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 monsoon has got bad press because Nepal’s tourism operators actively told visitors to avoid <a href="https://nepalitimes.com/opinion/managing-the-monsoon?%2F">the rainy season</a>. It is time to change that. The reason can be found right here in the vast alpine meadows of Central Nepal where this time of year you can walk on velvet grass of pastures abloom with delicate pink, red and yellow flowers as the mist rolls up the valley. There is no sound except the hum of bumble bees. &nbsp;&nbsp; There are dozens of places across high Nepal called Chaurikharka, which means yak pasture. But this particular Chaurikharka in Rukum East located at an altitude of 4,000m stands out for its serene beauty, rustic charm and bucolic setting. There is just the occasional chime of <a href="https://nepalitimes.com/here-now/when-yaks-go-so-does-culture">yak bells</a> in the distance, and the sharp whistle of herders corralling sheep. &nbsp;&nbsp; The grass shoots are so fragile that one hesitates to step on them, the rounded ridges appear and quickly vanish in waves of mist. With the<a href="https://nepalitimes.com/here-now/before-the-next-monsoon"> arrival of monsoon</a>, these meadows are a soothing shade of green dotted with millions of <a href="https://nepalitimes.com/review/the-anatomy-of-a-flower?%2F=">multi-coloured flowers</a>. Until very recently, it took a week or so to hike up to places like Chaurikharka, but with the expansion of the road network even to these far-flung mountains in the lap of Dhaulagiri, they are much more accessible. It is just a three-hour uphill from the Mid-Hill Highway on the border between Baglung and Rukum East.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250802130828_a0b06b494d751b2144ffbbf10894ea64b29e8aed844bc8c66171783abfaf4e16.jpg" data-media-id="editor_4" data-image-id="20250802130828_a0b06b494d751b2144ffbbf10894ea64b29e8aed844bc8c66171783abfaf4e16" data-rendition-name="original" width="2048" height="1365" loading="lazy" alt="Visit Nepal in the monsoon"> </figure>  Purists would say that such easy access devalues the sanctity of these remote high meadows, but it also means more people will be moved to treasure the experience, appreciate <a href="https://nepalitimes.com/banner/natures-fragile-gift-to-nepal">the value of nature </a>so they can take steps to protect it.&nbsp; To be sure, the <a href="https://nepalitimes.com/here-now/deadly-monsoon-in-nepal-turns-deadlier">monsoon season can be challenging for road travel</a>. The roads are rough even at the best of times, and in the monsoon they become muddy and treacherous, often blocked by<a href="https://nepalitimes.com/news/monsoon-deluge-in-nepal"> landslides</a>. But that could be precisely the kind of adventure that the more intrepid visitors crave. Improved road connectivity has already made Chaurikharka and places like Badimallika &nbsp;and other sacred lakes in the mountains of western Nepal popular with domestic tourists. What is driving this traffic is the urge to go to exotic new places and share videos and selfies on social media. Several of Nepal’s travel vloggers have visited Chaurikharka and popularised the place, enticing followers on TikTok or YouTube to retrace their footsteps. But even as they become more popular, these fragile and once-remote places should be protected from over-tourism.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250731110736_f97110b7cdc3e7f80d5877690948fc9f4c95a09c583deb23b07355491e6c5446.jpg" data-media-id="editor_8" data-image-id="20250731110736_f97110b7cdc3e7f80d5877690948fc9f4c95a09c583deb23b07355491e6c5446" data-rendition-name="original" width="1083" height="699" loading="lazy" alt="Visit Nepal in the monsoon NT"> </figure>  <h2>INCREASING FOOTFALL</h2> Chaurikharka is located in Bhume Rural Municipality of East Rukum, near the scenic valley of Dhorpatan in Baglung district. Even in the <a href="https://nepalitimes.com/banner/monsoon-culture">middle of the monsoon</a>, there is a steady stream of Nepali hikers trooping to these high pastures – especially during festival days like Saune Sankranti which this year was on 17 July and actually marks the auspicious beginning of the monsoon here. “This year the rains have not been as heavy and there have been some clear mornings when we could see everything from Dhaulagiri to Machapuchre,” says Khageswar Bhandari, who trekked up here from the road. “The flowers, the greenery and the snowy mountain views make this an incredibly unique place.”