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

<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 news headlines this week said: ‘The House of Representatives passed the Nepal Citizenship (Second Amendment) Bill that now makes <a href="https://nepalitimes.com/here-now/nepals-unequal-citizenship-law">acquiring citizenship through the mother</a> as equal as through the father.’&nbsp;
Could it really be true? There is genuine confusion or deliberate misunderstanding in the public about the Bill. Here is an explainer:
What is the Bill?
The Second Amendment to the Nepal Citizenship Act 2006 was tabled by the government on 11 March, 2024. The lengthy list of amendments underwent a detailed discussion within the State Affairs and Good Governance Committee of the HoR which presented a shortened list of agreed amendments.&nbsp;
The HoR passed this amended list of amendments on 28 June. While the original Bill contained eight amendment proposals, only three major amendments were presented by the Committee, and approved by the HoR.
Has it become law now?
No. It is yet to be passed by the National Assembly and endorsed by the President.
What exactly is contained in the amendments?&nbsp;
<ol>
 <li>Addition to Section 5 of the Act: ‘For citizenship applications, a father’s identity is deemed unknown if the applicant and their mother both provide a self-declaration stating that the father is unidentified, as per Section 5, even if his name is listed on the person’s birth registration, educational qualifications, or other certificates, yet his other identity is not available and is currently out of contact.’</li>
</ol>
This simply provides a definition to what the Act means by ‘father unidentified’ or ‘father untraceable’. Section 5 derives its authority from Article 11(5) of the Constitution that grants citizenship by descent to children whose mother is a Nepali citizen, but father is unidentified or untraceable.&nbsp;
The Nepal Citizenship Act 2006 and Regulation 2006 (both promulgated prior to the present 2015 Constitution) was amended in 2023 to incorporate the provisions of the new Constitution. In doing so, it included the procedural rule requiring both the applicant and their mother to sign a self-declaration form.
The result: a lot of people who claimed citizenship under this provision were still denied access, simply because their educational or other documents mentioned the name or address or some information about their father. The officials interpreted the presence of such information as father’s identity being known and assumed the applicants were hiding facts.
Read also: <a href="https://nepalitimes.com/opinion/no-state-for-women">No state for women</a>, Neha Gurung
The Supreme Court in one of such cases had clearly interpreted the meaning of ‘father unidentified’. In its overarching decision, the court stated the following:
‘It seems neither lawful nor just to compel an individual to accept someone as an identified father merely because their biological father’s name, surname, or address is claimed to be known or mentioned in educational or other documents. It would be just to consider the father’s identity as “unidentified”; if the individual has not received paternal affection or care, and the alleged father has never taken any responsibility, borne any obligation, or been physically present before the children, leading to a situation where the children haven’t even seen their face. Such an alleged biological father should remain “unidentified” for these children until they formally acknowledge them as their son or daughter, or, in their absence, their family provides reasonable proof to confirm the fact and identifies the relationship through a process acceptable to the children, or until such a confirmation becomes impossible.’
Based on this decision, multiple implementation challenges, and growing advocacy around this concern, the government included the above-mentioned addition in <a href="https://nepalitimes.com/here-now/nepal-s-citizenship-amendment-bill-explained">the Bill</a>.
Is it new?
The proposed addition is neither an introduction of the new right, nor does it provide anything beyond what the Constitution mandates. Since the Constitution itself uses the term ‘father untraceable or unidentified’, the most a legislation can do is to ensure that the constitutional provisions are interpreted and implemented in its true meaning. Therefore, the current Bill only serves to clarify the existing misinterpretation of the phrase ‘father unidentified’.
In a country where about 17% of the population are <a href="https://archive.nepalitimes.com/regular-columns/Comment/stateless-daughters-in-nepal,863">single mothers</a>, this clarification may provide certain relief for those whose fathers name was mentioned in the document and the father is now unidentified. However, the addition does not grant anything new.
The <a href="https://nepalitimes.com/banner/are-women-not-nepali-enough">gender discriminatory citizenship </a>where the citizenship or legal identity of a person is always dependent on one’s husband or father still remains.
