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?

As dusk fell over Kathmandu, the thunderstorm continued unabated. It had been raining continuously for 18 hours, and the forecast said it would keep raining at least till 8am on Sunday. The Bagmati roared through Chobhar Gorge in awesome rapids – the only drainage outlet for the entire Kathmandu Valley. By evening, 120mm of rain had fallen in 18 hours, more than the average for the whole of October.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004161016_99ad9098124bec91da71ac42bbe889981fe64dda2dd3012b8bb289cf78ba4c54.jpg" data-media-id="editor_0" data-image-id="20251004161016_99ad9098124bec91da71ac42bbe889981fe64dda2dd3012b8bb289cf78ba4c54" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="Kathmandu floods 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004161016_59b97f3a3b2af91d3876b298963b3e68395c8b388aba6d9972c9bde1f668608d.jpg" data-media-id="editor_1" data-image-id="20251004161016_59b97f3a3b2af91d3876b298963b3e68395c8b388aba6d9972c9bde1f668608d" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="Kathmandu floods 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004161016_1715f4d6ff1ee87302b697d3c95df36486bea71ed279852ef606c8f5dc68439b.jpg" data-media-id="editor_2" data-image-id="20251004161016_1715f4d6ff1ee87302b697d3c95df36486bea71ed279852ef606c8f5dc68439b" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="Kathmandu floods 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004161016_ecd3dec69270afbd5a5c71dfa71780b6f8982984a95f3fbb83f23ee594451224.jpg" data-media-id="editor_3" data-image-id="20251004161016_ecd3dec69270afbd5a5c71dfa71780b6f8982984a95f3fbb83f23ee594451224" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="Kathmandu floods 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004161016_53e47ae222c9f4397bcdad6d8021a711a5671fd45373fb3df2ed5c6413d58359.jpg" data-media-id="editor_4" data-image-id="20251004161016_53e47ae222c9f4397bcdad6d8021a711a5671fd45373fb3df2ed5c6413d58359" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="Kathmandu floods 2025"> </figure>  Settlements along the banks of Bagmati and Vishnumati in Kathmandu have been evacuated and affected families will be temporarily sheltered in schools across the capital.&nbsp; Bagmati Province has set up a Unified Command Team for disaster management while the Home Ministry has instructed CDO and security personnel to be on duty 24/7.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004171048_7e5d10f8e0042190e54e6db6cddbd51ed9d6d9dbc0cdb087d7af3207c9eaa2d0.jpg" data-media-id="editor_5" data-image-id="20251004171048_7e5d10f8e0042190e54e6db6cddbd51ed9d6d9dbc0cdb087d7af3207c9eaa2d0" data-rendition-name="original" width="1600" height="888" loading="lazy" alt="heavy rain in Kathmandu"> <figcaption>Friday's satellite precipitation forecast for Sunday morning at 0600 showing heavy rainfall along the Chure Hills and Madhes Province south of Kathmandu. </figcaption> </figure>  The torrential rain has obstructed several highways as well as caused infrastructure damage, but no human casualties have been reported so far. Many had feared a repeat of the deadly flashfloods on 28 September 2024 in which 200 people were killed and half of Nepal's hydropower generation capacity siped out. The government has declared 5 and 6 October as a public holiday to prevent people from travelling during the Dasain festival, and to reduce risk. All highways in and out of Kathmandu closed till Monday. Flood-prone river corridor roads in Kathmandu have been closed after 6PM on Saturday. Meanwhile, all domestic flights were suspended from Kathmandu and other airports from 2PM Saturday, and most inbound international flights were diverted from 3PM onwards. Rerouted flights started arriving in kathmandu late Saturday as the core of the storm system moved east.