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.)

original

674x448

610x380

500x500

400x266

400x240

400x203

301x200

1250x600

1084x550

thumbnail

viewImage

Meltpools in the Himalaya

<a href="https://nepalitimes.com/banner/including-local-knowledge-to-study-climate-change">Alton Byers</a> has organised frequent research expeditions to the Himalaya for more than 50 years. Recently, he returned to the <a href="https://nepalitimes.com/banner/tracing-past-glacial-floods-in-kangchenjunga">Kanchenjunga region</a> which he has visited three times since 2019. His team was there to gather more data for an ongoing study of glacial, ecological and socioeconomic changes in the region. But, his attention was soon diverted when a young man from the local community told Byers that locals had noticed large meltwater ponds forming at the toe of the <a href="https://nepalitimes.com/here-now/saving-kangchenjunga">Kanchenjunga</a> Glacier, upstream from Ghunsa and Kambachen. “He asked if we could go take a look at it,” Byers said. “We were on our way up to the Kanchenjunga base camp, so we made a detour. Sure enough, you could see these considerable lakes, perhaps a half-a-square-mile and growing.” Byers sprung into action. First, he interviewed other community members about the ponds — they confirmed the observations and growing concern. Then, over the ensuing months, he assembled a team of experts to conduct a study of how the ponds were changing. <a href="https://www.mdpi.com/2073-4441/17/10/1457#:~:text=This%20study's%20modeling%20results%20suggest,Ghunsa%20in%20the%20form%20of">The study was published in the journal Water earlier this month</a>. The paper outlines a number of potentially dangerous flood scenarios that could be triggered at the site in the future. The researchers urge regional authorities to implement mitigation measures, including a monitoring program and an early warning system for flooding.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030756_e4eda873993e7aa17a2e90dc95a162c85e4dc4627f6251ee8a9543681e3367b3.png" data-media-id="editor_4" data-image-id="20250708030756_e4eda873993e7aa17a2e90dc95a162c85e4dc4627f6251ee8a9543681e3367b3" data-rendition-name="original" width="1967" height="2128" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Predicted future Kanchenjunga proglacial lake extent and depth, frontal moraine, and potential avalanche location, which were used as input for modeling the GLOF cascade in r.avaflow. The background image is from Google Earth Imagery taken on 25 December 2020.</figcaption> </figure>  Byers’ first call for collaboration was to <a href="ttps://www.icimod.org/team/sonam-wangchuk/">Sonam Wangchuk</a>, an expert in snow and ice research via satellite imagery at the International Centre for Integrated Mountain Development. The images were striking. From 2022 to 2024, the ponds grew from puddles to large, interconnected bodies of water.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030740_d60cec33fe26074cb49a6a7c4d8f42ef8870c63f606c945d60fc3bf0327b1a3b.png" data-media-id="editor_6" data-image-id="20250708030740_d60cec33fe26074cb49a6a7c4d8f42ef8870c63f606c945d60fc3bf0327b1a3b" data-rendition-name="original" width="1861" height="2126" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Evolution of supraglacial lakes on debris-covered glacier (27.7726, 88.0187) at Kanchenjunga. Time series satellite composite images were acquired by Sentinel-2 Multispectral Instrument between September and October, with the exception of the April–May 2024 images. Two large and distinct lakes which expanded rapidly in 2022 and continued to grow in 2023 and 2024 are labeled as 1 and 2, for locational comparison with the oblique view taken on 25 May 2024. Photo: ALTON BYERS</figcaption> </figure>  “It’s sort of an indicator of how these melting processes are accelerating,” Byers said. Next, Byers and collaborators estimated that the meltwater ponds could form a large glacial lake. That lake, if it forms, will be vulnerable to <a href="https://nepalitimes.com/here-now/nepal-s-mountains-are-melting">outburst flooding</a>, which could be triggered by melting processes, structural collapse or rockfall from surrounding slopes. Finally, the researchers focused their efforts on modeling potential floods. They identified four scenarios, from small to large.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030744_ecafcf2013548954fcd0c76ce9ab299d68222fae99892d168dcba70f0fd802ae.png" data-media-id="editor_8" data-image-id="20250708030744_ecafcf2013548954fcd0c76ce9ab299d68222fae99892d168dcba70f0fd802ae" data-rendition-name="original" width="2637" height="3197" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Flood extent under various scenarios: areas impacted by all four GLOF scenarios are labelled as 4, those affected by three scenarios as 3, by two scenarios as 2, and by only one scenario as 1. (B) Hydrograph generated from GLOF modeling in r.avaflow and used as the input flow data for modeling each GLOF scenario in HEC-RAS. Flow depth and velocity at Kampachen (C,D) and Ghunsa (E,F). Discharge rate and time of peak, and flow arrival at Kampachen (G) and Ghunsa (H) under different scenarios.</figcaption> </figure>  Under the mildest scenario, the flood surge would travel 100km down the Tamor River, and under the worst-case scenario it would travel at least 220km with impact on houses and bridges, livestock, crops and tourism infrastructure. Byers warns that without adequate preparation, glacial outburst flooding can be deadly. The paper advises local and regional authorities to take measures to prevent a flood originating from the study site. Their recommendations include establishing early warning systems for flooding, partnering with research organisations in Kathmandu to monitor the site and adapting zoning laws to prevent new buildings in flood zones.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708030748_dccee85332d2844413dc5693050899b4bc49a25f9c66abc6b1ac1f5a80786d58.jpg" data-media-id="editor_9" data-image-id="20250708030748_dccee85332d2844413dc5693050899b4bc49a25f9c66abc6b1ac1f5a80786d58" data-rendition-name="original" width="1356" height="668" loading="lazy" alt="Mapping Kangchenjunga glacial flood risk"> <figcaption>Imja Lake, a glacial lake in the Mount Everest region of Nepal, began as meltwater ponds in 1962 and now contains 90 million cubic meters of water. Its water level was lowered to protect downstream communities. Photo: ALTON BYERS</figcaption> </figure>  Read also: <a href="https://nepalitimes.com/multimedia/the-not-so-permanent-frost">The not-so-permanent frost</a>, Wilfried Haeberli and C Alton Byers One of the cheapest and most effective early warning systems is deceptively simple: cell phones. Says Byers: “Not everyone can afford multi-million dollar early warning systems that rely on laser readings of water depth. But, studies have shown that cell phones, at least during the daytime, are one of the better early warning systems out there.” Byers hopes the study can help the same people that brought the issue to his attention: “The goal was always to share the research with the local community. Then they have all of the information they need to make the best decisions possible.” <a href="https://www.colorado.edu/instaar/2025/05/27/researchers-model-dangerous-glacial-lake-himalayas-and-propose-solutions">Gabe Allen</a> is Senior communications specialist at the Institute of Arctic and Alpine Research at the University of Colorado Boulder.