Additionally, the current addition does not completely incorporate the Supreme Court’s decision which is broader and more comprehensive, requiring that the father be considered unidentified irrespective of the knowledge of the father’s name, surname and address, if the applicant/person has not felt the paternal affection or care, and the alleged father has never taken any responsibility, or borne any obligation or been physically present before the children.
The Bill only takes ‘father’s name’ into consideration. It does not recognize the mention of surname or address in the applicant’s certificates, nor the absence of emotional and physical presence, and responsibility in their life.
2. Addition to Section 18 of the Act:
i. Unless otherwise provided in this Act, a person dissatisfied with an order or decision made by an official under this Act may file a petition with the Secretary of the Ministry of Home Affairs within thirty-five days from the date of such order, through the District Administration Office or directly through Nepal Government.
ii. Upon receiving the report pursuant to sub-section (1), the Secretary of the Ministry of Home Affairs shall (must) issue their decision or order after obtaining the report from the official who issued the order or made the decision, within 30 days from the date of appeal, and such decision or order made by them shall be final.’
This provision is already present in the Act itself, and the Bill simply amends or adds the parts that are in bold letters. The positive part is that it makes the right to redress mandatory. Meaning, it not only ensures the right to appeal against the unsatisfactory decisions made by the local authorities, but also the right to receive the decision.
Earlier, it depended on the government's discretion to hear the appeal, but if this amendment is passed, it now becomes the State's obligation to ensure this as a due process of law.
This makes it easier for individuals denied citizenship, by the Chief District Office (CDO), to register an appeal in the higher office, which is the Home Ministry. However, in cases concerning a certain category of naturalised citizenship that falls under the jurisdiction of the Home Ministry, its decision becomes final and cannot be appealed.
This means that Nepal has two categories of naturalised citizenship. One that falls under the jurisdiction of CDO, such as naturalised citizenship to foreign women via marriage relationship. Another that falls under the jurisdiction of the Home Ministry, such as naturalised citizenship to persons born to Nepali mother and foreign father or foreigners who intend to acquire citizenship via stay requirement.&nbsp;
While the former can be appealed if the applicant is not satisfied with the decision of the official, the former, which is the government's decision, cannot be appealed.
3. Addition of Section 22(a) to the Act: ‘Shall provide a minor’s identity card to a person who is under 16 years of age, if either mother or father is a Nepali citizen.’
This provision can be considered as a positive extension of the child’s constitutional right. The Constitution of Nepal in Article 39 (1) states that ‘every child shall have the right to name and birth registration along with his or her identity’. The current Bill extends this right to a minor's ID card.
However, a minor ID card does not guarantee a citizenship certificate, which in Nepal, a person is eligible to apply only at the age of 16. This means: even though the child has the minor’s ID card and perhaps also a passport based on it, while applying for citizenship at the age of 16 or beyond, the person is bound by citizenship laws — which as we have seen is heavily dependent on the father's identity.
The conclusion?
The current amendment does not ensure any dramatic legal reform nor ensure a complete <a href="https://archive.nepalitimes.com/article/nation/The-right%20-to-have-rights,2656">gender equality in nationality laws</a>, simply because it technically and legally cannot.
When the Constitution itself uses gendered language such as ‘mother’, ‘father', ‘Nepali citizen man’, and ‘foreign citizen woman’, a legislation cannot override it. Nevertheless, recent amendments to the Act, including the first amendment, shows the government’s leniency towards gender equal citizenship laws.
Additionally, Article 49 of the Constitution also recognises equal lineage right of women, meaning that the family descent is legally recognised to be carried on by both genders. Hopefully in the nearest future, Nepal will carry this same principle to shape its citizenship law as well.&nbsp;
A transformative reform by ensuring gender equal nationality rights through constitutional amendment is still possible. Nepal, a member state to the CEDAW and CRC, is still in the list of 24 countries in the world that have gender unequal citizenship laws. &nbsp;It has the obligation as well as potentiality to become a pioneer in recognizing<a href="https://nepalitimes.com/editorial/quality-of-equality-for-women"> women’s equal rights </a>to confer citizenship to their children and spouse in par with men.
Neha Gurung is a human rights lawyer dedicated to advocating for equal citizenship rights, and co-founder of the Citizenship Affected People's Network. A Fulbright scholar, Gurung obtained LLM from the Washington College of Law.