&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250802130824_1b9e26f2e9853fdfe69154bb42a7c9ea6da4bf4940efc1da99b304dcfbd7d3d9.jpg" data-media-id="editor_10" data-image-id="20250802130824_1b9e26f2e9853fdfe69154bb42a7c9ea6da4bf4940efc1da99b304dcfbd7d3d9" data-rendition-name="original" width="2048" height="1152" loading="lazy" alt="Visit Nepal in the monsoon"> </figure>  Chaurikharka is worthwhile to get to in any season, but it has a different charm during the monsoon. Word has spread and because it is now easy to get to from Baglung or even Pokhara, people have been flocking here.&nbsp; “Holidays and Saturdays see the largest crowds, with up to 500 visitors every day,” says ward chair Mankaji Pun of Bhume.&nbsp; There was a time not too long ago when local herders brought sheep, goats, cows, buffaloes, horses, and mules to graze here during the monsoon. Although there are still livestock around, animals have been replaced by visitors taking selfies. Read also: <a href="https://nepalitimes.com/here-now/the-monsoon-and-nature-s-arithmetic">The monsoon, and nature’s arithmetic</a>, Tom Robertson Ward Chair Pun says infrastructure development is his main priority. A foot trail to Chaurikharka was built last year by the Tourism Division Office in Kohalpur, but access via the Raniwas-Koipa road section still remains challenging.&nbsp; “If we get more budget, we can improve the road and facilities to make Chaurikharka the main tourist attraction of this region,” says Bhume Municipality Chair Hom Prakash Shrestha. “After that, we hope to promote Chaurikharka as a top tourist spot.”&nbsp; Economic activity is also picking up with the arrival of visitors, but there seems to be a need to manage the makeshift sheds made of corrugated sheets that spoil the beauty of the place. Tea shops and lodges are also available but facilities are basic. Kuldeep Neupane took a three-day trip from Ghorahi in Dang to visit Chaurikharka recently, and says: “This is an ideal trip to make a quick getaway and let nature recharge your mind and body. And it is much more fun with a tent, to watch the sunrise over the Himalaya or the mist blowing in.”

Visit Nepal in the monsoon

The final investigation report on the crash of a Saurya Airlines jet on 24 July 2024 at Kathmandu airport has revealed flaws in the carrier’s technical operation procedures, poor monitoring by the Civil Aviation Authority of Nepal (CAAN) and gaps in the airport’s emergency response. Eighteen people including a child were killed, and only the captain survived as the plane plunged seconds after takeoff, crashing within the airport perimeter. This was the latest in a series of aircraft accidents in previous years, and further tarnished Nepal’s already poor aviation safety record and contributed to the country being retained in the EU’s air safety list. &nbsp;&nbsp;&nbsp; The circumstances in the Saurya crash were different from the Yeti Airlines crash in Pokhara in January 2022 that killed all 72 on board, and two Tara Air crashes in February 2016 and May 2022 on approach to Jomsom that together claimed 45 lives. However, all four tragedies were a result of negligence of carriers and crew, failure to follow procedures, regulatory slackness, and overconfidence. The Saurya crash, especially, was a glaring example of how an ailing airline broke its own rules to allow passengers, including non-employees, a joy ride to Pokhara on a maintenance ferry flight. CRASH REPORT The Final Investigation Report prepared by the Aircraft Accident Investigation Commission and released on the first anniversary of the crash last week carried a long list of rules that were ignored or broken, and of regulatory failure. The first mistake was to cram spares, tools and inflammable chemicals needed for the aircraft’s C-Check in Pokhara into the cargo hold flouting its own ground handling procedures.