Mapping Kangchenjunga glacial flood risk

On the afternoon of 28 May, a massive glacier avalanche destroyed the idyllic village of Blatten in the Valais region of Switzerland. Footage of the disaster rapidly circulated around the world, sparking renewed conversation about the increasing instability of the mountain cryosphere and climate-related risks. The population of nearly 300 people had been evacuated a week prior due to concerns that unstable slopes above the glacier could trigger a catastrophic event. This is remarkable, and a testament to the value of hazard monitoring and anticipatory action. Shocked by the intensity of avalanche impacts and devastating loss, people struggled to comprehend the alternative: what if the village had been full? In Nepal, the people of the Langtang Valley, survivors of a massive glacier avalanche that killed over 300 people in April 2015, know exactly what it feels like for an entire village to be <a href="https://www.theguardian.com/world/2015/may/17/nepal-earthquake-langtang-village-everyone-was-dead">‘wiped off the map’</a> in a little more than a minute. The avalanche that buried the village of Langtang was similarly catastrophic, as the avalanche fell over 3,000m and <a href="https://www.nytimes.com/2015/12/19/world/asia/nepal-avalanche-langtang.html">carried nearly as much force as the Hiroshima atomic bomb</a>. Unfortunately, the people of Langtang had no warning. While these two disasters are quite different, there are some important connections between them. As the world contemplates the threat of increasing climate-related glacier hazards and wonders if and how Blatten will rebuild, I would like to draw attention to the ever-present risk of similar disasters in the Himalayas, where the scale of the problem is (arguably) larger and resources are (inarguably) more limited. As events like these become increasingly common, we need to build monitoring and <a href="https://www.undrr.org/implementing-sendai-framework/sendai-framework-action/early-warnings-for-all">early warning systems for all</a> at-risk communities. We also need more comparative analysis of the ways mountain people make sense of climate-related risks, particularly around wicked questions like hazard zoning and resettlement or relocation. How do institutions determine where to invest in hazard monitoring and early warning systems? Who gets to decide where people can rebuild, what kind of risks are ‘acceptable’, or whose uncertainties matter? As a survivor of the Langtang disaster and an applied anthropologist, this is not a thought exercise for me. I spent more than two years working with the Langtangpa community as a volunteer, and the last ten years conducting research focused on the aftermath of the Langtang avalanche and the ways people cope with disaster and climate risk in the Himalayan region. Since late 2022, I have been <a href="https://www.stimson.org/project/early-warning-systems-for-cascading-disasters-in-nepal/">working with the Stimson Center </a>to consider how we might build systems to assess and monitor the changing risks of cascading hazards in the Himalayan region. As the Swiss and a range of international organizations consider how they might provide warning for other Alpine villages living beneath glaciers, we need to expand the conversation to consider the many Himalayan villages that are similarly at-risk. The question of climate causality currently haunts the Blatten disaster -- just as it has for other similar events in recent years, including the Langtang avalanche. While attribution is incredibly complicated, many scientists have already highlighted the ways that melting permafrost and loss of seasonal snowcover and glacial mass created instability in the overall system above the Birch Glacier on Kleines Nesthorn. Not all glaciers are receding. In Blatten, recurring slope failures had also been piling debris on the glacier slowly over the years, pushing the ‘glacier tongue’ forward and weakening its integrity – and this acceleration attracted attention and focused monitoring. <a href="https://www.linkedin.com/feed/update/urn:li:activity:7334623807573278721/">A recent post from Christian Huggel, a leading cryosphere scientist based at University of Zurich</a> examined these details and clearly stated: “Considering all these processes it would be absurd, ignorant or dishonest to state that anthropogenic warming has not played any role in the ice-rock avalanche disaster in <a href="https://www.linkedin.com/search/results/all/?keywords=%23blatten&amp;origin=HASH_TAG_FROM_FEED">Blatten</a>. Interestingly, <a href="https://www.theguardian.com/environment/2025/jun/01/this-is-ground-zero-for-blatten-the-tiny-swiss-village-engulfed-by-a-mountain">other scientists have indicated that “exact attribution is almost beside the point.”</a> Tellingly, it took almost ten years for formal scientific recognition (see <a href="https://www.nature.com/articles/s43247-024-01624-z">this Nature paper published in 2024</a>) in part because it was seismically triggered, overshadowing the climate-related signal.That said, many Langtangpa highlighted these connections immediately after the disaster, as many are doing in Blatten right now. <a href="https://nepalitimes.com/banner/the-courage-and-endurance-of-the-langtangpa">My friends in Langtang have spent the last ten years rebuilding their lives</a> while wondering if another event of this magnitude might be possible.