Full equality vs status quo

The sudden and massive flood on the Bhote Kosi early Tuesday morning washed away a strategic bridge on Nepal’s main border crossing with China for trade, tourists and pilgrims. Slurry from the nearly 10m high debris flow left 9 dead and 20 missing, 12 of them Nepalis and six Chinese nationals, and 150 others were rescued by helicopter.&nbsp; Four <a href="https://nepalitimes.com/banner/climate-smarter-himalayan-infrastructure">hydropower plants</a> Rasuwagadi, Trisuli III, Trisuli, &nbsp;Benighat and the Trisuli substation sustained heavy damage, knocking &nbsp;out 230MW of Nepal’s power supply – approximately 8% of the total. Over 100 cargo trucks and new electric vehicles parked at &nbsp;Timure Dry Port were swept away. Read also: <a href="https://nepalitimes.com/news/mapping-kangchenjunga-glacial-flood-risk">Mapping Kangchenjung glacial flood risk</a>, Gabe Allen Officials had initially thought &nbsp;the Bhote Kosi had flooded due to heavy rain in Tibet. However, the Department of Hydrology and Meteorology (DHM) and the National Disaster Risk Reduction and Management Authority (NDRRMA) now say a <a href="https://nepalitimes.com/here-now/living-below-nepal-s-melting-mountains">Glacial Lake Outburst Flood (GLOF)</a> is likely.&nbsp; NDRRMA spokesperson Suresh Sunar said it was too early to tell which one, but the flood was most likely the result of one of the glacial lakes in Tibet. Bhote Kosi begins on the north slope of the Ganesh Himal near the Nepal-China border, and its tributary Lende drains the catchment area north of Langtang. The slurry flood on Tuesday was on the Lende (map).&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250709110720_bbc99c5f3e3d61a3d340892e0273fee3605a8d334a2beb354126137bcf0c8d27.jpg" data-media-id="editor_3" data-image-id="20250709110720_bbc99c5f3e3d61a3d340892e0273fee3605a8d334a2beb354126137bcf0c8d27" data-rendition-name="original" width="629" height="759" loading="lazy" alt="Bhote Kosi flood map"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250709110720_39e2f574ff8c12cecda2e5a999d2ba8a0310f599f6b2261dcad7dd43f94df2a1.jpg" data-media-id="editor_4" data-image-id="20250709110720_39e2f574ff8c12cecda2e5a999d2ba8a0310f599f6b2261dcad7dd43f94df2a1" data-rendition-name="original" width="997" height="613" loading="lazy" alt="Bhote Kosi flood map"> </figure>  “Preliminary study suggest that the disaster was not caused by rain in Tibet, but by a glacial lake burst, or another accident,” said Kamal Ram Joshi of the DHM. The level of water at a self-monitoring station in Timure in Rasuwa increased by 3.5m at 3:10AM on Tuesday morning while 13km downstream in Syabrubesi, the level rose by 3.65m at 3:30AM. The same station recorded 5.37m ten minutes later, after which it stopped giving a reading, possibly because the station was also washed away. The flood reached <a href="https://nepalitimes.com/here-now/neither-side-lost-both-sides-won">Betrawati</a> by 5AM, and some of the debris flow reached Mugling during Tuesday. DHM’s Flood Forecasting Division noted that there was no major precipitation in the Bhote Kosi watershed in Nepal and China in the 24 hours preceding the flood.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708100724_313a684b65fc5317064779e47409a40f2bbce2c0c84db995e7f8fc6e1c142105.jpg" data-media-id="editor_6" data-image-id="20250708100724_313a684b65fc5317064779e47409a40f2bbce2c0c84db995e7f8fc6e1c142105" data-rendition-name="original" width="3600" height="1662" loading="lazy" alt="Bhotekosi flood"> <figcaption>The Miteri bridge before it was swept away by the flood in Bhotekosi on the Nepal-China border. Photo: SUBASH DHUNGANA / RSS</figcaption> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708100732_ec43f13bae979f7b61bc0db939db4157dc93d3f0767ed527f564bd5c3d12be27.jpg" data-media-id="editor_7" data-image-id="20250708100732_ec43f13bae979f7b61bc0db939db4157dc93d3f0767ed527f564bd5c3d12be27" data-rendition-name="original" width="720" height="432" loading="lazy" alt="Bhotekosi flood NT 2"> <figcaption>The bridge after the flood.</figcaption> </figure>  On Wednesday, several remote-sensing experts using Copernicus &nbsp;satellite images pinpointed the cause of the flood to Purepu Cangbu where supraglacial ponds had merged in June to form a large lake which did not burst, but overflowed &nbsp;and found a channel through englacial conduits to the headwaters of the Lende. The river meets the Bhote Kosi at the Nepal-China checkpoint in Rasuwa.