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151056_bad029b05dbfda622986270a798edc6efcc2791ff34f53b9d1283554ac72c39a.jpg" data-media-id="editor_6" data-image-id="20251004151056_bad029b05dbfda622986270a798edc6efcc2791ff34f53b9d1283554ac72c39a" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rainfall in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151052_9e740929c7ef0899b0f397195695b873bba45b089bb1e11cf37dbe125d0cd60d.jpg" data-media-id="editor_7" data-image-id="20251004151052_9e740929c7ef0899b0f397195695b873bba45b089bb1e11cf37dbe125d0cd60d" data-rendition-name="original" width="2048" height="1363" loading="lazy" alt="heavy rain in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151056_2b75c2ea57df76dae1c470f0e460720b7d258868258789729e491ab93cb41ebd.jpg" data-media-id="editor_8" data-image-id="20251004151056_2b75c2ea57df76dae1c470f0e460720b7d258868258789729e491ab93cb41ebd" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rainfall in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151056_6c045ac30e50710bcf3ca7b6ca4ac9c45e8d8881ed39f522779c860b0d3f15c3.jpg" data-media-id="editor_9" data-image-id="20251004151056_6c045ac30e50710bcf3ca7b6ca4ac9c45e8d8881ed39f522779c860b0d3f15c3" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rainfall in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151052_9ef160b8403764495b86159661cc9a11d9d7d3b848686a631e5ec8cff0c4c38f.jpg" data-media-id="editor_10" data-image-id="20251004151052_9ef160b8403764495b86159661cc9a11d9d7d3b848686a631e5ec8cff0c4c38f" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rain in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151052_e5825bcc6666e5235d9db2d4854a19cd6536335ebaf4cd65413acc601ceee3b5.jpg" data-media-id="editor_11" data-image-id="20251004151052_e5825bcc6666e5235d9db2d4854a19cd6536335ebaf4cd65413acc601ceee3b5" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rain in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151056_097077400e96f571f4418cd7b57c082045d86dd9035c31c5acd7ede2bfc54349.jpg" data-media-id="editor_12" data-image-id="20251004151056_097077400e96f571f4418cd7b57c082045d86dd9035c31c5acd7ede2bfc54349" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rainfall in Kathmandu 2025"> </figure>   <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004151056_30a4da8f384f6fe1a862e775124ae08ccf51c1db60e71e7e2d683e0f25f33546.jpg" data-media-id="editor_13" data-image-id="20251004151056_30a4da8f384f6fe1a862e775124ae08ccf51c1db60e71e7e2d683e0f25f33546" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="heavy rainfall in Kathmandu 2025"> </figure>  Madhes, Bagmati and Kosi provinces are the worst hit with Maheshpur in Rautahat district recording 270mm of rain as of 3PM on Saturday. Similarly, Gaur received 243.6mm, Kalaiya in Bara 200.6mm and Birganj 221.4mm. The Department of Meteorology did not blame climate change, but said the unusually heavy precipitation at a time when the monsoon is supposed to have ended was caused by the head-on collision between moisture-laden westerlies with the retreating monsoon.

More dark clouds over Nepal

Kathmandu: A Reader, the latest publication from Martin Chautari, is an anthology of anthropological essays exploring Kathmandu through various lenses across the 21st century. This compilation is edited by Benjamin Linder and attempts to bring modern discourses on Kathmandu and its urbanity together, in a single volume. The book is divided into three sections: the physical form of the city, the imprints it bears from past political upheavals, and the complexity in the lives of its people. The book examines these diverse aspects, leaving readers who have just witnessed the momentous events of September with anxiety, and perhaps a greater understanding of Kathmandu’s context. Urban planning expert Biresh Shah’s discourse on the Valley’s urban sprawl and its landmarks is insightful, but also prophetic when he warns about seismic risk.&nbsp; Jan Brunson’s chapter on female mobility in Kathmandu via scooters is more optimistic, suggesting small-scale, daily-life movements in Kathmandu transform the city for its various demographics — in this case young women.&nbsp; Linder himself contributes with a discourse on the toponymy of Thamel, close-reading Kathmandu’s tourist hub through the usage and understanding of its name over the ages. MYTHBUSTERS The book is a collage of pieces held together by a thread that runs through the chapters of a vibrant, bustling image of the Valley. One common theme is Linder’s attempt to expand on common understandings and urban myths about Kathmandu. Readers who have spent time in the city will relate to the many anecdotes. for example, Niels Gutschow bringing up the lack of open spaces, or Mark Liechty mentioning restaurants in Kathmandu being melting pots of cultures and castes.