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250607140612_5ccfd4786416a151e1c2d44f79add3c196da34e1c30af9188de10982b45d72f8.jpg" data-media-id="editor_9" data-image-id="20250607140612_5ccfd4786416a151e1c2d44f79add3c196da34e1c30af9188de10982b45d72f8" data-rendition-name="original" width="1250" height="885" loading="lazy" alt="Blatten NT"> <figcaption>Copernicus statellite image of the avalanche that buried the village Blatten in Switzerland on 28 May, 2025.</figcaption> </figure>  &nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250607140616_306112d2eb5330d0a5117bae3fc372861afce5137b52f793285e6b1cf89ca31a.jpg" data-media-id="editor_10" data-image-id="20250607140616_306112d2eb5330d0a5117bae3fc372861afce5137b52f793285e6b1cf89ca31a" data-rendition-name="original" width="1733" height="1053" loading="lazy" alt="Langtang NT"> <figcaption>The deadly earthquake-triggered avalance that destroyed Langtang village in Nepal on 25 April, 2015.</figcaption> </figure>  Like the people of the Swiss Alps, the Langtangpa have been living with avalanches for centuries, and they have used both situated knowledge and practical systems to adapt to changing risks. But, in Langtang as in Blatten, the scale and impact of this singular tragedy was both unprecedented and unforeseen. Tellingly, Langtang was not a scientific hinterland: groups from a dozen different countries were conducting glaciological, hydrological, and climatological research there prior to the disaster. Blatten is a case where the scientists knew where to look. But even in relatively well-studied places like Langtang, disasters can emerge in our blind spots.&nbsp; <a href="https://nepalitimes.com/here-now/lives-on-the-line-in-the-himalaya">Last year’s Thame glacial lake outburst flood</a> (GLOF) also began in an overlooked and understudied area – <a href="https://www.stimson.org/2024/rethinking-himalayan-cryosphere-risk-assessment-in-the-wake-of-nepals-thame-disaster/">prompting scientists to rethink the ways we assess glacial lakes</a>. Issues related to <a href="https://www.icimod.org/mountain/permafrost/">melting permafrost</a>, which seems to have been a factor for both the Blatten disaster and <a href="https://www.linkedin.com/posts/tashi-lhazom-5a433b22b_rebuildtil-limifloodrelief-fromtearstohope-activity-7332420946013691904-N0sH?utm_source=share&amp;utm_medium=member_desktop&amp;rcm=ACoAAADxlvsBK3zQKg0X2xPLPS94HyMEettoSU4">the cascading ‘thermokarst lake outburst flood’ that recently occurred in the Limi Valley</a>, are increasingly recognised as a pervasive risk but it is difficult to monitor and the science is young. A multitude of different cryosphere-related disasters are possible across the Himalaya, and background risk is increasing. How do we triage between these different kinds of hazards? How do we know where to look? While it might not have been possible to monitor the glaciers and cryosphere features that contributed to the Langtang disaster, we need to be actively looking for other places where monitoring systems and early warning is possible in Nepal and the broader Himalayan region. Of course, we do need to be precise in our analysis and communication around climate attribution, but consensus does exist on some general trends: climate change is driving new hazard interactions that can generate extreme flows. Therefore, we also need to recognise the undeniable: that background risk is undeniably rising, that lives are at risk, and that we need to invest in building systems that can help anticipate events like Blatten (which takes time, time that others don’t have) immediately. The fact that Langtang has been fully rebuilt and community leaders were effective in determining the shape of their own future and ‘building back better’ their way (as complicated as that may be), demonstrates that a future can be possible, amid uncertainty. But the future of many other communities in the Himalaya, who should never have to go through what the Langtangpa went through if we can avoid it, still remains at-risk without more scientific attention and investment. Meanwhile, the monsoon is arriving in Nepal and another disaster could happen any day now. Coverage of the Blatten disaster has been rightfully robust. Praise for the scientists and authorities who identified these risks and correctly analyzed the situation is also deserved, for that is difficult work. A wider call to learn from this event and use insights to inform policy on climate risk assessment or questions of managed retreat is also exceedingly necessary and urgent. As many scientists are saying: events like this will happen again. This is a scary time in the mountains, in the Alps, in the Himalaya, and many other regions. That said, not all places are equally exposed or vulnerable. To reiterate a core question that I have been asking for years: <a href="https://dialogue.earth/en/climate/opinion-climate-disasters-integrate-local-knowledge/">Whose uncertainties matter</a>? When and why? We know that climate-related loss and damage will not be equally or equitably distributed, and that is one of the core reasons for the UN’s Early Warnings for All program. Blatten is being talked about this week <a href="https://globalplatform.undrr.org/2025/preparatory-days/global-ew4all-multi-stakeholder-forum">while the Global Platform for Disaster Risk Reduction is going in Geneva</a>, from where some of my Nepali colleagues posted photos of them posing with a sign that speaks to the justice issue: ‘Early warnings work. They must work for everyone.” Working toward this noble goal will require a concerted and committed global effort. -- Austin Lord, PhD is a Senior Fellow at the Stimson Center and an environmental anthropologist who has been conducting research in Nepal for the past 13 years on disaster and climate risk management, water and energy policy, infrastructure development, and environmental governance.

