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

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Meltpools in the Himalaya

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

Living below Nepal’s melting mountains

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

Two weeks ago, Prime Minister KP Sharma Oli announced jubilantly on social media that Nepal had achieved a historic annual growth of 81.8% in exports. He was right. Nepal’s trade did take a great leap forward compared to last year. But the dramatic rise was mainly due to processed soya bean oil.&nbsp; However, Nepal does not produce the edible oil it exports. In fact, the soya and palm oil that make up 44% of total exports are imported from Southeast Asia and South America, and simply re-exported, mostly to India.&nbsp; Under the SAFTA (South Asian Free Trade Area) Agreement, Nepal can export products to India duty-free if it has at least 30% value-added. Nepal’s traders have taken advantage of SAFTA even though the edible oils they export do not reach that value addition threshold. “The 30% value addition requirement is often only on paper,” says former commerce secretary Purushottam Ojha. “It is clear that simply packaging edible oils in Nepal does not fulfil the terms of the trade agreement.” Prime Minister Oli is aware of this, and even called Nepal’s export figures “fake” at an earlier event. The government is relying on other iffy figures to suggest that Nepal’s economy is strong and getting stronger. For example, the value of imports rose by 13.25% in 2024-25 compared to the previous fiscal year.&nbsp; Some of it was due to a jump in electric vehicle imports worth Rs 31.76 billion, but mostly it was because more wholesale soya oil was imported to be re-packaged and sold in India. The very fact that the government boasts about increased imports is an indication of how much it relies on taxing them for revenue. Touting such trade figures cannot be the basis to claim an economic rebound.&nbsp; “A jump in the value of imports can be interpreted as an increase in purchasing power, but it is not evidence of a stronger economy,” says economist Keshav Acharya. “Even though imports have increased, Nepal's domestic production and productive capacity have not improved.” Nepal Rastra Bank's semi-annual economic activity study report shows that industrial production was down in the first six months of the last fiscal year. This despite an increase in the number of new industries registered and investment commitments. Out of the Rs70.2 billion proposed foreign investment, Nepal received only Rs17.9 billion last year.&nbsp; Meanwhile, the rate of capital formation was limited to 24% last year, which is lower than the year before, suggesting that new investment, job creation and economic expansion all declined. If domestic production does not improve in relation to this year’s inflated trade figures, the outflow will put pressure on foreign exchange reserves like it did three years ago. At that time, Nepal borrowed from the IMF under its Extended Credit Facility Program to kickstart the economy.&nbsp;  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/2025080710084_2cdaaa5795828c4a7de93a0604ba884ef0a8b8f24cccd939f6c24e279ab6058f.jpg" data-media-id="editor_0" data-image-id="2025080710084_2cdaaa5795828c4a7de93a0604ba884ef0a8b8f24cccd939f6c24e279ab6058f" data-rendition-name="original" width="1633" height="723" loading="lazy" alt="Nepal's bubble economy NT"> <figcaption>Source: NEPAL RASTRA BANK</figcaption> </figure>  The macroeconomy is on firm footing with foreign exchange reserves at a comfortable Rs2,520 billion in May, up 23% from last year. This was largely due to remittances, and partly due to a falling NPR exchange rate. Real estate transactions and the stock market index have also been climbing as a result of government policies to revive the sector.&nbsp; However, former executive director of Nepal Rastra Bank Nar Bahadur Thapa cautions: “This is not organic growth, it is the result of deliberate policy decisions to relax rules on real estate and stock markets transactions.” In reality, the sharp rise in land prices have increased the cost of production, and excessive monetisation of the real estate has become the main source of Nepal’s economic woes. The central bank has announced a slew of new policies, shifting the terms of loan repayment for industrialists and entrepreneurs, reducing interest rates, and injecting more working capital — all designed to inject adrenaline into the real estate and stock market sectors.&nbsp; When he was governor, Mahaprasad Adhikari made several financial reforms during the latter half of his tenure to stimulate the economy, including tightening credit flow.&nbsp; By the last fiscal year, additional financial reforms had resulted in a credit expansion rate of around 8%. As the pace of credit expansion slows, real estate prices have started to fall. This is actually beneficial to the economy, because it lays the foundation for improvements in land-related entrepreneurship, production, and the construction sector. Just because real estate and the stock market transactions increase, it does not indicate an economic turnaround — especially when manufacturing and productive sector continues to languish.&nbsp; “It is foolish to believe that real estate and the stock market have magically revived our economy. Agriculture employs more than half of the population, but it is in decline. Investment in the productive sector has not increased, and job creation has not increased.” Two years ago, Nepal’s industrialists, business leaders, and political leadership predicted a recession amidst a sluggish business, declining market demand, large-scale job loss, and a shrinking real estate and share market.&nbsp; Still, the economy grew by 3.36% in fiscal year 2023/24. In fact, Nepal’s economy has grown nominally over the last two decades even when all sectors of the economy are in decline.&nbsp; Says Keshav Acharya: “The growth in trade, real estate, and the stock market are bubbles. The real economy remains stagnant.”