&nbsp; “Analysis of weather forecasts and satellite data shows the Tibet region did not receive enough rain to cause this scale of flooding,” explained Binod Pokharel, associate professor of hydrology and meteorology at Tribhuvan University. “The flood could have been caused by a GLOF."&nbsp; Two weeks ago, Chinese officials had reportedly warned the Rasuwa District Administration in Nepal to be on high alert for floods on rivers that originate in Tibet. It could be that Chinese scientists had observed the alarming<a href="https://nepalitimes.com/here-now/the-climate-crisis-is-a-water-crisis-in-the-himalaya"> expansion of glacial lakes</a> in the Lende and Bhote Kosi catchments. If that was the case, it is an example of the kind of trans-boundary forewarning that would be critical to save lives in future.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250708100736_1710142917b30d4f85b343ed52743554d723db918c708f0bade8a0491ba999b2.jpg" data-media-id="editor_9" data-image-id="20250708100736_1710142917b30d4f85b343ed52743554d723db918c708f0bade8a0491ba999b2" data-rendition-name="original" width="1001" height="500" loading="lazy" alt="Bhotekosi flood"> </figure>  However, Rasuwa’s Assistant Chief District Officer Dhruv Prasad Adhikari seems to have no knowledge of any warning from the Chinese side, either formally or informally. &nbsp; “The Chinese Embassy has said the cause of the flood is unknown that it will coordinate with Nepal to find the cause," Adhikari told us. Chinese Ambassador Chen Song and Prime Minister Oli visited the border on Tuesday (pictured). &nbsp; The sharing of real-time trans-boundary rainfall and river flow data would be crucial in early warning about the <a href="https://nepalitimes.com/news/mapping-kangchenjunga-glacial-flood-risk">risk and consequences of GLOFs</a> to reduce human and material loss. But Nepali officials say China has been reluctant to share weather-related information and data not just in this disaster, but in the past as well. “There is no mechanism or system in place for us to obtain hydrological and meteorological data of the Tibetan region,” said DHM Director General Joshi. The <a href="https://nepalitimes.com/here-now/for-destruction-ice-is-also-great-and-will-suffice">Himalaya is melting twice as fast as the rest of the world</a> due to a phenomenon called ‘elevation dependent warming’, and receding glaciers have led to an increasing number of transboundary GLOFs.&nbsp; According to <a href="https://nepalitimes.com/here-now/danger-nepal-s-glacial-lakes-are-filling-up">a 2018 ICIMOD study</a>, of the 47 of the most dangerous lakes that threaten Nepal, 25 are on glaciers in China, 21 in Nepal and one in India. Many of these glaciers are expanding rapidly due to global warming. One of the authors of the report, glacial lake expert Samjwal Bajracharya, says that the report was prepared based on data from 2015. But climate change has accelerated since then. Moreover, seismic activity has further destabilises the landscape, adding to <a href="https://nepalitimes.com/here-now/nepals-glacial-lakes-in-danger-of-bursting">GLOF risk</a>.&nbsp; “Considering the rapid rate of snowmelt and consequent increase in size of Himalayan glaciers, studies should be conducted every year, and a monitoring system should be set up on the glaciers,” says Bajracharya. “However, no studies have been conducted in the Himalaya in a decade, which has been our biggest weakness.” &nbsp;

Rasuwa flood likely a GLOF

Former president Bidhya Devi Bhandari last week officially made her comeback to <a href="https://nepalitimes.com/news/what-just-happened-in-nepali-politics">national politics </a>at an event commemorating her late husband UML leader Madan Bhandari’s 70th birth anniversary. Bhandari’s announcement was not a surprise, nor was the furious flutter it created both within and outside the UML. A former president returning to party politics sets a dangerous precedent, many said. &nbsp;&nbsp;&nbsp; “Now that I have been released of my previous political responsibilities, I have renewed my party membership with the righteous intention of remaining in the CPN-UML and continuing the<a href="https://nepalitimes.com/latest/post-convention-uml-eyes-set-on-elections"> party's political journey</a>,” Bhandari said, not very convincingly. Nepal’s Constitution does not prohibit a former head of state from returning to active politics once their presidential term is over, essentially leaving such decisions to ethics rather than any legality. But her return to the UML fold has angered party leaders who considered themselves Oli’s successors as well commentators who saw it as yet another example of the <a href="https://nepalitimes.com/latest/the-business-of-politics-in-nepal">deep rot in Nepal’s politics</a>. ‘<a href="https://nepalitimes.com/news/coalition-set-to-snub-president-bhandari">Bidya Devi Bhandari </a>has not tired of ‘serving’ us despite having held multiple ministerial positions, high-level party positions, and serving two terms as President, but the country and its citizens are tired of her unceasing and immoral ‘service’,’ political commentator Muma Ram Khanal wrote sardonically on social media. ‘Please do not embarrass us through your lifetime ‘service’.’ Bhandari tried to mollify critics by pledging to forego all perks and facilities she is entitled to as a former head of state. This was met with enthusiastic cheers from supporters at the public function. Prime Minister KP Oli, sitting right beside her on the stage, remained stone-faced. He has been against Bhandari’s political comeback, and has tried to talk her out of it. &nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250711040740_0f2b201ed3ce2f85540554c83fc7aae6bcfcd1377aef614bbc3759eef30baa3f.jpg" data-media-id="editor_4" data-image-id="20250711040740_0f2b201ed3ce2f85540554c83fc7aae6bcfcd1377aef614bbc3759eef30baa3f" data-rendition-name="original" width="2400" height="1599" loading="lazy" alt="PM Oli and Bidya Devi "> </figure>  Oli has reasons to worry, as Bhandari has made it clear that she intends to run for party chair in the next UML general convention. There are also those within the UML who have grown resentful of <a href="https://nepalitimes.com/news/nepal-government-changes-again">Oli’s leadership</a>, and this has polarised the party into two camps with leaders like Ishwar Pokharel in Bhandari’s corner. Oli wields absolute authority over the party, particularly after he sidelined and silenced rivals Madhav Kumar Nepal, Jhalanath Khanal, and Bamdev Gautam.&nbsp; He has removed the party’s 70-year age limit to hold leadership position so that he can continue to be chair even as he approaches the end of term limit, and questions about his health after two kidney transplants. Bhandari wasted no time in wading right into politics to forge alliances. Last week she met Kathmandu Mayor Balen Shah to discuss “latest developments”. She is said to have urged <a href="https://nepalitimes.com/opinion/comment/kathmandu-s-balen-phenomenon">Kathmandu’s popular independent mayor</a> to enter national politics through a party. The mayor is keeping his cards close to his chest. &nbsp; The former president’s return to active politics has also not sat well with other parties, either. Nepali Congress (NC) president Sher Bahadur Deuba, and Oli’s coalition partner, is said to have raised issue with Bhandari’s comeback. The NC Central Committee meeting this week was abuzz with corridor talk about how retired presidents returning to politics affects not just the UML, but undermines <a href="https://nepalitimes.com/editorial/slapping-democracy">Nepal’s democracy</a>. &nbsp; The UML is not the only party roiled in internal strife. The NC Central Committee meetings turned lively as the rank and file fed up with<a href="https://nepalitimes.com/news/deuba-s-long-and-winding-road"> long-serving Deuba</a> and the higher political profile Foreign Minister Arzu Rana, his wife, demanded an overhaul of the leadership.&nbsp; The surname Koirala still has strong brand equity in the NC, and a rival faction led by Shekhar Koirala has questioned Deuba’s competence and has intensified calls for the party’s next general convention to be held on time. His cousin, Shashank Koirala also supports a constitutional amendment to revert Nepal back to Hindu state – possibly with an eye on <a href="https://nepalitimes.com/news/women-first-in-2027-wfnchctq">the 2027 election</a>. The NC’s young turks are no longer young. Party General Secretary Gagan Thapa is approaching middle age while waiting for a greater leadership role with the promise of fresh new blood to rejuvenate the party. &nbsp; Meanwhile, CPN-Unified Socialists chair and former prime minister Madhav Kumar Nepal is facing calls for resignation from within his party after being charged with corruption by Commission for the Investigation of Abuse of Authority (CIAA) for alleged involvement in the Patanjali land scam.&nbsp; Nepal, who has been stripped of his lawmaker status, is currently out on bail. He has said the case against him is politically motivated, fuelled by one-time comrade K P Oli's vendetta.