Blatten, Langtang, and Disasters Yet to Come?

The recent Nepali Times Substack post titled ‘Unresident Nepalis’ made me realise I also belong to the category of Nepalis who are technically Non-resident Nepali (NRN), but want to ‘permanently reside inside Nepal’.&nbsp;
Although this was meant as a joke, it is ironic that many of those who go abroad long to come back home, and those who have not emigrated cannot think of a good enough reason to stay back in Nepal.&nbsp;
As soon as the NRN Citizenship was officially introduced in late 2023, I had tried to apply for one but was shut down before even submitting my documents as the district administration office firmly told my then lawyer that I needed to prove “तिन पुस्ता” proof of three generations of Nepalis from my father’s side.&nbsp;
My late father was from Japan and relinquished his citizenship to become a Naturalised Nepali citizen in 2006. Three years ago, I dismissed the rejection with the thought that I will try again later when government officials would gain more experience with such applications.&nbsp;
Now, with an ailing mother and an energetic toddler, I felt the need to act soon and reached out to a law firm that specialises in NRN citizenship applications. To my surprise, they were positive after reviewing my documents, although they did warn me that we may need to overcome some obstacles.&nbsp;
In 2023, I had applied in the district office where my father had received his naturalised citizenship, but now the suggestion was to try from the district where my mother had received her Nepali ancestral origin “बंसागज” citizenship.&nbsp;
The lawyers pointed to the NRN citizenship mandate which clearly states that it can be acquired via a Nepali origin father, mother, grandfather or grandmother. The firm helped arrange the necessary documents required and the first step was to get a “सिफारिस” &nbsp;recommendation letter from my mother’s ward office.&nbsp;
This was the first hurdle as the ward office was unsure if they could issue such a letter, so they checked in with their head office, and luckily we received the go ahead. After persistent follow up from the law associates, they were able to provide us with a recommendation letter and we filled out the application forms.&nbsp;
The law firm wisely suggested that I take the paperwork myself to my mother’s district office while they stayed in the background in case I needed help explaining my situation.&nbsp;
With a big smile and cheerful tone, I dutifully followed the process and to my surprise, I found most of the officials ready to help without creating unnecessary hurdles. The application has to be signed off by the Chief District Officer (CDO) or Assistant CDO and just when I thought wow, I am going to breeze through this, one officer noticed that my father’s naturalised citizenship was from a different district and told me that I should apply for my NRN from there.&nbsp;
I explained that my father has already passed away and as he was not originally a Nepali, therefore it is not possible for me to get my NRN from his documents, as the requirement is ancestral “बंसागज” citizenship. The officer then went to check with their seniors and later told me that I would need police verification as an extra precaution.&nbsp;
Off I went to the police headquarters where they issued a sealed letter to be given to the police station that was in the same vicinity as my mother’s ward office. At the station I was told to get four people who are not my relatives to testify our documents are true.&nbsp;
This process happened to be more stressful than dealing with the government offices. At first, it turned out that most of my mother’s old neighbours had already passed away or had citizenship papers from another area. Others confirmed their availability, but later had conflicting schedules. Luckily, one very helpful old neighbour was able to arrange for enough people to verify the documents.&nbsp;
Encouraged that the end of the tunnel was in sight, I went back to the district office with all the requested documents, and after some initial pushback, I was finally referred to meet the official who signs off the documents before it goes to the CDO.&nbsp;
As luck would have it, the officials were in a meeting that lasted more than two hours, and I had to give my mother her insulin shot and noodles from the cafeteria in the waiting area.&nbsp;
When we were finally able to meet the officer, he didn’t even look at my papers properly and started questioning my lawyers whether they had even read the law, how could I apply for Nepali citizenship when I already had a Japanese passport, etc. He somehow assumed that I was looking to get a normal Nepali citizenship from my mother’s side, and we informed him that I was only looking to get an NRN citizenship, after which his tone became more apologetic and said that he would need to look into the law more closely.&nbsp;
It had already been three full days of working through each step of the process, and I had no problem waiting another day for the conclusion.&nbsp;
Perhaps because this NRN citizenship is a fairly new law and perhaps a lot of NRNs apply from the Nepal’s embassies in their country of domicile, throughout my experience, officials kept on telling me that a case such as mine has not been processed before.&nbsp;
My case being that I have never had a Nepali citizenship, my father having a naturalised Nepali citizenship and my mother being the only 100% Nepali in the family. I kept on saying that just because it has never been done before does not mean that it cannot be done, and sure enough, the next day the officer signed off on my documents, even kindly saying that they should have highly respected my application upon learning about my late father and his contributions to Nepal.&nbsp;
Although the intricacies of the NRN citizenship law have not been fully hacked out such as the transfer of land ownership, it is definitely a positive step in securing the rights and aspirations of fellow NRNs as many would agree that no matter where we go, “यो मन त मेरो नेपाली हो!”&nbsp;
Sonia Miyahara, Managing Director of Hotel Everest View, Trans Himalayan Tours &amp; Trekking Pvt Ltd &amp; Himalaya Kanko Kaihatsu Co. Ltd.

