes. The door was carved by a local wood carver and has typical birds of Nepal around it. Inside are 10 roof-support carvings designed by the retired Director of the National Museum in Kathmandu, Mr. C.M. Maskey.&nbsp; They were carved by the best wood carvers in Patan very skilfully. The building has three rooms: the library, the exhibition room, and a smaller workroom which can be used by our newly formed Woman’s Club as well as other groups or classes.’  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071901074_03d3359c65389d30a0134e9a4862778994121e7e833b7d28b18e06e36fc76ff8.jpg" data-media-id="editor_3" data-image-id="2025071901074_03d3359c65389d30a0134e9a4862778994121e7e833b7d28b18e06e36fc76ff8" data-rendition-name="original" width="629" height="599" loading="lazy" alt="How the Peace Corps changed a volunteer's life"> <figcaption>Mierow with local women in Pokhara in 1969.</figcaption> </figure>  Dorothy promoted her project to influential Nepalis connected with organisations whose support she solicited: The Department of Archaeology, the Department of Agriculture, the Godavari Botanical Gardens; Tribhuvan University’s Science and Education Department, Nature Conservation Society.&nbsp; The museum was opened officially in early 1967. The Annapurna Natural History Museum, the building Dorothy designed and had constructed, is still open and features some exhibits which she created many years ago.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071901074_54326a8a0685e980e782378076de2f5cd02d2426e9b0d94eed972d3dbe83af26.jpg" data-media-id="editor_4" data-image-id="2025071901074_54326a8a0685e980e782378076de2f5cd02d2426e9b0d94eed972d3dbe83af26" data-rendition-name="original" width="1333" height="1000" loading="lazy" alt="How the Peace Corps changed a volunteer's life"> <figcaption>The Annapurna Natural History Museum.</figcaption> </figure>  Dorothy returned to America in 1967, but she longed for Nepal. In the spring of 1969, she again tried to enroll as a Peace Corps volunteer but was told that as she had spent more than four years, she would not be eligible for another assignment. Undeterred, she persuaded the college in Pokhara to invite her to return as a teacher.&nbsp; UNICEF and the Forestry Department sponsored Dorothy to prepare charts on trees, birds, animals and flowers in colour for distribution to the schools of Nepal. Dorothy, back in the Peace Corps, returned to Pokhara and the Museum in 1972. She formed a friendship with her former geography student from Sikles, Chandra Prasad Gurung, and in 1974, she brought Chandra to America, where he enrolled in Colorado College and studied cultural anthropology.&nbsp; Chandra subsequently earned his PhD in geography from the University of Hawaii and returned to Pokhara to become director of the Annapurna Conservation Area Project. Gurung actively promoted ecotourism, landscape conservation, and biodiversity conservation in Nepal. His life was cut short along with those of 23 other Nepalis and foreigners who perished in a helicopter crash near Taplejung in September 2006.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025071901074_322d3c3ac6f1b08ffa07c44a19998b937a7db9eb43527f7539cf6481e1546314.jpg" data-media-id="editor_5" data-image-id="2025071901074_322d3c3ac6f1b08ffa07c44a19998b937a7db9eb43527f7539cf6481e1546314" data-rendition-name="original" width="2500" height="1000" loading="lazy" alt="How the Peace Corps changed a volunteer's life"> <figcaption>Mierow's four books on Nepal and its biodiversity. </figcaption> </figure>  Dorothy worked with several well-known Nepalis to publish her paintings and photos in beautifully illustrated books. She and Hemanta Mishra of the National Parks and Wildlife Service wrote Wild Animals of Nepal (Ratna Pustak Bhandar, 1976). More than 400 photos Dorothy took on treks to the Everest region, Gosaikunda, Muktinath, Jumla and Rara Lake, as well as travels in the Tarai, appeared in Himalayan Flowers and Trees (Sahayogi Prakashan, 1978).&nbsp; The botanist Tirtha Bahadur Shrestha identified the species. Dorothy and Kesar Lall published This Beautiful Nepal (Sahayogi Press, 1981). Birds of the Central Himalayas (1988) contained Dorothy’s paintings of 250 species of birds found along the areas of the Kali Gandaki River, Pokhara, Chitwan and the central Tarai. Dorothy summed up her life and work in Nepal in Thirty Years in Pokhara (Pilgrims Book House, 1997). Dorothy returned to Pokhara and her adopted Gurung family several times during the 1980s and 1990s to celebrate festivals and meet old friends. Her final years were spent at her mountain cottage in Green Mountain Falls north of Colorado Springs. She died at the age of 79 in August, 2000. Nepal gave new meaning and purpose to Dorothy Mierow’s life. Daniel W Edwards was a Peace Corps volunteer in 1966 and is the author of several books on Nepal. The author thanks Special Collections, Tutt Library, Colorado College.