&nbsp; There was no check-in of passengers, some of whom were not even employees – even though regulations say only flight and maintenance crew should be on board a maintenance positioning flight. Many brought their own luggage into the plane and stored it unsecured in the cabin. There was no flight attendant to give a safety briefing to passengers. The load and trim charts given to the flight crew were rough estimates, and the total takeoff weight of the plane was 18,300kg plus or minus 200 kg. That would still have been all right, but there was a glaring mistake in the speedchart Saurya pilots were using to calculate the minimum takeoff speed (known as VR), and it had been wrong ever since the 21-year-old aircraft entered service with the airline in 2017. FAULTY DATA&nbsp; The Commission probed Flight Data Recorder inputs from previous takeoffs of the Canadian-built CRJ200-LR in 2023-2024 and found that the undetected error in the speedchart had caused the plane to pitch up at an abnormal rotation rate at least 18 times on previous takeoffs.&nbsp; Any rotation rate more than 3°/sec is regarded as unusual. But on at least two occasions, this aircraft with tail number 9N-AME had rotation rates of 5.8°/sec and 5.5°/sec, the second one was when the pilot who survived was flying in March 2024.&nbsp; On this particular day, the plane’s rotation rate was 6.5°/sec, causing it to go into a deep stall soon after takeoff, the Commission report said. Essentially, the plane was not flying fast enough down the runway to take off safely.&nbsp; It is not yet clear whether excess weight, unsecured luggage, wrong centre of gravity were also factors, but relying on a faulty speedchart for the given takeoff weight, the captain flying pulled back on the yoke before the plane had reached takeoff speed and at a pitch angle that was too steep. The investigation report says the plane then went into a deep stall and started banking right with the stick shaking. At this point, the flight officer on the right hand seat is heard on the cockpit voice recorder saying: “Whoa, whoa, whoa. Sir, Sir, Sir…” It then banked left before the pilot flying turned the plane sharply to the right again in an evasive action to avoid the parking aprons of the international and domestic terminals. Had he not done so, there would have been a disaster of a much greater magnitude at Kathmandu airport that day. The plane scraped the runway with its right wingtip, collided with a container having helicopter spare parts, and plunged into a gully east of the runway, exploding in a fireball. The investigation also noted that the impact forces seemed to be survivable for some occupants. The fire trucks took unnecessarily long to reach the site even though it was inside the airport perimeter. The absence of an ICAO-standard runway strip, inadequate rescue drills, lack of training, and a blocked emergency service gate leading to the crash site were cited as other factors. &nbsp;&nbsp; <h2>Timestamp of a Disaster</h2>  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250731110724_39cdd04693994ce6e55a5b302905c0fa4884fe85bed21ff0779bb1439f3a5725.jpg" data-media-id="editor_0" data-image-id="20250731110724_39cdd04693994ce6e55a5b302905c0fa4884fe85bed21ff0779bb1439f3a5725" data-rendition-name="original" width="778" height="826" loading="lazy" alt="Flouting rules caused Saurya tragedy NT"> </figure>  11:10:34 - The Saurya Airlines CRJ200 on the takeoff roll from runway 02. It had a takeoff weight of about 18,300kg, but the pilot’s speedcard had a previously undetected mistake about the minimum takeoff speed. 11:10:55 -The plane with tail number 9N-AME goes into deep stall soon after takeoff because it does not have enough speed to lift its weight. The plane also has an abnormally steep nose-up attitude.&nbsp; 11:11:03 - Without enough speed to generate lift, the plane banks right, then left and right again in CCTV photos taken from the domestic apron (below). If it had not banked right, it could have hit the aprons and terminal buildings. Seen parked is Saurya’s other CRJ200 with tail number 9N-ANM.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250731110732_608132f7225c649125cca2691dd6a6bf930984c5b359e888d7ad9e5eacce3afd.jpg" data-media-id="editor_1" data-image-id="20250731110732_608132f7225c649125cca2691dd6a6bf930984c5b359e888d7ad9e5eacce3afd" data-rendition-name="original" width="770" height="555" loading="lazy" alt="Flouting rules caused Saurya tragedy NT"> </figure>  11:11:08 - The plane scrapes the runway with its right wingtip, and falls into the gully. The captain is thrown off the left side of the cockpit and survives. 11:11:15: Plane explodes in a fireball inside the airport perimeter. Firefighters take time to reach the site because of lack of access road and a blocked gate. Read the full investigation report <a href="https://www.tourism.gov.np/files/9N-AME%20AIC%20Final%20Report.pdf">here</a>.