How I got my NRN Citizenship in Nepal

Nepal showed inconsistent performance at the T20 World Cup 2026 in Mumbai with flashes of brilliance, but ultimately snatched defeat from the jaws of victory. The <a href="https://nepalitimes.com/news/rhinos-hit-the-ground-running">near-win against England</a>, a test cricket team by an associate country, in the opening game showed promise and suggested that Nepal’s cricket was on the cusp of glory. The Nepal Premier League and a flawless performance in the qualifiers had raised hopes that perhaps the Rhinos could progress out of the group stage. However, subsequent losses against newcomers Italy and the West Indies were harsh reality checks about the true state of the game: there is a lot of catching up to do in the present, and structural changes to put in place to win big in the future. Head Coach Stuart Law summed it all up quite harshly: “To go from that high to then go to an extreme low four days later, that’s not showing mental toughness.” He was worried about the distraction of social media and lack of focus among players: “When you’re in cricket, do your cricket. It’s a difficult one for me because I’m a social media dinosaur, I don’t understand it. You don’t have to keep showing your face if we’re winning games.” Finally a late-night win against Scotland on Tuesday redeemed some of Nepal’s pride. A strong opening partnership, yet another rugged Dipendra Singh Airee innings and Sompal Kami’s vindictive 3 for 25 helped Nepal beat Scotland in their last group game at the T20 World Cup.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_6ca369f6aefc8b653c2572467f050e96b029c96b71fed5fb4213898c7d469325.jpg" data-media-id="editor_1" data-image-id="20260218010220_6ca369f6aefc8b653c2572467f050e96b029c96b71fed5fb4213898c7d469325" data-rendition-name="original" width="1366" height="2048" loading="lazy" alt="T20 World Cup Nepal"></figure>  There was nothing riding on the game but honour, it means at least that Nepal do not crash out on zero. The game ebbed and flowed. Scotland started well and looked set to score 200 before collapsing in the end at 170. The Nepal batting effort also started out well, but in the middle overs after some wickets had fallen, it looked like the team was whimpering out again. Boundaries dried up, the run rate creeped up to almost 13, before Airee and Jha woke up and took charge and got to 171 with a few balls to spare. The dhaka topi crowd in the stands loved it. A big part of the reason Nepal’s performance was so much better against England than in the other games was the mentality going in. Against England, Nepal were clear underdogs and could play freely. Even a nasty defeat would have been forgiven. Against newcomers Italy, these roles were flipped. Fans and perhaps the players underestimated Italy, a nation much better known for its football culture. But it had put together a smart, experienced team made up of Italian cricketers with South African, Australian, English, Indian, Pakistani and Sri Lankan heritage. And Nepal may have won a series against West Indies last year, but against the full strength Caribbean squad they were easily beaten.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_dc27adaa2102b493f940a97f9572769e695c2c1c41c8558fc4c23657cc1c3261.jpg" data-media-id="editor_2" data-image-id="20260218010220_dc27adaa2102b493f940a97f9572769e695c2c1c41c8558fc4c23657cc1c3261" data-rendition-name="original" width="2048" height="1366" loading="lazy" alt="T20 World Cup Nepal"></figure>  Another key difference is that Nepal was batting second against England. Against Italy and the West Indies, having to set a target rather than chase it, there was miserable batting failure. The front of the order — openers Kushal Bhurtel and Aasif Sheikh, captain Rohit Poudel — did not pace themselves well. They started much too slow, not able to take advantage of the first six powerplay overs. Airee’s 58 and Sompal Kami’s 26 off 11 against the West Indies were the only innings of any note. The middle order of Bam, Jha, Aarif Sheikh was not much better. Nepal really struggled with the ball too in that game, taking the one wicket against the West Indies and none against Italy. Of course, it is a huge ask of your bowling attack to defend anything below 150 in the modern T20 game. There were questionable tactical choices. Early wickets are essential when defending a low score. But key wicket taker Sandeep Lamichhane was not brought on until the middle overs, when the opponents had made too many runs to feel any fear. So they took him on and he had a really poor tournament, going for a lot of runs.