&nbsp; The essays here further extend these urban legends by giving historical and anthropological contexts. In-migration and the rise in land prices have led to shrinking open spaces, the creation of cosmopolitan food outlets, and even hubs for sex workers. The Bagmati cleanliness campaign extends to a past understanding of the Bagmati Civilisation. Urban myths become puzzles to be solved by connecting the various threads of discussion across the book. The sections in Kathmandu: A Reader are all by experts in their various fields and present a holistic, well-rounded picture. Yet, it is obvious there is still more ground to cover, more themes to explore — perhaps by more Nepali scholars.&nbsp; In his introduction, Linder admits that due to practical reasons, ‘many wonderful works were left on the cutting room floor’. That is a pity. Indeed, there could have been more discourse on the changing ethnic composition of Kathmandu. A close-read into the lives of people termed as ‘outsiders’ but forming a growing slice of the population would be important to also chart future trends. &nbsp; The religious importance of Kathmandu as a unique civilisational alloy forged by melding the Hindu and Buddhist faiths can be explored more too. One can imagine a future edition including an examination of the post-Covid era Kathmandu valley.&nbsp; This need to broaden the ethnographic literature on Kathmandu becomes more apparent because 11 out of the 15 essays here are written by non-Nepali scholars, including the entire section focusing on urban cultural politics. Linder explains in his introduction that this was largely due to the community of academics in Nepali urban studies being fairly small. Kathmandu: A Reader then becomes even more integral as a gateway for new authors looking to work in the space of urban research on the Valley — undergraduates in the humanities for future theses and research ideas.&nbsp; In a time when Kathmandu is littered with new exam coaching centres for medical and engineering students, an anthology like this helps remind young scholars that there is plenty of scope for qualitative research in the social sciences. Sabin Ninglekhu’s discourse on the sukumbasi and aesthetics in Kathmandu are reminders that stories and academic journeys can be inspired from one’s surroundings. Kathmandu: A Reader has a good balance between academic and lighter readings, and is almost encyclopaedic in nature. There is even content about Kathmandu’s gangsters and scooty girls — allowing readers to venture deeper into their milieu.&nbsp; Kshitiz Pratap Shah is a recent graduate in English from Ashoka University.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251002051016_c8ce28ecfd0dde4986023822b3d40360ead97d29b7f186f6494d8da67021c5a5.jpg" data-media-id="editor_0" data-image-id="20251002051016_c8ce28ecfd0dde4986023822b3d40360ead97d29b7f186f6494d8da67021c5a5" data-rendition-name="original" width="1136" height="702" loading="lazy" alt="Kathmanu a reader"> </figure>

A reader for Kathmandu

One is an archipelago, the other is landlocked. But the Philippines and Nepal have a lot in common: both are disaster-prone, their economies dependent on overseas migrant workers, both went though Maoist insurrections that failed to replace a feudal order dominated by political dynasties. And both countries suffer from rampant corruption. Twelve days after <a href="https://nepalitimes.com/news/nepal-s-new-normal" target="_blank">deadly protests toppled Nepal’s government</a> tens of thousands of Filipinos, many of them youth, also poured out into the streets demanding transparency and better government. Cars were set on fire, and more than 200 people were arrested, nearly half of them minors. The ‘Trillion Peso March Against Corruption’ was fuelled by <a href="https://www.nytimes.com/2025/09/21/world/asia/manila-philippines-rally-protest.html" target="_blank">anger over embezzlement</a> by politicians and their <a href="https://pcij.org/2025/08/31/5-reveals-from-the-flood-control-data/" target="_blank">crony contractors</a> estimated to top $17 billion in flood control infrastructure that were either never completed, or non-existent.