Nepal’s bubble economy

Nepal is graduating to become a developing country on 24 November 2026 after half-century in the Least Developed Country (LDC) category. By 2030, the country hopes to transition to middle-income status.&nbsp; Everone from Prime Minister K P Oli have boasted that this is a matter of national pride, and will have a multiplier impact on trade and economy.&nbsp; But will it make any difference to the average Nepali? Not unless improved governance <a href="https://nepalitimes.com/news/why-invest-in-nepal">spurs investment and creates jobs</a>.&nbsp; Countries need to meet at least two of the three criteria in two consecutive triennial reviews to be eligible for graduation from LDC. Nepal has consistently met the thresholds for the Human Assets Index (HAI) and the Economic and Environmental Vulnerability Index (EVI) in 2015, 2018, and 2021. But Nepal was recommended for graduation before meeting the per capita <a href="https://nepalitimes.com/banner/nepals-great-income-divide">Gross National Income (GNI)</a> threshold of $1,306. “A major implication of LDC graduation is the loss of preferential market access available through Generalised System of Preferences (GSP) and other arrangements,” explains economist Sameer Khatiwada. “But over two-thirds of <a href="https://nepalitimes.com/news/nepal-doesnt-produce-its-2-biggest-export-items">Nepal’s exports</a> are to India, and the preferential market access to India is through a bilateral trade agreement. This has nothing to do with our LDC status.”  <figure> <img src="https://publisher-publish.s3.eu-central-1.amazonaws.com/pb-nepalitimes/swp/asv65r/media/20250815060832_f5eabe7628a8cdf84f33b25d7cef3c4dc8913a26d8e5b253ea52a36e176b8a85.jpg" data-media-id="editor_3" data-image-id="20250815060832_f5eabe7628a8cdf84f33b25d7cef3c4dc8913a26d8e5b253ea52a36e176b8a85" data-rendition-name="original" width="640" height="470" loading="lazy" alt="LDC graduation "> </figure>  Furthermore, a provision under the South Asian Free Trade Area (SAFTA) allows Nepal to export to India duty-free if the items are at least 30% value-added. Nepali traders take advantage of this by re-exporting edible oils without meeting that requirement, falsely boosting Nepal’s exports.“ Following graduation from LDC, the value addition threshold might increase to 40%,” says Kalpana Khanal of the Policy Research Institute. “This is supposed to work to our advantage, because on paper value addition inherently means <a href="https://nepalitimes.com/multimedia/staying-home-to-create-jobs">job creation at home</a>.” But Nepal’s exports to other major destinations will face <a href="https://nepalitimes.com/news/nepal-and-the-us-india-tariff-tiff">tariff increases</a> with the graduation. A South Asia Watch on Trade, Economics and Environment (SWATEE) study shows that while tariff increase in the US market is relatively low (see page 5) it is considerably higher in Europe. The International Trade Centre (ITC) in a 2022 study also estimated that graduation could result in a 4.3% decline in Nepal’s projected exports, but this is excluding the impact of changes in ‘rules of origin’ provisions in preference-granting countries such as the UK and Europe.&nbsp; Nepal’s top export to these preference-granting countries is <a href="https://archive.nepalitimes.com/news.php?id=1482">carpets</a>, and will not be impacted, but other items such as textiles and apparel will be heavily affected due to higher cost of production. The impact will felt mostly by small and medium enterprises which represent the largest share of exports to LDC-specific preference-granting countries. As for the service exports, Nepal never really made use of the World Trade Organization’s LDC services waiver anyway, hence the effect will be minimal, if any. There is also concern about Nepal’s graduation at a time when the global economy is topsy-turvy, amidst <a href="https://nepalitimes.com/opinion/turning-point-in-us-india-relations">tariff wars and conflicts</a>. This affects Nepalis abroad directly and may impact <a href="https://nepalitimes.com/news/more-remittance-more-than-remittance">remittances </a>which hit $11 billion in 2024. In comparison, Nepal only received $350 million in foreign loans and grants last year.