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_b0301b854ddf235e1bcb84e8ed58060a68c8f3f13d3bb5a7596e1f51184e0d03.jpg" data-media-id="editor_3" data-image-id="20260218010220_b0301b854ddf235e1bcb84e8ed58060a68c8f3f13d3bb5a7596e1f51184e0d03" data-rendition-name="original" width="1366" height="2048" loading="lazy" alt="T20 World Cup Nepal"></figure>  To captain Poudel’s credit, he acknowledged the bad showing against Italy: “It was not a 123 all-out wicket. We are professionals and not turning up for the game was disappointing.” Coach Law thinks that Nepal is going to get to the next step. If the team is ambitious, and hopes to compete at the elite level, then it cannot celebrate a loss against England. If it wants to win consistently, it has to shed the ‘Cardiac Kids’ nickname. It is better to win than to be fun to watch but lose. The T20 game is so brisk and so it is often won in the margins. Good catching and fielding can create momentum and save a team the 5, 10 runs that win the game. Nepal were uncharacteristically poor in the field against Italy and West Indies, often fumbling and leaking boundaries. Airee didn’t get any of his usual run-outs either. Nepal lost cheap wickets through run-outs and stumpings. All these unforced errors right through the match add up on the scoreboard.  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_1630c283f277631dfbddd3d7f29b930b124bde97c8f6a411cc2e1d089e452f45.jpg" data-media-id="editor_4" data-image-id="20260218010220_1630c283f277631dfbddd3d7f29b930b124bde97c8f6a411cc2e1d089e452f45" data-rendition-name="original" width="1366" height="2048" loading="lazy" alt="T20 World Cup Nepal"></figure>  SKILL SET Mentality is important but sport performance ultimately comes down to skill. There looked to be a large gap, and perhaps one of the reasons is because the Nepal team is so full of all-rounders. Airee’s two-way performance is undeniable, but Bhurtel, Paudel and Karan KC do plenty of both too and they do not do it super well very often. If the team wants to get consistent, it must have consistent performers with the bat and ball. That calls for some of these players to focus completely on one skill over the other. You do not see openers bowling so much in the top teams as Bhurtel does. The main reason for this skill gap, and one of the hardest parts about being an associate nation, is how little cricket the members of the team play compared to the test nations. Said Stuart Law: “The longer format is where you learn how to play the game. The shorter formats are where you have your fun. We need some sort of multi-day games.”  <figure><img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20260218010220_652ef3ba6fceab394a94c18cabd322dca8ba4a1266557660064339de9169c91d.jpg" data-media-id="editor_5" data-image-id="20260218010220_652ef3ba6fceab394a94c18cabd322dca8ba4a1266557660064339de9169c91d" data-rendition-name="original" width="2048" height="1366" loading="lazy" alt="T20 World Cup Nepal"></figure>  The contrast in experience showed during the Italy game. Most of the members of the Italy team were well into their thirties, had played a high volume of domestic cricket and were more self-assured. So, while the young Nepali team were more athletic, they seemed to lack the skill and experience to know what to do when things were going wrong. The Italians seemed to go about their game with a lot more self assurance. In the long run, this means setting up grassroot structures, getting kids into formal training when young, and setting up a longer format domestic league. In the short term, CAAN could organise frequent series with other associate nations, and individual athletes could go play long form club cricket abroad. Surely some team in the world has to have a spot for a player like Airee, for example. It has been Airee’s tournament. Scores of 44 v England, 58 v West Indies, and now a match-winning 50 against Scotland that gives the travelling Nepali support something to cheer for. The tournament could have been a lot more, but it is wholesome to end on a win.