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025100411108_85daed60ed5599f53235312e5b33703244bbac8640dbaf5161f90e5abe83f7eb.png" data-media-id="editor_3" data-image-id="2025100411108_85daed60ed5599f53235312e5b33703244bbac8640dbaf5161f90e5abe83f7eb" data-rendition-name="original" width="2326" height="1366" loading="lazy" alt="Phillipines anti-corruption protests"> </figure>  “We learnt from Nepal and <a href="https://www.nytimes.com/2025/09/30/world/anime-protests-flag-moldova-nepal-indonesia-gaza.html" target="_blank">Indonesia</a> how to deploy social media as a tool to spread information, we are digital natives and well connected within the country and across borders,” said <a href="https://www.linkedin.com/in/yuri-lemana-68322b183/?originalSubdomain=ph" target="_blank">Yuri Lemana</a> of the <a href="https://www.facebook.com/FOIYouthPH/" target="_blank">Youth Alliance for Freedom of Information</a>, and a part of the GenZ protests.&nbsp; “The system has failed us, unemployment is on the rise, there are shrinking opportunities for youth, and we face environmental threats. There is a realisation that our future is at stake,” Lemana added. Online groups started highlighting bribery and kickbacks in July after President Ferdinand (Bongbong) Marcos Jr himself brought up corruption in the infrastructure budget in his annual address to the nation, and launched a probe.&nbsp; The protests gained traction after powerful visuals of <a href="https://nepalitimes.com/news/international-spotlight-on-nepal" target="_blank">rallies in Indonesia and Nepal</a> circulated on digital platforms. Filipino journalists also exposed the <a href="https://www.youtube.com/watch?v=-f0MFz3vmfE" target="_blank">high-flying lifestyle of contractors</a> involved in siphoning off the infrastructure budget.&nbsp; As in Nepal, the youth protests were joined in by various radical groups. In Manila they reportedly included supporters of ex-president Rodrigo Duterte who is currently on trial at the <a href="https://www.icc-cpi.int/philippines/duterte" target="_blank">International Criminal Court (ICC)</a> in the Hague for extrajudicial killings during his ‘war on drugs’ 2011-2019. Duterte still has a lot of support, especially in the Filipino diaspora, for being tough on crime. Duterte was allied with Marcos in the 2022 elections, and his daughter Sara Duterte is currently vice-president. But the two families had a massive falling out, and the Supreme Court annulled the Lower House’s attempt to impeach the vice-president. This week in Manila, a remarkably well-informed Grab driver replayed TikTok videos of Kathmandu’s burning Parliament building to a passenger from Nepal. After his garment factory was driven out of business by cheap Chinese imports, he started driving a ride-hailing cab and was livid with successive governments not providing opportunities to ordinary people like him. Traffic was gridlocked because of flooded streets, and the driver vented out his anger: “Look at this. The streets are always flooded because of corruption. We should have done here what you did in Nepal.” Even before the protests, Senate President Francis Escudero and House Speaker Martin Romualdez had both resigned over the 'Floodgate Scandal'. Romualdez is Marcos’ cousin and is now said to be in Madrid, where his every movement is being tracked by Filipino diaspora in social media posts. The Independent Commission for Infrastructure has issued subpoenas to probe corruption in flood control projects. As in Nepal and Indonesia, much of the anger was over the offspring of politicians extravagantly flaunting their ill-gotten wealth on Instagram and TikTok. In the Philippines, the outrage is also over political clans passing on electoral seats to offspring. The 21 September protests were centred around Rizal Park and the EDSA Intersection in Manila — both symbolic for previous people’s movements against the Spanish colonialists and the 1986 uprising against the dictatorship of Ferdinand Marcos (father of the present president). “People here had seen what happened in Nepal, and were asking why we weren’t as angry as people there? Why not show our anger, too?” said one reporter who covered the protests. But, he added: “Let’s not be naive. It may have started with youth anger, but there were also people who were paid to infiltrate and instigate. We were also wary that things should not get out of hand like in Nepal.”  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025100411104_2c02ece56d29b2d8222433572d75c2dcc9bc2f3425d277a0056f393b521eecd0.png" data-media-id="editor_10" data-image-id="2025100411104_2c02ece56d29b2d8222433572d75c2dcc9bc2f3425d277a0056f393b521eecd0" data-rendition-name="original" width="1550" height="996" loading="lazy" alt="Phillipines youth protests"> <figcaption>An Instagram post of the protests in Manila with a comment relating it to the Nepal unrest two weeks earlier.