How the Peace Corps changed a volunteer’s life

· On the night of 15 May, two glacial lakes burst in Tharka in Humla and the debris flow washed away homes and bridges.&nbsp; · Last week, a slurry surge on the Kali Gandaki in Upper Mustang caused at least Rs15 million in damage, and was traced to a melting glacier. · Dozens are feared dead after <a href="https://nepalitimes.com/news/rasuwa-flood-likely-a-glof">an expanding glacial lake in Tibet overflowed</a>, sweeping down into Nepal and damaging four hydropower plants generating 230MW, nearly 8% of the country’s total grid supply.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250718060748_45225dc707c1e9c2968ca8dbf6e564e01e4eb6e2ff254fb8eb940cf62cdd910b.jpg" data-media-id="editor_1" data-image-id="20250718060748_45225dc707c1e9c2968ca8dbf6e564e01e4eb6e2ff254fb8eb940cf62cdd910b" data-rendition-name="original" width="2667" height="1500" loading="lazy" alt="Rasuwa flood"> <figcaption>Miteri friendship bridge connecting Nepal and China was swept away in the Rasuwa flood. Photo: PRAKASH CHANDRA TIMILSENA / NPL</figcaption> </figure>  And those are just in the past month. Climate scientists say Himalayan glacial lake outbursts are becoming more frequent and destructive, and a warning for Nepal not to put all its eggs in the hydropower basket.&nbsp; <a href="https://nepalitimes.com/editorial/when-it-rains-it-pours-ksqprbu3">Record precipitation last September</a> unleashed floods that killed 200 people, and temporarily slashed Nepal’s total generation capacity of 3,000MW by nearly half. The <a href="https://nepalitimes.com/banner/nepal-valley-suffers-quadruple-disaster">Melamchi flood of 2021</a> caused by <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost">permafrost melting</a> on a glacier upstream nearly destroyed a $800 million water supply scheme, Nepal’s largest infrastructure project which four years later still has not resumed full operation. The <a href="https://nepalitimes.com/news/sikkim-flood-is-warning-to-nepal">glacial lake overflow in Sikkim</a> caused by record rainfall in September 2023 that destroyed the $1.2 billion Chungthung Dam and caused catastrophic damage to infrastructure on the Teesta River. This was a warning to the cascade of hydropower plants on the Arun and Marsyangdi river basins.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250718060736_6f61797a6be308321e3bae26e55d2f64cba4b9e5eb262adacb9e92fb5f3c6152.jpg" data-media-id="editor_6" data-image-id="20250718060736_6f61797a6be308321e3bae26e55d2f64cba4b9e5eb262adacb9e92fb5f3c6152" data-rendition-name="original" width="919" height="549" loading="lazy" alt="hydro disasters and hydropower plants"> </figure>  Nepal has set a target of generating an additional 28,500MW by 2035 -- out of the feasible 48,000MW -- but how viable is an energy strategy that is exposed to heightened risk due to climate breakdown? &nbsp; “As extreme weather events increase, we must design and build infrastructures respecting river flow and topography,” says former Energy Secretary Dwarika Nath Dhungel. “We must make the best use of our water resources, but not by letting excavators loose everywhere mining riverbeds and building haphazardly where we shouldn’t.”&nbsp; Although no project can be disaster-proof, <a href="https://nepalitimes.com/banner/climate-smarter-himalayan-infrastructure">climate smart design</a> can minimise damage from flash floods and landslides. Recent disasters have driven up insurance premiums for energy projects in Nepal, and smaller ones cannot even afford them. The 456MW Upper Tamakosi hydroelectric project which is still not fully functional after the September floods has claimed insurance worth Rs1.8 billion. The alternative to high risk high investment hydropower projects is <a href="https://nepalitimes.com/here-now/what-s-cooking-in-nepal-besides-politics">energy diversification</a> to other renewables such as solar, wind or biogas. Nepal gets annual sunlight of 300 days with 6-7 hours on average to total 50,000 terawatt-hours (TWh) per year.