&nbsp; The CPN-US members do not seem keen on Nepal taking the already beleaguered party down with him. Firebrand leader Ram Kumari Jhakri called for a new leadership at an event of the party’s youth wing last week, obviously pushing herself as a possible successor.&nbsp; “The party chair is facing legal and constitutional challenges, we cannot move forward with this dead weight on our shoulders,” Jhakri said, calling for an early general convention to choose new leadership. CPN-US leadership has since admonished her gently about her remark, but others like Jhalanath Khanal and Ghanashyam Bhushal have lent their support. Khanal, a former prime minister himself, even asked for Nepal’s resignation at the party’s secretariat meeting earlier this week.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250711050712_bed4145c696497f12eedc746dcd0308d251ca02312bef88c549a51d54a5032a8.png" data-media-id="editor_10" data-image-id="20250711050712_bed4145c696497f12eedc746dcd0308d251ca02312bef88c549a51d54a5032a8" data-rendition-name="original" width="262" height="402" loading="lazy" alt="Two to tango"> </figure>  Over at the Maoist-Centre, Pushpa Kamal Dahal is also said to be at loggerheads with top comrades, particularly Deputy General Secretary Janardan Sharma, who used to be a guerrilla commander during the conflict. &nbsp; Dahal and Sharma’s relationship has been strained since the party’s last general convention, when Dahal bypassed Sharma for General Secretary. The two have traded barbs in public and private since then. Sharma has long called for competition in party leadership, but like Oli and Deuba, Dahal is reluctant to give up the reins. Dahal has reportedly been reluctant to hold a general convention fearing he will be voted out of his chairmanship. &nbsp; In response, Dahal has attempted to fill the ranks with his own confidants, including actively lobbying for the return of former vice-president Nanda Bahadur Pun to active politics despite objections from the party. Like Bidya Bhandari, this has not been welcomed within the party and outside. And then there is the<a href="https://nepalitimes.com/news/in-with-the-new-out-with-the-old"> Rastriya Swatantra Party (RSP)</a>, the fourth largest in Parliament whose chair, former tv anchor leader Rabi Lamichhane, is in detention for multiple charges of defrauding cooperatives. The three main parties see the RSP as a threat in 2027 and want to tie Lamichhane up with court convictions, but his prolonged detention has actually allowed him to gather some public sympathy – at least on social media. The RSP has rallied around Lamichhane in public, but there are rifts within the party. In April, MP Sumana Shrestha resigned as the party’s joint general secretary, levelling criticism at the leadership and the lack of intra-party democracy and calling for reforms. But Lamichhane’s legal troubles have put a dent on the RSP’s Mission-2084 election campaign, which has come to a standstill.&nbsp; Aisde from internal feuds in all the main parties, the four main parties are also jostling for advantage ahead of 2027. And last week, the Janata Samajwadi Party and Nagarik Unmukti Party both withdrew from the alliance. &nbsp; Speculation is rife of a rift between the two largest parties in the coalition. This is driven by the two parties, which have been bitter rivals since 1990 but are now partners in government, in the leadup to elections. &nbsp; In public, the two parties have maintained that the coalition remains strong as ever. Oli is said to be considering recalling some of his ministers to pacify the NC’s dissatisfaction with UML cabinet members. Deuba seems determined not to let the coalition collapse ahead of his turn to be prime minister for the sixth time next year as per a ‘gentlemen’s agreement’ with Oli.&nbsp; The cement that binds the coalitions together is the mutual threat they feel about <a href="https://nepalitimes.com/opinion/higher-corruption-in-high-places">corruption </a>probes of their leaders. The former RSP-NC-Maoist coalition collapsed last year after Deuba and Oli got wind that Home Minister <a href="https://nepalitimes.com/banner/the-rise-and-fall-of-rabi-lamichhane">Rabi Lamichhane</a> had started investigating the involvement of their top leaders on the fake refugee and tea estate scams. &nbsp; For the moment, though, it seems as though the relationship between Oli and Deuba is more stable than the support both leaders have within their own &nbsp;parties. But the question as the elections approaches is, for how much longer.