Nepal goes in and out of T20

Besides being an election year in Nepal, 2026 is also the year of anniversaries. It is exactly 30 years since the Maoists launched their armed struggle on <a href="https://nepalitimes.com/editorial/13-february">13 February 1996</a>, and it was on 27 April 2006 that the ceasefire came into effect after a month of massive pro-democracy protests.
Alas, <a href="https://nepalitimes.com/editorial/not-ever-again">three decades on</a>, the decade-long conflict that claimed 17,000 lives has been <a href="https://nepalitimes.com/banner/ghosts-of-war">air brushed from our history</a>. For the survivors, and the families of those disappeared and killed, memories of loss and suffering are fading. The party that fought the war in Mao’s name has dropped it.
It is important on this day to remember not to forget that <a href="https://archive.nepalitimes.com/news.php?id=3203">violent decade</a> -- so that it does not happen again, and so the youth movement that has led to this election will also not be in vain.
The 8 September 2025 rally, <a href="https://nepalitimes.com/news/nepal-s-8-september-massacre">the massacre that followed</a>, and the nationwide mayhem and carnage the next day were largely a result of public anger boiling over. Nepalis had been let down repeatedly by rulers promising revolution in the name of the ‘people’: from the 1990 People’s Movement I, to the Maoist ‘People’s War’, and the 2006 People’s Movement II.
There are some positive residual effects of the insurgency. One-third of the Maoist militia was <a href="https://archive.nepalitimes.com/article/nation/Nation-sibling-war-juna-rai,731">composed of women</a>, this empowered not just the female guerrillas themselves, but indirectly made a whole generation of young women aware of their rights.&nbsp;
The peace process itself resulted in the Maoists entering the democratic mainstream, and the induction of many of the guerrillas into the national army – a rare occurrence after a conflict.
The ceasefire was followed by an interim government, and the first elected <a href="https://nepalitimes.com/editorial/the-letter-and-spirit">Constituent Assembly</a> abolished the monarchy in 2008. Deadlock over the model of federalism meant a second election had to be held in 2013, and the new Constitution <a href="https://archive.nepalitimes.com/regular-columns/by-the-way/new-constitution-should-adopt-inclusive-democracy-with-federalism-republicanism-secularism,538">finally promulgated in 2015</a>.&nbsp;
That statute was supposed to devolve political decision-making away from Kathmandu to autonomous provinces, improve inclusive representation of women and hitherto excluded castes and ethnicities at all three levels of government, ensure accountability and good governance to generate jobs and lift living standards.
There were seven governments in ten years after 2015, and tottering coalitions one after another failed to fulfil any of those provisions in the Constitution. There were subliminal gains in representation of women thanks to affirmative action, but as this election shows, women candidates are still used as proxies by patriarchal parties.&nbsp;
Since the two warring sides of the Maoist war both became the state, sharing power in dozens of coalition cabinets since 2006, they colluded to bury the <a href="https://nepalitimes.com/news/nepal-s-unpunished-war-crimes">transitional justice process</a>.
The former supreme commander of the Maoists Pushpa Kamal Dahal (Prachanda) has become prime minister three times in the last 20 years. He is contesting this election from Rukum East, where he marked the 30th anniversary of the start of armed struggle on Friday.
The word ‘Maoist’ has been erased from the Nepali Communist Party which Dahal formed with more than a dozen other smaller leftist outfits. His main rival, Janardan Sharma, quit the Maoists and is standing for elections in Rukum West.
Both former comrades are competing for the hearts and minds of people of this former base area from where the Maoists went on warpath on 13 February 1996 by attacking a police station in Athbiskot, and simultaneously on targets in <a href="https://archive.nepalitimes.com/news.php?id=7812">Holeri of Rolpa</a>, Sindhuli and Gorkha.
The former ideologue of the Maoist party, <a href="https://archive.nepalitimes.com/article/editorial/20-years-wasted-in-war,2850">Baburam Bhattarai</a>, was the architect of the revolution while Dahal was the <a href="https://archive.nepalitimes.com/news.php?id=6369#.Y-XIii8w1KM">executor</a>. Bhattarai submitted a list of 40 demands to the <a href="https://nepalitimes.com/editorial/deubas-denouement">Sher Bahadur Deuba</a> (during his first tenure as prime minister in 1995) but did not wait for a reply before launching the armed struggle.
The Maoists felt that the constitutional monarchy after 1990 was too feudal, and a patronage-driven parliamentary system too slow to bring about change. Besides, the democratic parties were accused of using state security to prevent Maoist candidates from winning elections.
The Maoists followed Mao’s Red Book to the letter, attacking police stations, looting weapons and targeting local elected governments, eliminating ‘class enemies' with summary executions.&nbsp;
They destroyed telecommunication towers, highways, bridges and airfields in remote areas. Threats forced health posts, schools, post offices to be withdrawn from areas where people needed them the most. The country’s development was pushed back decades.
Nepal in the early 1990s was ripe for revolution. There was inequality, social injustice, exclusion, and the political parties in Kathmandu were too busy squabbling to do their job. The Maoists wanted an end to the monarchy, but in 2001 the monarchy imploded with the royal massacre.
ABSOLUTE POWER
King Gyanendra succeeded his <a href="https://archive.nepalitimes.com/news.php?id=8338">murdered brother</a> to the throne, and took the country back to absolute rule with a military-backed coup in 2005. Within a year, street protests forced him to step aside. And by 2008, it was too late to save the monarchy.
We can look back as far as we want to the roots of the Maoist conflict. It can be blamed on elected leaders post-1990 who abandoned the people once in power, the 30 years of partyless Panchayat system that stifled dissent and let social pressures build up, or even 100 years of Rana rule.&nbsp;
It was the prolonged indifference on the part of successive rulers in Kathmandu that fed public discontent. These accumulated grievances were also the reason for the <a href="https://nepalitimes.com/news/nepal-s-gen-z-protest-turns-deadly">September 2025 events</a>.&nbsp;
During China’s Cultural Revolution, Mao Zedong said: ‘The old has to be uprooted to be replaced with the new’, and that could almost be the anthem of the GenZ movement and this election.
The objective conditions that drove the Maoist insurgency 30 years ago are still evident today. And much will depend on the government(s) that will be formed after March.&nbsp;