&nbsp; Tourism arrivals have finally reached pre-pandemic levels, but bad publicity about pollution, poor infrastructure and bureaucratic hurdles hinder further growth. Manufacturing continues to struggle, while hydropower and the IT sector have taken off.&nbsp; “Look at data -- <a href="https://nepalitimes.com/news/tourism-needs-a-new-push">tourism arrivals</a> are up, spending is up, IT exports are up, <a href="https://nepalitimes.com/news/why-nepal-needs-to-restore-ev-tax-subsidy">EV sales </a>are up, Europe still needs 85-90 million skilled workers. We are sitting on $16 billion in cash reserves, our balance of payment, foreign exchange reserve, tax to GDP ratio, credit flow are all positive, we have to build on these factors,” says Sujeev Shakya of the Nepal Economic Forum. He adds: “Our mindset creates negativity to promote rent-seeking behaviour, but this cynicism will go away after 2026 with LDC graduation. We must deal with data, look at trends, and projects which will bring in <a href="https://nepalitimes.com/from-the-nepali-press/why-there-is-no-foreign-investment-in-nepal">international investments</a>.” Khanal agrees that investment is not dependent on<a href="https://archive.nepalitimes.com/regular-columns/backside/Nepal-not-the-least-developed-country,306"> LDC status</a>. The factors that that affect investment are policy stability, a strong legal framework, market potential and ease of doing business. She adds, “That is where our focus needs to be, and we need to retain <a href="https://nepalitimes.com/diaspora-diaries/migrant-worker-returns-to-create-work-at-home?fbclid=IwAR09xJfsClCwn8uRVAmz28CU658vdKpuyDwB_b1sNlvKtAFFnSldnA0JS2g">Nepalis with jobs at home</a> for our sustained growth.” After 2026, financing support from donors and aid agencies could be affected and Nepal will no longer be able to access Least Developed Countries Fund (LDCF) to adapt to the impacts of climate change. But the Global Environment Fund and Green Climate Fund will still be available.“ LDC status does not determine bilateral development aid, that is usually driven by broader <a href="https://nepalitimes.com/here-now/looking-beyond-two-boulders">geopolitical considerations</a>,” says Sameer Khatiwada. “The World Bank and Asian Development Bank, which provide concessional loans to Nepal, it is determined mainly by per capita income, not LDC status.” &nbsp;However, Nepal may lose some concessional terms for loans. Nepal is currently a lower-middle-income country as per the World Bank in the bracket for GNI between $1,036 and $4,045. The country is already receiving more loans than grants and in July the World Bank increased its interest rate on loans by 100% from 0.75 to 1.5%. “All this means that the impact of LDC graduation for Nepal might not be as earth-shattering as some tend to think. Countries that have recently graduated, such as Botswana and the Maldives, have shows that graduation is just a step in a country’s development path,” says Khatiwada. Sujeev Shakya also sees the glass as half full, explaining that LDC graduation is just a stepping stone if Nepal has the right policies in place. He adds, “Nepal’s biggest advantage is our<a href="https://nepalitimes.com/opinion/investing-in-people"> working age population</a> and we have investments coming in. These aided by how adaptive we are as a society are the very foundations on which Nepal will grow.”

Not poor, but not rich

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>.

glaciers-lake-outburst-flood

Meltpools in the Himalaya

Living below Nepal’s melting mountains

Visit Nepal in the monsoon

Nepal’s bubble economy

Not poor, but not rich

Flouting rules caused Saurya tragedy