Uncontrolled instability in Nepal

Recent outrage in Sikkim over an Indian Army expedition climbing <a href="https://nepalitimes.com/here-now/saving-kangchenjunga">Kangchenjunga</a>, the world’s third-highest peak, has spiked attention to the need to balance mountaineering jobs with indigenous reverence for sacred landmarks. Kangchenjunga (8,586m) is not a peak as much as it is a mountain range with 16 peaks above 7,000m on the border between India and Nepal -- the word itself means ‘five treasures of the snows’ in Tibetan. Some of the highest prominences like Kangchenjunga West and Kangbachen are in Nepal, while the Main, Central and South Peaks are on the border. Climbing the peak from the Indian side has been banned since 2001 because the indigenous Lepcha community there regard the mountain as the abode of Dzoe-nga, the patron deity of Sikkim, which was an independent Himalayan Kingdom until it was annexed by India in 1975.&nbsp; Buddhists in Sikkim say their saint, Padmasambhava, recognised the mountain as a protective spirit. The state has declared the base of the mountain Kangchenjunga National Park, which covers an area one-third of Sikkim. ‘The act of scaling this sacred peak is not only a matter of serious concern but also a violation of both the prevailing legal provisions and the deeply held religious beliefs of the people of Sikkim,’ read a letter from Chief Minister Prem Singh Tamang (Golay) to Amit Shah, India’s Minister of Home Affairs and Cooperation.&nbsp; Tamang continued: ‘We further request Your Honour to take up the issue with the Government of Nepal to ensure that no future expeditions are permitted on the sacred mountain, in deference to the deeply held beliefs and cultural values of the people of Sikkim.’ Kangchenjunga was climbed for the first time exactly 70 years ago by a British team who told King Tashi Namgyal, the Choegyal of Sikkim, that they would not set foot on the summit. Since then, there have been about 532 successful climbs of the peaks and 52 have died while trying.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250628060616_5c268e08cf49f36b79ef9b31933fc2d9bf9a6f65414e7ca06dd028bf04e7ccc1.png" data-media-id="editor_1" data-image-id="20250628060616_5c268e08cf49f36b79ef9b31933fc2d9bf9a6f65414e7ca06dd028bf04e7ccc1" data-rendition-name="original" width="1782" height="1178" loading="lazy" alt="Kangchenjunga: too sacred to climb NT"> <figcaption>Indigenous communities in Sikkim held purification ceremonies following the Indian expedition to Kangchenjunga. Photo: THE VOICE OF SIKKIM / FACEBOOK</figcaption> </figure>  <a href="https://nepalitimes.com/here-now/peak-climbing-season-2025-s4abrxny">This spring climbing season</a> alone, there were 70 climbing permits for foreigners issued for Kangchenjunga by the Nepal government, and made it to the top while one French climber died.&nbsp; One of the expeditions this year was an Indian Army team led by Col Ranveer Jamwal, who has summited the highest peaks on all seven continents, and Mt Everest thrice. Jamwal’s team was on the final leg of a ‘<a href="https://economictimes.indiatimes.com/news/india/nimas-summits-mt-kangchenjunga-concludes-historic-har-shikhar-tiranga-mission-successfully/articleshow/121341315.cms?from=mdr">Har Shikhar Tiranga</a>’ (The Tricolour on Every Peak) mission to plant the Indian flag at the highest points of each of India’s 28 states. Kanchenjunga was the last peak they had left, and the hardest, but the expedition put five climbers on the summit. What seems to have incensed the Sikkimese is that while it has banned climbing the mountain from its side, it was an Indian military expedition that went to Nepal to climb the mountain. After news broke of the climb in May, the Sikkim Indigenous Lepcha Tribal Association asked people to observe purification ceremonies in temples across the state. Mayalmit Lepcha of the association acknowledged that the Sikkim government was also partly at fault: “I don’t think such an expedition could have gone forward without the state government being informed, so it could have done something to intervene. It shows weakness. What’s done is done, all we can do is carry out these sanctification ceremonies.”