Remembering not to forget

As Nepal mourned its dead in the September violence and public buildings smouldered, former Chief Justice Sushila Karki was installed as prime minister to pull the country back from the brink.
She gave herself six months to conduct elections, and has gone about achieving that goal with a single-minded sense of purpose. Supporters praise her poise and decisiveness, while others fault her for not pursuing justice for the death and destruction, and postponing the release of the inquiry commission yet again.&nbsp;
But that also highlights her steadfastness to hold free, fair and peaceful elections on 5 March, and not allow it be derailed by distractions. It has not been easy for the 73-year-old — she has had to balance radical calls for scrapping the Constitution while appeasing entrenched leaders of established parties.&nbsp;
Karki has displayed patience, determination, foresight, and, above all, a deep love for country. It has been a lonely struggle, no doubt.
The very youth who voted for her on Discord demanded her resignation, &nbsp;she had to cajole discredited leaders to take part in polls, and she was not dismayed when her chosen ministers abandoned the government to contest polls. And this is not to mention geopolitical demands that must be happening behind the scenes.
This being Nepal, there is endless speculation about who is ‘pulling the strings’. Yet her record both as chief justice and interim prime minister offer ample evidence of integrity and principled leadership.
Regardless of geopolitical interpretations of her intentions, Karki is a Nepali leader through and through who has lifted herself from the highest judicial office to the highest executive position, adhering to both mandates.
Organising national elections within five months was a formidable task, which many doubted — and are still doubting — can be accomplished. Karki has worked closely with the Election Commission, security forces, and mainstream political parties to ensure participation.&nbsp;
In doing so, she has set an example not only for Nepal but for South Asia. Bangladesh, which went through its own GenZ protest in 2024 and held elections on Thursday offers a study in contrast. The Awami League and its exiled prime minister who was deposed have been banned from front contesting, there is growing influence of the Jamaat-e-Islami-led alliance.
Her first address to the National Assembly on 2 February was characteristically candid. She laid out the facts sequentially and emphasised Nepal’s most urgent priority: holding elections on schedule and transferring authority to elected representatives. Timely election was the only constitutional path forward, she said.
She acknowledged that GenZ activists had pressured her to appoint certain individuals to her Cabinet. She had to personally persuade Kulman Ghising, Mahabir Pun, and Jagdish Kharel to join her Cabinet. Others she was advised to induct turned out to have controversial pasts, and she was forced to rescind the nominations. She admitted Pun resigned as education minister because he could not get legislative proposals passed.
Educated, professionally accomplished, known for her frugal lifestyle, Karki has distanced herself from the culture of excess often associated with power, and has turned down multiple invitations for foreign junkets.
Her meeting with editors at Baluwatar in December was a breath of fresh air for Nepal’s jaded journalists used to excessive displays of power and pomp. Her frankness about threats from the GenZ and pressures from disgraced party leaders drew gasps.
In the last five months, Karki has attempted to restore a sense of governance anchored in constitutional duty rather than partisan ambition. But Nepal’s problems have been decades in the making, and it would be unrealistic to expect an interim government to solve all of them at once.
Nepal now stands at a crucial juncture. Leadership alone cannot safeguard democracy, elections alone do not guarantee legitimacy. That must come from delivery, performance and accountability. Citizens casting informed votes on 5 March will determine whether Karki’s handover to leaders capable of placing national interest above party and personal agendas.
In a region where democratic transitions often falter, Nepal has another chance to demonstrate that home-grown movements, constitutional discipline, and principled leadership can coexist.&nbsp;
Whether this moment becomes a turning point depends not only on one leader, but on the collective resolve of the nation and polity.
Watch a timelapse video of how Anup Tamu drew this portrait of Sushila Karki, <a href="https://youtube.com/shorts/tchdBwBZDJE?si=PD9Sd3__t-1-lILh">here</a>.&nbsp;