Flouting rules caused Saurya tragedy

French citizen Louis arrived in Nepal for the first time earlier this year, planning to <a href="https://nepalitimes.com/banner/the-abcs-of-a-winter-trek-in-nepal">trek the Annapurna Circuit </a>before heading down to Bardia to hopefully catch a glimpse of some<a href="https://nepalitimes.com/news/nepal-counting-its-tigers"> tigers</a>. Before he began his journey from Besisahar, Louis (who only revealed his first name) had imagined breathing crisp mountain air, and following the melodious gurgle of the Marsyangdi.&nbsp; Instead, he had to breathe fumes and dust all the way to Chame. Louis says he masked his face with a handkerchief: “It was not what I expected, this is not right.”  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025080304080_f03fce1527cf8a63178e4e82589a1a7096c8cfa28893ca4a5f7fe82d91a6e38a.jpg" data-media-id="editor_2" data-image-id="2025080304080_f03fce1527cf8a63178e4e82589a1a7096c8cfa28893ca4a5f7fe82d91a6e38a" data-rendition-name="original" width="2419" height="1814" loading="lazy" alt="Manang trails NT 1"> </figure>  Many other trekkers are similarly disappointed as roads have been built along what used to be <a href="https://nepalitimes.com/banner/a-walk-back-in-time-chandragiri-hatiban">walking trails</a>. Manang and Humla are the last remote regions in the Himalaya to be connected to the national road network. &nbsp;Construction of the 87km Besisahar-Manang road began in 1994, but was stalled during <a href="https://nepalitimes.com/news/14-years-after-conflict-no-closure-in-nepal">the Maoist conflic</a>t, and finally finished in 2012.&nbsp; Most of it has not yet been blacktopped, and sections have been carved out of vertical cliff faces, making them treacherous. But it has allowed road access to Manang, a journey that previously took a week on foot.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025080304084_32b3ca875a0df9f1dd42dbe915e6f6a2cd4f2e53f1cf2d3ee5cbdb3435905000.jpg" data-media-id="editor_5" data-image-id="2025080304084_32b3ca875a0df9f1dd42dbe915e6f6a2cd4f2e53f1cf2d3ee5cbdb3435905000" data-rendition-name="original" width="2400" height="1505" loading="lazy" alt="Manang trails NT 1"> </figure>  While the <a href="https://nepalitimes.com/opinion/the-road-out-of-nepal">road has improved access</a>, it has impacted on<a href="https://nepalitimes.com/here-now/trekking-in-the-time-of-climate-change"> trekking tourism </a>— the mainstay of Manang’s economy. The number of tourists visiting the scenic valley behind the Annapurnas grew from 21,245 in 2023 to 30,866 in 2024. The Annapurna Circuit is known for unique sights like <a href="https://archive.nepalitimes.com/news.php?id=9194">Tilicho</a>, one of the highest lakes in the world, the Thorong La pass that connects Manang to Mustang, and the valley’s own rich cultural heritage. Thorong La at 5,416m is the highest hiking pass in the world, and was used by locals for trade with Mustang before it became a <a href="https://nepalitimes.com/opinion/comment/lift-restrictions-on-upper-mustang">popular trekking route</a>. &nbsp; “For guests, the excitement of reaching Thorong La is now overshadowed by their disappointment of having to journey through dusty roads to get there,” says Manang lodge-owner Ongma Gurung. “That is the complaint we get the most.” <a href="https://nepalitimes.com/banner/tourism-that-treads-lightly-on-the-land">Local tourism </a>operators are trying to get the government to build alternative foot trails. But there have been delays due to a lack of budget.  