&nbsp; In 2000, one year before Sikkim’s ban, the state allowed an Austrian team to attempt Kanchenjunga’s northeast face for a fee of $20,000, on agreement that they would stop 10m before the summit. Despite this, there was outrage over the expedition on the grounds that it violated Indian laws regarding the defiling of religious sites and Sikkim’s rights to maintain its culture after merging with India. The Indian Army expedition was also seen to have circumvented Sikkim’s law and violated religious sensibilities by going through Nepal. While the team may have thought they were respecting Sikkim’s beliefs by finding a way to complete the mission, the people of Sikkim saw it as defilement.&nbsp; The somber mood of the Sikkim people at the ritual contrasts sharply with Jamwal’s sense of accomplishment. “Without a doubt, the most difficult summit of my life,” he told reporters after the climb. “It tested every ounce of our will.”&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250628060616_ccfe079c78dab788d19fe2080ee8a5d5dcb11de4157316f6d94e5964da097157.jpg" data-media-id="editor_4" data-image-id="20250628060616_ccfe079c78dab788d19fe2080ee8a5d5dcb11de4157316f6d94e5964da097157" data-rendition-name="original" width="787" height="377" loading="lazy" alt="Kangchenjunga: too sacred to climb NT"> <figcaption>Prayer flags along the Sikkim-Kangchenjunga trekking route. Photo: TREKKINGININDIA.COM</figcaption> </figure>  The <a href="https://nepalitimes.com/news/the-rise-and-fall-of-nims-purja">controversial Nepali-British mountaineer Nirmal Purja</a> was also on Kangchenjunga this spring the mountain, on a mission to summit all 14 8,000m peaks for a third time. He echoed Jamwal about the tough conditions: “The conditions above camp were extremely tough, with deep snow and challenging terrain—more crevasses than usual.” Nepal’s government has not said anything publicly, but it is unlikely that it will ban climbing on Kangchenjunga, since it is becoming popular with expeditions because of its technical challenges, and overcrowding on Mt Everest. Nepal does have bans in place for some of its mountains out of respect for local beliefs. <a href="https://nepalitimes.com/banner/to-open-machapuchre-for-mountaineering-or-not">Mt Machapuchre</a> (6,990m) the imposing pyramid that looms over Pokhara, for example, is seen as an icon of purity by the Gurung people and a symbol of Vishnu by the Hindu communities who live at its base. A strict climbing ban has been in place since 1957, when a British expedition led by Col Jimmy Roberts stopped 45m short of the summit – either because the last bit was too difficult or out of deference to local sentiments.&nbsp; Khumbila that stands above Namche Bazar is only 5,761m high, but like Kanchenjunga is considered the protector deity of the Sherpa people. Gauri Shankar on the Nepal-China border, called Chomo Tseringma by the local community, was off-limits between 1965 and 1979 due to its association with Lord Shiva and Gauri, his consort. Although expeditions are now allowed, there are not too many takers. In Tibet, climbing Mount Kailash is prohibited by the Chinese government because it revered by the Hindus, Buddhists and followers of the Bon faith. Even Mt Everest is regarded as sacred, and its Sherpa name is Chomolungma, Goddess Mother of the Earth.&nbsp; Economically, climbs on Kanchenjunga bring in decent revenue. This climbing season, the 41 permits, at $1,800 each, brought in $73,800. This is somewhat comparable to Makalu, Lhotse, and Annapurna I, but these numbers are dwarfed by the $4 million in <a href="https://nepalitimes.com/news/the-everest-industry">Everest permits</a>. Revenue from Kanchenjunga climbing permits is something Nepal could potentially forgo if necessary, but the expeditions also provide jobs to hundreds of high altitude guides, porters, base camp support staff and other logistical costs.&nbsp; As the third highest mountain in the world and the tallest in India, there will always be significant motivation to climb it from the Nepal side, especially as climbers are drawn by the technical climbing at high altitude.