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250718060744_4acd452b4117180ca9bb5d3be839ff46dfd5464e4d507f5ad3704cef6253bc48.jpg" data-media-id="editor_9" data-image-id="20250718060744_4acd452b4117180ca9bb5d3be839ff46dfd5464e4d507f5ad3704cef6253bc48" data-rendition-name="original" width="1080" height="720" loading="lazy" alt="solar power"> <figcaption>Farmers in Tarai using solar powered water pump. Photo: GHAMPOWER</figcaption> </figure>  The Solar and Wind Energy Resource Assessment (SWERA) calculates that Nepal could source 3,000MW from wind energy alone, considering 10% of the area with more than 300W/m2 wind power density. <a href="https://nepalitimes.com/opinion/people-power/decentralising-power-in-nepal">Solar energy</a> stations are cheaper and quicker to build, and would be an ideal alternative to reliance on hydropower.&nbsp; “There has been some investment in solar power, especially from the state sector,” says water expert Madhukar Upadhyay. “But there is an issue of land acquisition since the arrays need a lot of space. It is comparatively easier to get a permit to put up a hydropower plant on a river.” As for biogas, there is simply no incentive to build on past success with household level plants to <a href="https://nepalitimes.com/here-now/more-bullshit">promote industrial-scale production</a>. Scaling up biogas by integrating it with urban biodegradable waste would still be a viable alternative to LPG.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250718060744_715d44afd5eb4ba8dafa209b0ad0f19400665797b5f078f5636821e600f96684.jpg" data-media-id="editor_12" data-image-id="20250718060744_715d44afd5eb4ba8dafa209b0ad0f19400665797b5f078f5636821e600f96684" data-rendition-name="original" width="1419" height="954" loading="lazy" alt="windmill"> <figcaption>A wind mill in Hapsikot in Nawalpur. Photo: WINPOWER NEPAL</figcaption> </figure>  Nepal’s public sphere is buzzing with excitement over the discovery of potentially 430 billion cubic metres of methane gas beneath Dailekh district that, if properly harnessed, would meet the country’s energy demand for the next 50 years. Even though a feasibility study is awaited, politicians from the prime minister down see this as a petro bonanza that will make Nepal rich. But drilling, storage and distribution of CNG in the country’s current kleptocratic state make that unlikely. If Nepal was to get rich solely on its hydro-energy potential, it could have done so in the past 50 years. Says Dhungel: “This is not exactly a new discovery, but it is premature to celebrate until its extraction is proven to be cost effective. And let us hope it does not get <a href="https://nepalitimes.com/news/balance-of-power">tangled in geopolitics</a>, since China is involved in the prospecting and drilling, which could make India uneasy.”&nbsp; The country suffers from the Dutch Disease curse even before its resource is fully exploited. And the same cronyism, corruption and rent-seeking structure cannot deliver the riches we expect from Dailekh’s methane discovery. Now, <a href="https://nepalitimes.com/here-now/right-climate-for-nepal-s-energy-transition">with hydropower in jeopardy</a>, Nepal’s planners will have to evolve a new strategy for energy security into the future. But first, governance needs to be cleaned up with long-term strategic planning that takes climate risk into account. For example, do we need to mine fossil gas when there are renewable options? Will Dailekh take Nepal away from its climate commitments? Says Madhukar Upadhyay: “Nepal has always been resource rich and management poor. And the larger the resource, the bigger our management incapacity. It is a societal malaise.”&nbsp;

glaciers-lake-outburst-flood

Meltpools in the Himalaya

Living below Nepal’s melting mountains

Nepal in 2050

Metlife signs Nepal cricket captains

How the Peace Corps changed a volunteer’s life

Nepal’s Resource Curse