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025080304084_c5f76e398182785bb17846a148e3ca89de5687b4623580f8e2d725a7a287edfa.jpg" data-media-id="editor_11" data-image-id="2025080304084_c5f76e398182785bb17846a148e3ca89de5687b4623580f8e2d725a7a287edfa" data-rendition-name="original" width="2419" height="1762" loading="lazy" alt="Manang trails"> </figure>  The Naso Rural Municipality has identified other routes along the Annapurna Circuit in Chyamche, Tal, and Khotro so trekkers can bypass heavy vehicles involved in the construction of the Manang-Marsyangdi Hydropower Project. “But the local government cannot do everything,” admits the chair Dhan Bahadur Gurung. “And for leaders in Kathmandu, Manang is out of sight and out of mind.” Munindra Jung Gurung represents Manang in the Gandaki Provincial Assembly, and says he has raised the issue in <a href="https://nepalitimes.com/news/pokhara-s-tourism-woes">Pokhara</a>. He is hopeful there will be a hearing. To be sure, the road is not all bad news. Locals benefit, the number of visitors has grown, and trekkers can now also save time and use it to explore <a href="https://archive.nepalitimes.com/news.php?id=5960">side valleys in Manang</a>, visiting the villages like Nar and Phu. Annapurna Conservation Area (ACA) chief Rabin Kadariya concedes that the road to Upper Manang was crucial to connect the remote region with the rest of Nepal, but adds: “We have built an alternative trail connecting Talgaun, and we will consult local communities about their priorities on other hiking trails.”&nbsp;

Trailing off in Manang

American artist Peter Makela was in Nepal in 2022 on a Fulbright scholarship when he experienced the Matya festival in Patan in which devotees made the rounds of the city’s shrines.&nbsp;
He joined the procession, walking through 2,600 stupa and 140 bahal of the town. That immersion left a lasting impression.
As part of Gallery Mcube’s international residency program in Patan, he put his inspiration to canvas in the exhibition Yala Yatra: Walking, Working, Worshipping. The exhibition also coincides with this month’s Matya festival.&nbsp;
Makela has visited Nepal often in the past 11 years but he mostly stayed in and spent his time around Boudha. “This time I stayed in Patan, put the sites I wanted to visit on my map, and off I went,” he tells us. “Each of my artwork is inspired by the stupas and shrines in Patan that I visited.”
The stupa and Ganesh are recurring motifs in his watercolours, and the elephant gods are located in chaityas — reflecting the interplay and blending of the Hindu and Buddhist faiths in Kathmandu Valley.&nbsp;
The stupas and Ganesh are painted in vivid red, yellow, blue and green against abstract backgrounds meant to represent the sky.
“I use the sky as a backdrop because the sky has no border,” says Makela. “The four colours represent the four elements, the different Buddha families and also lights bouncing off of a rainbow.”
The use of just four colours for all the artwork stands out, and combined with the absence of heavy canvases, frames or stands render Makela’s art striking in its simplicity.&nbsp;
The Ganesh is always holding something and the art also portrays the elephant god’s sacred vehicle, the mouse.
While his vibrant stupas and Ganesh reflect the tangibility of Patan’s tradition and heritage, it is as if the backdrops with their shades of grey and red and yellow capture the soul of the city’s shrines.
“If you look closely, there is a sense of form and formlessness at the same time,” he says.&nbsp;
Makela walked 108 kora around the shrines during his exploration of the town, and in the process developed a spiritual connection with Patan’s heritage and traditions.&nbsp;
The exhibition connects with visitors on a deeper, more spiritual, level as well. And with it, they feel a sense of pride as well as the need to urgently preserve Patan’s heritage for future generations.
“Peter’s inclination and approach towards Nepali art and culture is fascinating, and it reflects in his work,” says Mcube curator Manish Lal Shrestha, whose international artist residency program promotes Nepal’s cultural heritage. &nbsp;&nbsp;
Yala Yatra: Walking, Working, Worshipping
1-5 August&nbsp;
10AM-7PM
Gallery Mcube, Patan