</figcaption> </figure>  Seventy percent of Filipinos are Millennials and GenZ of voting age, and they were impatient with a rigged electoral system. In a clear parallel to what happened in Kathmandu two weeks earlier, radical groups, political rivals, and the general public furious with the system all joined in the protests. Catholic priests, people from all generations and professions had participated in the EDSA Uprising against Marcos in 1986. This time, it was the youth who took the lead. Joseph Francisco Ortega of the <a href="https://www.facebook.com/nationalyouthcommission/" target="_blank">Philippine National Youth Commission</a> said he understands the frustration among the youth that fuelled the unrest. The discontent is also because despite there being young legislators, they are either party-affiliated or scions of political dynasties. “If we can convince young politicians to do the right thing, then we have won half the battle,” Ortega said. “If we want to rebuild quickly and for the long term, we have to change the system from within. There is a constructive way to do this, while exercising the right to non-violent protest.” CROSS-POLLINATION The <a href="https://www.youtube.com/watch?v=6w8monPKdrc" target="_blank">violence in Manila streets</a> on 21 September was nowhere near the scale of what happened in Kathmandu on 8-9 September, but both transcended GenZ to be an outlet for pan-generational rage much like 1986 in the Philippines.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20251004111012_e9cf9abfa8e35f3c074506dfdf94a262b5b311da6863cc2ec7bc3458a983df71.jpg" data-media-id="editor_13" data-image-id="20251004111012_e9cf9abfa8e35f3c074506dfdf94a262b5b311da6863cc2ec7bc3458a983df71" data-rendition-name="original" width="6566" height="4377" loading="lazy" alt="Nepal GenZ protests"> <figcaption>Angry crowd torched Parliament building among others during the 8-9 September GenZ protests in Nepal. Photo: AMIT MACHAMASI</figcaption> </figure>  “With due respect to the youth, it is not about age but about technology,” explained journalist Malou Mangahas of the <a href="https://www.facebook.com/R2KRN/" target="_blank">Right To Know, Right Now Coalition</a> who participated in the 1986 uprising against Marcos. “We were all young and angry once. We are older, but still angry, and demanding good governance, transparency and accountability.” Just like in Nepal, young Filipinos rallying against corruption were also wary of infiltration, and it was clear from the anti-Marcos graffiti who the instigators of violence were. The GenZ were mainly wearing white while the pro-Duterte crowd <a href="https://www.youtube.com/watch?v=6w8monPKdrc" target="_blank">are seen in videos</a> in black.&nbsp; The minors seem to have just joined in the melee from their street-side settlements. Rights groups have called for their release, accusing police of rough interrogation and ‘red-tagging’ as Communist provocateurs. Much of the transboundary cross-pollination of anti-government protests across Asia last month used gaming characters, memes, and anime personas like the manga cartoon One Piece flag depicting a grinning skull in a straw hat which became an icon of youth protests.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025100411100_2d09f075663678fe92d4e4dcc631ee6ad1aa8a99996f4c4a3649e4bf4d85132f.png" data-media-id="editor_16" data-image-id="2025100411100_2d09f075663678fe92d4e4dcc631ee6ad1aa8a99996f4c4a3649e4bf4d85132f" data-rendition-name="original" width="810" height="1208" loading="lazy" alt="One Piece"> <figcaption>The One Piece Flag flying during protests in Manila on 21 September. Photo:  CYBERNETICBOYLOL / WIKIPEDIA</figcaption> </figure>  Yuri Lemana adapted a saying of gaming character <a href="https://www.warhammer.com/en-WW/shop/mechanicum-archmagos-prime-2024?srsltid=AfmBOorpYg8Zk5G5WiPUS9SXTampX969gMw79sP7ZzkE1G6H5pICR4PW" target="_blank">Archmagos Cortiko</a> in <a href="https://start-warhammer.com/" target="_blank">Warhammer 40,000</a>: “Prayer has its power, but fury also has its uses. If the government tries to hide things from us, we will find a way. Fury will find a way.” Kunda Dixit is the Publisher of Nepali Times, and was a foreign correspondent based in Manila in the early 1990s.

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